!+---+-----------------------------------------------------------------+
!.. This subroutine computes the moisture tendencies of water vapor,
!.. cloud droplets, rain, cloud ice (pristine), snow, and graupel.
!.. Prior to WRFv2.2 this code was based on Reisner et al (1998), but
!.. few of those pieces remain.  A complete description is now found in
!.. Thompson, G., P. R. Field, R. M. Rasmussen, and W. D. Hall, 2008:
!.. Explicit Forecasts of winter precipitation using an improved bulk
!.. microphysics scheme. Part II: Implementation of a new snow
!.. parameterization.  Mon. Wea. Rev., 136, 5095-5115.
!.. Prior to WRFv3.1, this code was single-moment rain prediction as
!.. described in the reference above, but in v3.1 and higher, the
!.. scheme is two-moment rain (predicted rain number concentration).
!..
!.. Beginning with WRFv3.6, this is also the "aerosol-aware" scheme as
!.. described in Thompson, G. and T. Eidhammer, 2014:  A study of
!.. aerosol impacts on clouds and precipitation development in a large
!.. winter cyclone.  J. Atmos. Sci., 71, 3636-3658.  Setting WRF
!.. namelist option mp_physics=8 utilizes the older one-moment cloud
!.. water with constant droplet concentration set as Nt_c (found below)
!.. while mp_physics=28 uses double-moment cloud droplet number
!.. concentration, which is not permitted to exceed Nt_c_max below.
!..
!.. Most importantly, users may wish to modify the prescribed number of
!.. cloud droplets (Nt_c; see guidelines mentioned below).  Otherwise,
!.. users may alter the rain and graupel size distribution parameters
!.. to use exponential (Marshal-Palmer) or generalized gamma shape.
!.. The snow field assumes a combination of two gamma functions (from
!.. Field et al. 2005) and would require significant modifications
!.. throughout the entire code to alter its shape as well as accretion
!.. rates.  Users may also alter the constants used for density of rain,
!.. graupel, ice, and snow, but the latter is not constant when using
!.. Paul Field's snow distribution and moments methods.  Other values
!.. users can modify include the constants for mass and/or velocity
!.. power law relations and assumed capacitances used in deposition/
!.. sublimation/evaporation/melting.
!.. Remaining values should probably be left alone.
!..
!..Author: Greg Thompson, NCAR-RAL, gthompsn@ucar.edu, 303-497-2805
!..Last modified: 11 Feb 2015   Aerosol additions to v3.5.1 code 9/2013
!..                 Cloud fraction additions 11/2014 part of pre-v3.7
!+---+-----------------------------------------------------------------+
!wrft:model_layer:physics
!+---+-----------------------------------------------------------------+
!
      MODULE module_mp_thompson

      USE module_wrf_error
      USE module_mp_radar
#if ( defined( DM_PARALLEL ) && ( ! defined( STUBMPI ) ) )
      USE module_dm, ONLY : wrf_dm_max_real
#endif

      IMPLICIT NONE

      LOGICAL, PARAMETER, PRIVATE:: iiwarm = .false.
      LOGICAL, PRIVATE:: is_aerosol_aware = .false.
      LOGICAL, PARAMETER, PRIVATE:: dustyIce = .true.
      LOGICAL, PARAMETER, PRIVATE:: homogIce = .true.

      INTEGER, PARAMETER, PRIVATE:: IFDRY = 0
      REAL, PARAMETER, PRIVATE:: T_0 = 273.15
      REAL, PARAMETER, PRIVATE:: PI = 3.1415926536

!..Densities of rain, snow, graupel, and cloud ice.
      REAL, PARAMETER, PRIVATE:: rho_w = 1000.0
      REAL, PARAMETER, PRIVATE:: rho_s = 100.0
      REAL, PARAMETER, PRIVATE:: rho_g = 500.0
      REAL, PARAMETER, PRIVATE:: rho_i = 890.0

!..Prescribed number of cloud droplets.  Set according to known data or
!.. roughly 100 per cc (100.E6 m^-3) for Maritime cases and
!.. 300 per cc (300.E6 m^-3) for Continental.  Gamma shape parameter,
!.. mu_c, calculated based on Nt_c is important in autoconversion
!.. scheme.  In 2-moment cloud water, Nt_c represents a maximum of
!.. droplet concentration and nu_c is also variable depending on local
!.. droplet number concentration.
      REAL, PARAMETER, PRIVATE:: Nt_c = 100.E6
      REAL, PARAMETER, PRIVATE:: Nt_c_max = 1999.E6

!..Declaration of constants for assumed CCN/IN aerosols when none in
!.. the input data.  Look inside the init routine for modifications
!.. due to surface land-sea points or vegetation characteristics.
      REAL, PARAMETER, PRIVATE:: naIN0 = 1.5E6
      REAL, PARAMETER, PRIVATE:: naIN1 = 0.5E6
      REAL, PARAMETER, PRIVATE:: naCCN0 = 300.0E6
      REAL, PARAMETER, PRIVATE:: naCCN1 = 50.0E6

!..Generalized gamma distributions for rain, graupel and cloud ice.
!.. N(D) = N_0 * D**mu * exp(-lamda*D);  mu=0 is exponential.
      REAL, PARAMETER, PRIVATE:: mu_r = 0.0
      REAL, PARAMETER, PRIVATE:: mu_g = 0.0
      REAL, PARAMETER, PRIVATE:: mu_i = 0.0
      REAL, PRIVATE:: mu_c

!..Sum of two gamma distrib for snow (Field et al. 2005).
!.. N(D) = M2**4/M3**3 * [Kap0*exp(-M2*Lam0*D/M3)
!..    + Kap1*(M2/M3)**mu_s * D**mu_s * exp(-M2*Lam1*D/M3)]
!.. M2 and M3 are the (bm_s)th and (bm_s+1)th moments respectively
!.. calculated as function of ice water content and temperature.
      REAL, PARAMETER, PRIVATE:: mu_s = 0.6357
      REAL, PARAMETER, PRIVATE:: Kap0 = 490.6
      REAL, PARAMETER, PRIVATE:: Kap1 = 17.46
      REAL, PARAMETER, PRIVATE:: Lam0 = 20.78
      REAL, PARAMETER, PRIVATE:: Lam1 = 3.29

!..Y-intercept parameter for graupel is not constant and depends on
!.. mixing ratio.  Also, when mu_g is non-zero, these become equiv
!.. y-intercept for an exponential distrib and proper values are
!.. computed based on same mixing ratio and total number concentration.
      REAL, PARAMETER, PRIVATE:: gonv_min = 1.E4
      REAL, PARAMETER, PRIVATE:: gonv_max = 3.E6

!..Mass power law relations:  mass = am*D**bm
!.. Snow from Field et al. (2005), others assume spherical form.
      REAL, PARAMETER, PRIVATE:: am_r = PI*rho_w/6.0
      REAL, PARAMETER, PRIVATE:: bm_r = 3.0
      REAL, PARAMETER, PRIVATE:: am_s = 0.069
      REAL, PARAMETER, PRIVATE:: bm_s = 2.0
      REAL, PARAMETER, PRIVATE:: am_g = PI*rho_g/6.0
      REAL, PARAMETER, PRIVATE:: bm_g = 3.0
      REAL, PARAMETER, PRIVATE:: am_i = PI*rho_i/6.0
      REAL, PARAMETER, PRIVATE:: bm_i = 3.0

!..Fallspeed power laws relations:  v = (av*D**bv)*exp(-fv*D)
!.. Rain from Ferrier (1994), ice, snow, and graupel from
!.. Thompson et al (2008). Coefficient fv is zero for graupel/ice.
      REAL, PARAMETER, PRIVATE:: av_r = 4854.0
      REAL, PARAMETER, PRIVATE:: bv_r = 1.0
      REAL, PARAMETER, PRIVATE:: fv_r = 195.0
      REAL, PARAMETER, PRIVATE:: av_s = 40.0
      REAL, PARAMETER, PRIVATE:: bv_s = 0.55
      REAL, PARAMETER, PRIVATE:: fv_s = 100.0
      REAL, PARAMETER, PRIVATE:: av_g = 442.0
      REAL, PARAMETER, PRIVATE:: bv_g = 0.89
      REAL, PARAMETER, PRIVATE:: av_i = 1847.5
      REAL, PARAMETER, PRIVATE:: bv_i = 1.0
      REAL, PARAMETER, PRIVATE:: av_c = 0.316946E8
      REAL, PARAMETER, PRIVATE:: bv_c = 2.0

!..Capacitance of sphere and plates/aggregates: D**3, D**2
      REAL, PARAMETER, PRIVATE:: C_cube = 0.5
      REAL, PARAMETER, PRIVATE:: C_sqrd = 0.3

!..Collection efficiencies.  Rain/snow/graupel collection of cloud
!.. droplets use variables (Ef_rw, Ef_sw, Ef_gw respectively) and
!.. get computed elsewhere because they are dependent on stokes
!.. number.
      REAL, PARAMETER, PRIVATE:: Ef_si = 0.05
      REAL, PARAMETER, PRIVATE:: Ef_rs = 0.95
      REAL, PARAMETER, PRIVATE:: Ef_rg = 0.75
      REAL, PARAMETER, PRIVATE:: Ef_ri = 0.95

!..Minimum microphys values
!.. R1 value, 1.E-12, cannot be set lower because of numerical
!.. problems with Paul Field's moments and should not be set larger
!.. because of truncation problems in snow/ice growth.
      REAL, PARAMETER, PRIVATE:: R1 = 1.E-12
      REAL, PARAMETER, PRIVATE:: R2 = 1.E-6
      REAL, PARAMETER, PRIVATE:: eps = 1.E-15

!..Constants in Cooper curve relation for cloud ice number.
      REAL, PARAMETER, PRIVATE:: TNO = 5.0
      REAL, PARAMETER, PRIVATE:: ATO = 0.304

!..Rho_not used in fallspeed relations (rho_not/rho)**.5 adjustment.
      REAL, PARAMETER, PRIVATE:: rho_not = 101325.0/(287.05*298.0)

!..Schmidt number
      REAL, PARAMETER, PRIVATE:: Sc = 0.632
      REAL, PRIVATE:: Sc3

!..Homogeneous freezing temperature
      REAL, PARAMETER, PRIVATE:: HGFR = 235.16

!..Water vapor and air gas constants at constant pressure
      REAL, PARAMETER, PRIVATE:: Rv = 461.5
      REAL, PARAMETER, PRIVATE:: oRv = 1./Rv
      REAL, PARAMETER, PRIVATE:: R = 287.04
      REAL, PARAMETER, PRIVATE:: Cp = 1004.0
      REAL, PARAMETER, PRIVATE:: R_uni = 8.314                           ! J (mol K)-1

      DOUBLE PRECISION, PARAMETER, PRIVATE:: k_b = 1.38065E-23           ! Boltzmann constant [J/K]
      DOUBLE PRECISION, PARAMETER, PRIVATE:: M_w = 18.01528E-3           ! molecular mass of water [kg/mol]
      DOUBLE PRECISION, PARAMETER, PRIVATE:: M_a = 28.96E-3              ! molecular mass of air [kg/mol]
      DOUBLE PRECISION, PARAMETER, PRIVATE:: N_avo = 6.022E23            ! Avogadro number [1/mol]
      DOUBLE PRECISION, PARAMETER, PRIVATE:: ma_w = M_w / N_avo          ! mass of water molecule [kg]
      REAL, PARAMETER, PRIVATE:: ar_volume = 4./3.*PI*(2.5e-6)**3        ! assume radius of 0.025 micrometer, 2.5e-6 cm

!..Enthalpy of sublimation, vaporization, and fusion at 0C.
      REAL, PARAMETER, PRIVATE:: lsub = 2.834E6
      REAL, PARAMETER, PRIVATE:: lvap0 = 2.5E6
      REAL, PARAMETER, PRIVATE:: lfus = lsub - lvap0
      REAL, PARAMETER, PRIVATE:: olfus = 1./lfus

!..Ice initiates with this mass (kg), corresponding diameter calc.
!..Min diameters and mass of cloud, rain, snow, and graupel (m, kg).
      REAL, PARAMETER, PRIVATE:: xm0i = 1.E-12
      REAL, PARAMETER, PRIVATE:: D0c = 1.E-6
      REAL, PARAMETER, PRIVATE:: D0r = 50.E-6
      REAL, PARAMETER, PRIVATE:: D0s = 200.E-6
      REAL, PARAMETER, PRIVATE:: D0g = 250.E-6
      REAL, PRIVATE:: D0i, xm0s, xm0g

!..Lookup table dimensions
      INTEGER, PARAMETER, PRIVATE:: nbins = 100
      INTEGER, PARAMETER, PRIVATE:: nbc = nbins
      INTEGER, PARAMETER, PRIVATE:: nbi = nbins
      INTEGER, PARAMETER, PRIVATE:: nbr = nbins
      INTEGER, PARAMETER, PRIVATE:: nbs = nbins
      INTEGER, PARAMETER, PRIVATE:: nbg = nbins
      INTEGER, PARAMETER, PRIVATE:: ntb_c = 37
      INTEGER, PARAMETER, PRIVATE:: ntb_i = 64
      INTEGER, PARAMETER, PRIVATE:: ntb_r = 37
      INTEGER, PARAMETER, PRIVATE:: ntb_s = 28
      INTEGER, PARAMETER, PRIVATE:: ntb_g = 28
      INTEGER, PARAMETER, PRIVATE:: ntb_g1 = 28
      INTEGER, PARAMETER, PRIVATE:: ntb_r1 = 37
      INTEGER, PARAMETER, PRIVATE:: ntb_i1 = 55
      INTEGER, PARAMETER, PRIVATE:: ntb_t = 9
      INTEGER, PRIVATE:: nic1, nic2, nii2, nii3, nir2, nir3, nis2, nig2, nig3
      INTEGER, PARAMETER, PRIVATE:: ntb_arc = 7
      INTEGER, PARAMETER, PRIVATE:: ntb_arw = 9
      INTEGER, PARAMETER, PRIVATE:: ntb_art = 7
      INTEGER, PARAMETER, PRIVATE:: ntb_arr = 5
      INTEGER, PARAMETER, PRIVATE:: ntb_ark = 4
      INTEGER, PARAMETER, PRIVATE:: ntb_IN = 55
      INTEGER, PRIVATE:: niIN2

      DOUBLE PRECISION, DIMENSION(nbins+1):: xDx
      DOUBLE PRECISION, DIMENSION(nbc):: Dc, dtc
      DOUBLE PRECISION, DIMENSION(nbi):: Di, dti
      DOUBLE PRECISION, DIMENSION(nbr):: Dr, dtr
      DOUBLE PRECISION, DIMENSION(nbs):: Ds, dts
      DOUBLE PRECISION, DIMENSION(nbg):: Dg, dtg
      DOUBLE PRECISION, DIMENSION(nbc):: t_Nc

!..Lookup tables for cloud water content (kg/m**3).
      REAL, DIMENSION(ntb_c), PARAMETER, PRIVATE:: &
      r_c = (/1.e-6,2.e-6,3.e-6,4.e-6,5.e-6,6.e-6,7.e-6,8.e-6,9.e-6, &
              1.e-5,2.e-5,3.e-5,4.e-5,5.e-5,6.e-5,7.e-5,8.e-5,9.e-5, &
              1.e-4,2.e-4,3.e-4,4.e-4,5.e-4,6.e-4,7.e-4,8.e-4,9.e-4, &
              1.e-3,2.e-3,3.e-3,4.e-3,5.e-3,6.e-3,7.e-3,8.e-3,9.e-3, &
              1.e-2/)

!..Lookup tables for cloud ice content (kg/m**3).
      REAL, DIMENSION(ntb_i), PARAMETER, PRIVATE:: &
      r_i = (/1.e-10,2.e-10,3.e-10,4.e-10, &
              5.e-10,6.e-10,7.e-10,8.e-10,9.e-10, &
              1.e-9,2.e-9,3.e-9,4.e-9,5.e-9,6.e-9,7.e-9,8.e-9,9.e-9, &
              1.e-8,2.e-8,3.e-8,4.e-8,5.e-8,6.e-8,7.e-8,8.e-8,9.e-8, &
              1.e-7,2.e-7,3.e-7,4.e-7,5.e-7,6.e-7,7.e-7,8.e-7,9.e-7, &
              1.e-6,2.e-6,3.e-6,4.e-6,5.e-6,6.e-6,7.e-6,8.e-6,9.e-6, &
              1.e-5,2.e-5,3.e-5,4.e-5,5.e-5,6.e-5,7.e-5,8.e-5,9.e-5, &
              1.e-4,2.e-4,3.e-4,4.e-4,5.e-4,6.e-4,7.e-4,8.e-4,9.e-4, &
              1.e-3/)

!..Lookup tables for rain content (kg/m**3).
      REAL, DIMENSION(ntb_r), PARAMETER, PRIVATE:: &
      r_r = (/1.e-6,2.e-6,3.e-6,4.e-6,5.e-6,6.e-6,7.e-6,8.e-6,9.e-6, &
              1.e-5,2.e-5,3.e-5,4.e-5,5.e-5,6.e-5,7.e-5,8.e-5,9.e-5, &
              1.e-4,2.e-4,3.e-4,4.e-4,5.e-4,6.e-4,7.e-4,8.e-4,9.e-4, &
              1.e-3,2.e-3,3.e-3,4.e-3,5.e-3,6.e-3,7.e-3,8.e-3,9.e-3, &
              1.e-2/)

!..Lookup tables for graupel content (kg/m**3).
      REAL, DIMENSION(ntb_g), PARAMETER, PRIVATE:: &
      r_g = (/1.e-5,2.e-5,3.e-5,4.e-5,5.e-5,6.e-5,7.e-5,8.e-5,9.e-5, &
              1.e-4,2.e-4,3.e-4,4.e-4,5.e-4,6.e-4,7.e-4,8.e-4,9.e-4, &
              1.e-3,2.e-3,3.e-3,4.e-3,5.e-3,6.e-3,7.e-3,8.e-3,9.e-3, &
              1.e-2/)

!..Lookup tables for snow content (kg/m**3).
      REAL, DIMENSION(ntb_s), PARAMETER, PRIVATE:: &
      r_s = (/1.e-5,2.e-5,3.e-5,4.e-5,5.e-5,6.e-5,7.e-5,8.e-5,9.e-5, &
              1.e-4,2.e-4,3.e-4,4.e-4,5.e-4,6.e-4,7.e-4,8.e-4,9.e-4, &
              1.e-3,2.e-3,3.e-3,4.e-3,5.e-3,6.e-3,7.e-3,8.e-3,9.e-3, &
              1.e-2/)

!..Lookup tables for rain y-intercept parameter (/m**4).
      REAL, DIMENSION(ntb_r1), PARAMETER, PRIVATE:: &
      N0r_exp = (/1.e6,2.e6,3.e6,4.e6,5.e6,6.e6,7.e6,8.e6,9.e6, &
                  1.e7,2.e7,3.e7,4.e7,5.e7,6.e7,7.e7,8.e7,9.e7, &
                  1.e8,2.e8,3.e8,4.e8,5.e8,6.e8,7.e8,8.e8,9.e8, &
                  1.e9,2.e9,3.e9,4.e9,5.e9,6.e9,7.e9,8.e9,9.e9, &
                  1.e10/)

!..Lookup tables for graupel y-intercept parameter (/m**4).
      REAL, DIMENSION(ntb_g1), PARAMETER, PRIVATE:: &
      N0g_exp = (/1.e4,2.e4,3.e4,4.e4,5.e4,6.e4,7.e4,8.e4,9.e4, &
                  1.e5,2.e5,3.e5,4.e5,5.e5,6.e5,7.e5,8.e5,9.e5, &
                  1.e6,2.e6,3.e6,4.e6,5.e6,6.e6,7.e6,8.e6,9.e6, &
                  1.e7/)

!..Lookup tables for ice number concentration (/m**3).
      REAL, DIMENSION(ntb_i1), PARAMETER, PRIVATE:: &
      Nt_i = (/1.0,2.0,3.0,4.0,5.0,6.0,7.0,8.0,9.0, &
               1.e1,2.e1,3.e1,4.e1,5.e1,6.e1,7.e1,8.e1,9.e1, &
               1.e2,2.e2,3.e2,4.e2,5.e2,6.e2,7.e2,8.e2,9.e2, &
               1.e3,2.e3,3.e3,4.e3,5.e3,6.e3,7.e3,8.e3,9.e3, &
               1.e4,2.e4,3.e4,4.e4,5.e4,6.e4,7.e4,8.e4,9.e4, &
               1.e5,2.e5,3.e5,4.e5,5.e5,6.e5,7.e5,8.e5,9.e5, &
               1.e6/)

!..Aerosol table parameter: Number of available aerosols, vertical
!.. velocity, temperature, aerosol mean radius, and hygroscopicity.
      REAL, DIMENSION(ntb_arc), PARAMETER, PRIVATE:: &
      ta_Na = (/10.0, 31.6, 100.0, 316.0, 1000.0, 3160.0, 10000.0/)
      REAL, DIMENSION(ntb_arw), PARAMETER, PRIVATE:: &
      ta_Ww = (/0.01, 0.0316, 0.1, 0.316, 1.0, 3.16, 10.0, 31.6, 100.0/)
      REAL, DIMENSION(ntb_art), PARAMETER, PRIVATE:: &
      ta_Tk = (/243.15, 253.15, 263.15, 273.15, 283.15, 293.15, 303.15/)
      REAL, DIMENSION(ntb_arr), PARAMETER, PRIVATE:: &
      ta_Ra = (/0.01, 0.02, 0.04, 0.08, 0.16/)
      REAL, DIMENSION(ntb_ark), PARAMETER, PRIVATE:: &
      ta_Ka = (/0.2, 0.4, 0.6, 0.8/)

!..Lookup tables for IN concentration (/m**3) from 0.001 to 1000/Liter.
      REAL, DIMENSION(ntb_IN), PARAMETER, PRIVATE:: &
      Nt_IN = (/1.0,2.0,3.0,4.0,5.0,6.0,7.0,8.0,9.0, &
               1.e1,2.e1,3.e1,4.e1,5.e1,6.e1,7.e1,8.e1,9.e1, &
               1.e2,2.e2,3.e2,4.e2,5.e2,6.e2,7.e2,8.e2,9.e2, &
               1.e3,2.e3,3.e3,4.e3,5.e3,6.e3,7.e3,8.e3,9.e3, &
               1.e4,2.e4,3.e4,4.e4,5.e4,6.e4,7.e4,8.e4,9.e4, &
               1.e5,2.e5,3.e5,4.e5,5.e5,6.e5,7.e5,8.e5,9.e5, &
               1.e6/)

!..For snow moments conversions (from Field et al. 2005)
      REAL, DIMENSION(10), PARAMETER, PRIVATE:: &
      sa = (/ 5.065339, -0.062659, -3.032362, 0.029469, -0.000285, &
              0.31255,   0.000204,  0.003199, 0.0,      -0.015952/)
      REAL, DIMENSION(10), PARAMETER, PRIVATE:: &
      sb = (/ 0.476221, -0.015896,  0.165977, 0.007468, -0.000141, &
              0.060366,  0.000079,  0.000594, 0.0,      -0.003577/)

!..Temperatures (5 C interval 0 to -40) used in lookup tables.
      REAL, DIMENSION(ntb_t), PARAMETER, PRIVATE:: &
      Tc = (/-0.01, -5., -10., -15., -20., -25., -30., -35., -40./)

!..Lookup tables for various accretion/collection terms.
!.. ntb_x refers to the number of elements for rain, snow, graupel,
!.. and temperature array indices.  Variables beginning with t-p/c/m/n
!.. represent lookup tables.  Save compile-time memory by making
!.. allocatable (2009Jun12, J. Michalakes).
      INTEGER, PARAMETER, PRIVATE:: R8SIZE = 8
      INTEGER, PARAMETER, PRIVATE:: R4SIZE = 4
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:,:,:)::             &
                tcg_racg, tmr_racg, tcr_gacr, tmg_gacr,                 &
                tnr_racg, tnr_gacr
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:,:,:)::             &
                tcs_racs1, tmr_racs1, tcs_racs2, tmr_racs2,             &
                tcr_sacr1, tms_sacr1, tcr_sacr2, tms_sacr2,             &
                tnr_racs1, tnr_racs2, tnr_sacr1, tnr_sacr2
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:,:,:)::             &
                tpi_qcfz, tni_qcfz
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:,:,:)::             &
                tpi_qrfz, tpg_qrfz, tni_qrfz, tnr_qrfz
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:)::                 &
                tps_iaus, tni_iaus, tpi_ide
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:):: t_Efrw
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:):: t_Efsw
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:,:):: tnr_rev
      REAL (KIND=R8SIZE), ALLOCATABLE, DIMENSION(:,:,:)::               &
                tpc_wev, tnc_wev
      REAL (KIND=R4SIZE), ALLOCATABLE, DIMENSION(:,:,:,:,:):: tnccn_act

!..Variables holding a bunch of exponents and gamma values (cloud water,
!.. cloud ice, rain, snow, then graupel).
      REAL, DIMENSION(5,15), PRIVATE:: cce, ccg
      REAL, DIMENSION(15), PRIVATE::  ocg1, ocg2
      REAL, DIMENSION(7), PRIVATE:: cie, cig
      REAL, PRIVATE:: oig1, oig2, obmi
      REAL, DIMENSION(13), PRIVATE:: cre, crg
      REAL, PRIVATE:: ore1, org1, org2, org3, obmr
      REAL, DIMENSION(18), PRIVATE:: cse, csg
      REAL, PRIVATE:: oams, obms, ocms
      REAL, DIMENSION(12), PRIVATE:: cge, cgg
      REAL, PRIVATE:: oge1, ogg1, ogg2, ogg3, oamg, obmg, ocmg

!..Declaration of precomputed constants in various rate eqns.
      REAL:: t1_qr_qc, t1_qr_qi, t2_qr_qi, t1_qg_qc, t1_qs_qc, t1_qs_qi
      REAL:: t1_qr_ev, t2_qr_ev
      REAL:: t1_qs_sd, t2_qs_sd, t1_qg_sd, t2_qg_sd
      REAL:: t1_qs_me, t2_qs_me, t1_qg_me, t2_qg_me

!+---+
!+---+-----------------------------------------------------------------+
!..END DECLARATIONS
!+---+-----------------------------------------------------------------+
!+---+
!ctrlL

      CONTAINS

      SUBROUTINE thompson_init(hgt, nwfa2d, nwfa, nifa, dx, dy,         &
                          is_start,                                     &
                          ids, ide, jds, jde, kds, kde,                 &
                          ims, ime, jms, jme, kms, kme,                 &
                          its, ite, jts, jte, kts, kte)

      IMPLICIT NONE

      INTEGER, INTENT(IN):: ids,ide, jds,jde, kds,kde, &
                            ims,ime, jms,jme, kms,kme, &
                            its,ite, jts,jte, kts,kte
      REAL, DIMENSION(ims:ime,kms:kme,jms:jme), INTENT(IN):: hgt

!..OPTIONAL variables that control application of aerosol-aware scheme

      REAL, DIMENSION(ims:ime,kms:kme,jms:jme), OPTIONAL, INTENT(INOUT) :: nwfa, nifa
      REAL, DIMENSION(ims:ime,jms:jme), OPTIONAL, INTENT(INOUT) :: nwfa2d
      REAL, OPTIONAL, INTENT(IN) :: DX, DY
      LOGICAL, OPTIONAL, INTENT(IN) :: is_start
      CHARACTER*256:: mp_debug


      INTEGER:: i, j, k, l, m, n
      REAL:: h_01, niIN3, niCCN3, max_test
      LOGICAL:: micro_init, has_CCN, has_IN

      is_aerosol_aware = .FALSE.
      micro_init = .FALSE.
      has_CCN    = .FALSE.
      has_IN     = .FALSE.

      write(mp_debug,*) ' DEBUG  checking column of hgt ', its+1,jts+1
      CALL wrf_debug(250, mp_debug)
      do k = kts, kte
         write(mp_debug,*) ' DEBUGT  k, hgt = ', k, hgt(its+1,k,jts+1)
         CALL wrf_debug(250, mp_debug)
      enddo

      if (PRESENT(nwfa2d) .AND. PRESENT(nwfa) .AND. PRESENT(nifa)) is_aerosol_aware = .TRUE.

      if (is_aerosol_aware) then

!..Check for existing aerosol data, both CCN and IN aerosols.  If missing
!.. fill in just a basic vertical profile, somewhat boundary-layer following.

#if ( defined( DM_PARALLEL ) && ( ! defined( STUBMPI ) ) )
      max_test = wrf_dm_max_real ( MAXVAL(nwfa(its:ite-1,:,jts:jte-1)) )
#else
      max_test = MAXVAL ( nwfa(its:ite-1,:,jts:jte-1) )
#endif

      if (max_test .lt. eps) then
         write(mp_debug,*) ' Apparently there are no initial CCN aerosols.'
         CALL wrf_debug(100, mp_debug)
         write(mp_debug,*) '   checked column at point (i,j) = ', its,jts
         CALL wrf_debug(100, mp_debug)
         do j = jts, min(jde-1,jte)
         do i = its, min(ide-1,ite)
            if (hgt(i,1,j).le.1000.0) then
               h_01 = 0.8
            elseif (hgt(i,1,j).ge.2500.0) then
               h_01 = 0.01
            else
               h_01 = 0.8*cos(hgt(i,1,j)*0.001 - 1.0)
            endif
            niCCN3 = -1.0*ALOG(naCCN1/naCCN0)/h_01
            nwfa(i,1,j) = naCCN1+naCCN0*exp(-((hgt(i,2,j)-hgt(i,1,j))/1000.)*niCCN3)
            do k = 2, kte
               nwfa(i,k,j) = naCCN1+naCCN0*exp(-((hgt(i,k,j)-hgt(i,1,j))/1000.)*niCCN3)
            enddo
         enddo
         enddo
      else
         has_CCN    = .TRUE.
         write(mp_debug,*) ' Apparently initial CCN aerosols are present.'
         CALL wrf_debug(100, mp_debug)
         write(mp_debug,*) '   column sum at point (i,j) = ', its,jts, SUM(nwfa(its,:,jts))
         CALL wrf_debug(100, mp_debug)
      endif


#if ( defined( DM_PARALLEL ) && ( ! defined( STUBMPI ) ) )
      max_test = wrf_dm_max_real ( MAXVAL(nifa(its:ite-1,:,jts:jte-1)) )
#else
      max_test = MAXVAL ( nifa(its:ite-1,:,jts:jte-1) )
#endif

      if (max_test .lt. eps) then
         write(mp_debug,*) ' Apparently there are no initial IN aerosols.'
         CALL wrf_debug(100, mp_debug)
         write(mp_debug,*) '   checked column at point (i,j) = ', its,jts
         CALL wrf_debug(100, mp_debug)
         do j = jts, min(jde-1,jte)
         do i = its, min(ide-1,ite)
            if (hgt(i,1,j).le.1000.0) then
               h_01 = 0.8
            elseif (hgt(i,1,j).ge.2500.0) then
               h_01 = 0.01
            else
               h_01 = 0.8*cos(hgt(i,1,j)*0.001 - 1.0)
            endif
            niIN3 = -1.0*ALOG(naIN1/naIN0)/h_01
            nifa(i,1,j) = naIN1+naIN0*exp(-((hgt(i,2,j)-hgt(i,1,j))/1000.)*niIN3)
            do k = 2, kte
               nifa(i,k,j) = naIN1+naIN0*exp(-((hgt(i,k,j)-hgt(i,1,j))/1000.)*niIN3)
            enddo
         enddo
         enddo
      else
         has_IN     = .TRUE.
         write(mp_debug,*) ' Apparently initial IN aerosols are present.'
         CALL wrf_debug(100, mp_debug)
         write(mp_debug,*) '   column sum at point (i,j) = ', its,jts, SUM(nifa(its,:,jts))
         CALL wrf_debug(100, mp_debug)
      endif

!..Capture initial state lowest level CCN aerosol data in 2D array.

!     do j = jts, min(jde-1,jte)
!     do i = its, min(ide-1,ite)
!        nwfa2d(i,j) = nwfa(i,kts,j)
!     enddo
!     enddo

!..Scale the lowest level aerosol data into an emissions rate.  This is
!.. very far from ideal, but need higher emissions where larger amount
!.. of existing and lesser emissions where not already lots of aerosols
!.. for first-order simplistic approach.  Later, proper connection to
!.. emission inventory would be better, but, for now, scale like this:
!.. where: Nwfa=50 per cc, emit 0.875E4 aerosols per kg per second
!..        Nwfa=500 per cc, emit 0.875E5 aerosols per kg per second
!..        Nwfa=5000 per cc, emit 0.875E6 aerosols per kg per second
!.. for a grid with 20km spacing and scale accordingly for other spacings.

      if (is_start) then
         if (SQRT(DX*DY)/20000.0 .ge. 1.0) then
            h_01 = 0.875
         else
            h_01 = (0.875 + 0.125*((20000.-SQRT(DX*DY))/16000.)) * SQRT(DX*DY)/20000.
         endif
         write(mp_debug,*) '   aerosol surface flux emission scale factor is: ', h_01
         CALL wrf_debug(100, mp_debug)
         do j = jts, min(jde-1,jte)
         do i = its, min(ide-1,ite)
            nwfa2d(i,j) = 10.0**(LOG10(nwfa(i,kts,j)*1.E-6)-3.69897)
            nwfa2d(i,j) = nwfa2d(i,j)*h_01 * 1.E6
         enddo
         enddo
!     else
!        write(mp_debug,*) '   sample (lower-left) aerosol surface flux emission rate: ', nwfa2d(1,1)
!        CALL wrf_debug(100, mp_debug)
      endif

      endif


!..Allocate space for lookup tables (J. Michalakes 2009Jun08).

      if (.NOT. ALLOCATED(tcg_racg) ) then
         ALLOCATE(tcg_racg(ntb_g1,ntb_g,ntb_r1,ntb_r))
         micro_init = .TRUE.
      endif

      if (.NOT. ALLOCATED(tmr_racg)) ALLOCATE(tmr_racg(ntb_g1,ntb_g,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tcr_gacr)) ALLOCATE(tcr_gacr(ntb_g1,ntb_g,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tmg_gacr)) ALLOCATE(tmg_gacr(ntb_g1,ntb_g,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tnr_racg)) ALLOCATE(tnr_racg(ntb_g1,ntb_g,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tnr_gacr)) ALLOCATE(tnr_gacr(ntb_g1,ntb_g,ntb_r1,ntb_r))

      if (.NOT. ALLOCATED(tcs_racs1)) ALLOCATE(tcs_racs1(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tmr_racs1)) ALLOCATE(tmr_racs1(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tcs_racs2)) ALLOCATE(tcs_racs2(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tmr_racs2)) ALLOCATE(tmr_racs2(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tcr_sacr1)) ALLOCATE(tcr_sacr1(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tms_sacr1)) ALLOCATE(tms_sacr1(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tcr_sacr2)) ALLOCATE(tcr_sacr2(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tms_sacr2)) ALLOCATE(tms_sacr2(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tnr_racs1)) ALLOCATE(tnr_racs1(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tnr_racs2)) ALLOCATE(tnr_racs2(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tnr_sacr1)) ALLOCATE(tnr_sacr1(ntb_s,ntb_t,ntb_r1,ntb_r))
      if (.NOT. ALLOCATED(tnr_sacr2)) ALLOCATE(tnr_sacr2(ntb_s,ntb_t,ntb_r1,ntb_r))

      if (.NOT. ALLOCATED(tpi_qcfz)) ALLOCATE(tpi_qcfz(ntb_c,nbc,45,ntb_IN))
      if (.NOT. ALLOCATED(tni_qcfz)) ALLOCATE(tni_qcfz(ntb_c,nbc,45,ntb_IN))

      if (.NOT. ALLOCATED(tpi_qrfz)) ALLOCATE(tpi_qrfz(ntb_r,ntb_r1,45,ntb_IN))
      if (.NOT. ALLOCATED(tpg_qrfz)) ALLOCATE(tpg_qrfz(ntb_r,ntb_r1,45,ntb_IN))
      if (.NOT. ALLOCATED(tni_qrfz)) ALLOCATE(tni_qrfz(ntb_r,ntb_r1,45,ntb_IN))
      if (.NOT. ALLOCATED(tnr_qrfz)) ALLOCATE(tnr_qrfz(ntb_r,ntb_r1,45,ntb_IN))

      if (.NOT. ALLOCATED(tps_iaus)) ALLOCATE(tps_iaus(ntb_i,ntb_i1))
      if (.NOT. ALLOCATED(tni_iaus)) ALLOCATE(tni_iaus(ntb_i,ntb_i1))
      if (.NOT. ALLOCATED(tpi_ide)) ALLOCATE(tpi_ide(ntb_i,ntb_i1))

      if (.NOT. ALLOCATED(t_Efrw)) ALLOCATE(t_Efrw(nbr,nbc))
      if (.NOT. ALLOCATED(t_Efsw)) ALLOCATE(t_Efsw(nbs,nbc))

      if (.NOT. ALLOCATED(tnr_rev)) ALLOCATE(tnr_rev(nbr, ntb_r1, ntb_r))
      if (.NOT. ALLOCATED(tpc_wev)) ALLOCATE(tpc_wev(nbc,ntb_c,nbc))
      if (.NOT. ALLOCATED(tnc_wev)) ALLOCATE(tnc_wev(nbc,ntb_c,nbc))

      if (.NOT. ALLOCATED(tnccn_act))                                   &
            ALLOCATE(tnccn_act(ntb_arc,ntb_arw,ntb_art,ntb_arr,ntb_ark))

      if (micro_init) then

!..From Martin et al. (1994), assign gamma shape parameter mu for cloud
!.. drops according to general dispersion characteristics (disp=~0.25
!.. for Maritime and 0.45 for Continental).
!.. disp=SQRT((mu+2)/(mu+1) - 1) so mu varies from 15 for Maritime
!.. to 2 for really dirty air.  This not used in 2-moment cloud water
!.. scheme and nu_c used instead and varies from 2 to 15 (integer-only).
      mu_c = MIN(15., (1000.E6/Nt_c + 2.))

!..Schmidt number to one-third used numerous times.
      Sc3 = Sc**(1./3.)

!..Compute min ice diam from mass, min snow/graupel mass from diam.
      D0i = (xm0i/am_i)**(1./bm_i)
      xm0s = am_s * D0s**bm_s
      xm0g = am_g * D0g**bm_g

!..These constants various exponents and gamma() assoc with cloud,
!.. rain, snow, and graupel.
      do n = 1, 15
         cce(1,n) = n + 1.
         cce(2,n) = bm_r + n + 1.
         cce(3,n) = bm_r + n + 4.
         cce(4,n) = n + bv_c + 1.
         cce(5,n) = bm_r + n + bv_c + 1.
         ccg(1,n) = WGAMMA(cce(1,n))
         ccg(2,n) = WGAMMA(cce(2,n))
         ccg(3,n) = WGAMMA(cce(3,n))
         ccg(4,n) = WGAMMA(cce(4,n))
         ccg(5,n) = WGAMMA(cce(5,n))
         ocg1(n) = 1./ccg(1,n)
         ocg2(n) = 1./ccg(2,n)
      enddo

      cie(1) = mu_i + 1.
      cie(2) = bm_i + mu_i + 1.
      cie(3) = bm_i + mu_i + bv_i + 1.
      cie(4) = mu_i + bv_i + 1.
      cie(5) = mu_i + 2.
      cie(6) = bm_i*0.5 + mu_i + bv_i + 1.
      cie(7) = bm_i*0.5 + mu_i + 1.
      cig(1) = WGAMMA(cie(1))
      cig(2) = WGAMMA(cie(2))
      cig(3) = WGAMMA(cie(3))
      cig(4) = WGAMMA(cie(4))
      cig(5) = WGAMMA(cie(5))
      cig(6) = WGAMMA(cie(6))
      cig(7) = WGAMMA(cie(7))
      oig1 = 1./cig(1)
      oig2 = 1./cig(2)
      obmi = 1./bm_i

      cre(1) = bm_r + 1.
      cre(2) = mu_r + 1.
      cre(3) = bm_r + mu_r + 1.
      cre(4) = bm_r*2. + mu_r + 1.
      cre(5) = mu_r + bv_r + 1.
      cre(6) = bm_r + mu_r + bv_r + 1.
      cre(7) = bm_r*0.5 + mu_r + bv_r + 1.
      cre(8) = bm_r + mu_r + bv_r + 3.
      cre(9) = mu_r + bv_r + 3.
      cre(10) = mu_r + 2.
      cre(11) = 0.5*(bv_r + 5. + 2.*mu_r)
      cre(12) = bm_r*0.5 + mu_r + 1.
      cre(13) = bm_r*2. + mu_r + bv_r + 1.
      do n = 1, 13
         crg(n) = WGAMMA(cre(n))
      enddo
      obmr = 1./bm_r
      ore1 = 1./cre(1)
      org1 = 1./crg(1)
      org2 = 1./crg(2)
      org3 = 1./crg(3)

      cse(1) = bm_s + 1.
      cse(2) = bm_s + 2.
      cse(3) = bm_s*2.
      cse(4) = bm_s + bv_s + 1.
      cse(5) = bm_s*2. + bv_s + 1.
      cse(6) = bm_s*2. + 1.
      cse(7) = bm_s + mu_s + 1.
      cse(8) = bm_s + mu_s + 2.
      cse(9) = bm_s + mu_s + 3.
      cse(10) = bm_s + mu_s + bv_s + 1.
      cse(11) = bm_s*2. + mu_s + bv_s + 1.
      cse(12) = bm_s*2. + mu_s + 1.
      cse(13) = bv_s + 2.
      cse(14) = bm_s + bv_s
      cse(15) = mu_s + 1.
      cse(16) = 1.0 + (1.0 + bv_s)/2.
      cse(17) = cse(16) + mu_s + 1.
      cse(18) = bv_s + mu_s + 3.
      do n = 1, 18
         csg(n) = WGAMMA(cse(n))
      enddo
      oams = 1./am_s
      obms = 1./bm_s
      ocms = oams**obms

      cge(1) = bm_g + 1.
      cge(2) = mu_g + 1.
      cge(3) = bm_g + mu_g + 1.
      cge(4) = bm_g*2. + mu_g + 1.
      cge(5) = bm_g*2. + mu_g + bv_g + 1.
      cge(6) = bm_g + mu_g + bv_g + 1.
      cge(7) = bm_g + mu_g + bv_g + 2.
      cge(8) = bm_g + mu_g + bv_g + 3.
      cge(9) = mu_g + bv_g + 3.
      cge(10) = mu_g + 2.
      cge(11) = 0.5*(bv_g + 5. + 2.*mu_g)
      cge(12) = 0.5*(bv_g + 5.) + mu_g
      do n = 1, 12
         cgg(n) = WGAMMA(cge(n))
      enddo
      oamg = 1./am_g
      obmg = 1./bm_g
      ocmg = oamg**obmg
      oge1 = 1./cge(1)
      ogg1 = 1./cgg(1)
      ogg2 = 1./cgg(2)
      ogg3 = 1./cgg(3)

!+---+-----------------------------------------------------------------+
!..Simplify various rate eqns the best we can now.
!+---+-----------------------------------------------------------------+

!..Rain collecting cloud water and cloud ice
      t1_qr_qc = PI*.25*av_r * crg(9)
      t1_qr_qi = PI*.25*av_r * crg(9)
      t2_qr_qi = PI*.25*am_r*av_r * crg(8)

!..Graupel collecting cloud water
      t1_qg_qc = PI*.25*av_g * cgg(9)

!..Snow collecting cloud water
      t1_qs_qc = PI*.25*av_s

!..Snow collecting cloud ice
      t1_qs_qi = PI*.25*av_s

!..Evaporation of rain; ignore depositional growth of rain.
      t1_qr_ev = 0.78 * crg(10)
      t2_qr_ev = 0.308*Sc3*SQRT(av_r) * crg(11)

!..Sublimation/depositional growth of snow
      t1_qs_sd = 0.86
      t2_qs_sd = 0.28*Sc3*SQRT(av_s)

!..Melting of snow
      t1_qs_me = PI*4.*C_sqrd*olfus * 0.86
      t2_qs_me = PI*4.*C_sqrd*olfus * 0.28*Sc3*SQRT(av_s)

!..Sublimation/depositional growth of graupel
      t1_qg_sd = 0.86 * cgg(10)
      t2_qg_sd = 0.28*Sc3*SQRT(av_g) * cgg(11)

!..Melting of graupel
      t1_qg_me = PI*4.*C_cube*olfus * 0.86 * cgg(10)
      t2_qg_me = PI*4.*C_cube*olfus * 0.28*Sc3*SQRT(av_g) * cgg(11)

!..Constants for helping find lookup table indexes.
      nic2 = NINT(ALOG10(r_c(1)))
      nii2 = NINT(ALOG10(r_i(1)))
      nii3 = NINT(ALOG10(Nt_i(1)))
      nir2 = NINT(ALOG10(r_r(1)))
      nir3 = NINT(ALOG10(N0r_exp(1)))
      nis2 = NINT(ALOG10(r_s(1)))
      nig2 = NINT(ALOG10(r_g(1)))
      nig3 = NINT(ALOG10(N0g_exp(1)))
      niIN2 = NINT(ALOG10(Nt_IN(1)))

!..Create bins of cloud water (from min diameter up to 100 microns).
      Dc(1) = D0c*1.0d0
      dtc(1) = D0c*1.0d0
      do n = 2, nbc
         Dc(n) = Dc(n-1) + 1.0D-6
         dtc(n) = (Dc(n) - Dc(n-1))
      enddo

!..Create bins of cloud ice (from min diameter up to 5x min snow size).
      xDx(1) = D0i*1.0d0
      xDx(nbi+1) = 5.0d0*D0s
      do n = 2, nbi
         xDx(n) = DEXP(DFLOAT(n-1)/DFLOAT(nbi) &
                  *DLOG(xDx(nbi+1)/xDx(1)) +DLOG(xDx(1)))
      enddo
      do n = 1, nbi
         Di(n) = DSQRT(xDx(n)*xDx(n+1))
         dti(n) = xDx(n+1) - xDx(n)
      enddo

!..Create bins of rain (from min diameter up to 5 mm).
      xDx(1) = D0r*1.0d0
      xDx(nbr+1) = 0.005d0
      do n = 2, nbr
         xDx(n) = DEXP(DFLOAT(n-1)/DFLOAT(nbr) &
                  *DLOG(xDx(nbr+1)/xDx(1)) +DLOG(xDx(1)))
      enddo
      do n = 1, nbr
         Dr(n) = DSQRT(xDx(n)*xDx(n+1))
         dtr(n) = xDx(n+1) - xDx(n)
      enddo

!..Create bins of snow (from min diameter up to 2 cm).
      xDx(1) = D0s*1.0d0
      xDx(nbs+1) = 0.02d0
      do n = 2, nbs
         xDx(n) = DEXP(DFLOAT(n-1)/DFLOAT(nbs) &
                  *DLOG(xDx(nbs+1)/xDx(1)) +DLOG(xDx(1)))
      enddo
      do n = 1, nbs
         Ds(n) = DSQRT(xDx(n)*xDx(n+1))
         dts(n) = xDx(n+1) - xDx(n)
      enddo

!..Create bins of graupel (from min diameter up to 5 cm).
      xDx(1) = D0g*1.0d0
      xDx(nbg+1) = 0.05d0
      do n = 2, nbg
         xDx(n) = DEXP(DFLOAT(n-1)/DFLOAT(nbg) &
                  *DLOG(xDx(nbg+1)/xDx(1)) +DLOG(xDx(1)))
      enddo
      do n = 1, nbg
         Dg(n) = DSQRT(xDx(n)*xDx(n+1))
         dtg(n) = xDx(n+1) - xDx(n)
      enddo

!..Create bins of cloud droplet number concentration (1 to 3000 per cc).
      xDx(1) = 1.0d0
      xDx(nbc+1) = 3000.0d0
      do n = 2, nbc
         xDx(n) = DEXP(DFLOAT(n-1)/DFLOAT(nbc)                          &
                  *DLOG(xDx(nbc+1)/xDx(1)) +DLOG(xDx(1)))
      enddo
      do n = 1, nbc
         t_Nc(n) = DSQRT(xDx(n)*xDx(n+1)) * 1.D6
      enddo
      nic1 = DLOG(t_Nc(nbc)/t_Nc(1))

!+---+-----------------------------------------------------------------+
!..Create lookup tables for most costly calculations.
!+---+-----------------------------------------------------------------+

      do m = 1, ntb_r
         do k = 1, ntb_r1
            do j = 1, ntb_g
               do i = 1, ntb_g1
                  tcg_racg(i,j,k,m) = 0.0d0
                  tmr_racg(i,j,k,m) = 0.0d0
                  tcr_gacr(i,j,k,m) = 0.0d0
                  tmg_gacr(i,j,k,m) = 0.0d0
                  tnr_racg(i,j,k,m) = 0.0d0
                  tnr_gacr(i,j,k,m) = 0.0d0
               enddo
            enddo
         enddo
      enddo

      do m = 1, ntb_r
         do k = 1, ntb_r1
            do j = 1, ntb_t
               do i = 1, ntb_s
                  tcs_racs1(i,j,k,m) = 0.0d0
                  tmr_racs1(i,j,k,m) = 0.0d0
                  tcs_racs2(i,j,k,m) = 0.0d0
                  tmr_racs2(i,j,k,m) = 0.0d0
                  tcr_sacr1(i,j,k,m) = 0.0d0
                  tms_sacr1(i,j,k,m) = 0.0d0
                  tcr_sacr2(i,j,k,m) = 0.0d0
                  tms_sacr2(i,j,k,m) = 0.0d0
                  tnr_racs1(i,j,k,m) = 0.0d0
                  tnr_racs2(i,j,k,m) = 0.0d0
                  tnr_sacr1(i,j,k,m) = 0.0d0
                  tnr_sacr2(i,j,k,m) = 0.0d0
               enddo
            enddo
         enddo
      enddo

      do m = 1, ntb_IN
         do k = 1, 45
            do j = 1, ntb_r1
               do i = 1, ntb_r
                  tpi_qrfz(i,j,k,m) = 0.0d0
                  tni_qrfz(i,j,k,m) = 0.0d0
                  tpg_qrfz(i,j,k,m) = 0.0d0
                  tnr_qrfz(i,j,k,m) = 0.0d0
               enddo
            enddo
            do j = 1, nbc
               do i = 1, ntb_c
                  tpi_qcfz(i,j,k,m) = 0.0d0
                  tni_qcfz(i,j,k,m) = 0.0d0
               enddo
            enddo
         enddo
      enddo

      do j = 1, ntb_i1
         do i = 1, ntb_i
            tps_iaus(i,j) = 0.0d0
            tni_iaus(i,j) = 0.0d0
            tpi_ide(i,j) = 0.0d0
         enddo
      enddo

      do j = 1, nbc
         do i = 1, nbr
            t_Efrw(i,j) = 0.0
         enddo
         do i = 1, nbs
            t_Efsw(i,j) = 0.0
         enddo
      enddo

      do k = 1, ntb_r
         do j = 1, ntb_r1
            do i = 1, nbr
               tnr_rev(i,j,k) = 0.0d0
            enddo
         enddo
      enddo

      do k = 1, nbc
         do j = 1, ntb_c
            do i = 1, nbc
               tpc_wev(i,j,k) = 0.0d0
               tnc_wev(i,j,k) = 0.0d0
            enddo
         enddo
      enddo

      do m = 1, ntb_ark
         do l = 1, ntb_arr
            do k = 1, ntb_art
               do j = 1, ntb_arw
                  do i = 1, ntb_arc
                     tnccn_act(i,j,k,l,m) = 1.0
                  enddo
               enddo
            enddo
         enddo
      enddo

      CALL wrf_debug(150, 'CREATING MICROPHYSICS LOOKUP TABLES ... ')
      WRITE (wrf_err_message, '(a, f5.2, a, f5.2, a, f5.2, a, f5.2)') &
          ' using: mu_c=',mu_c,' mu_i=',mu_i,' mu_r=',mu_r,' mu_g=',mu_g
      CALL wrf_debug(150, wrf_err_message)

!..Read a static file containing CCN activation of aerosols. The
!.. data were created from a parcel model by Feingold & Heymsfield with
!.. further changes by Eidhammer and Kriedenweis.
      if (is_aerosol_aware) then
         CALL wrf_debug(200, '  calling table_ccnAct routine')
         call table_ccnAct
      endif

!..Collision efficiency between rain/snow and cloud water.
      CALL wrf_debug(200, '  creating qc collision eff tables')
      call table_Efrw
      call table_Efsw

!..Drop evaporation.
      CALL wrf_debug(200, '  creating rain evap table')
      call table_dropEvap

!..Initialize various constants for computing radar reflectivity.
      xam_r = am_r
      xbm_r = bm_r
      xmu_r = mu_r
      xam_s = am_s
      xbm_s = bm_s
      xmu_s = mu_s
      xam_g = am_g
      xbm_g = bm_g
      xmu_g = mu_g
      call radar_init

      if (.not. iiwarm) then

!..Rain collecting graupel & graupel collecting rain.
      CALL wrf_debug(200, '  creating rain collecting graupel table')
      call qr_acr_qg

!..Rain collecting snow & snow collecting rain.
      CALL wrf_debug(200, '  creating rain collecting snow table')
      call qr_acr_qs

!..Cloud water and rain freezing (Bigg, 1953).
      CALL wrf_debug(200, '  creating freezing of water drops table')
      call freezeH2O

!..Conversion of some ice mass into snow category.
      CALL wrf_debug(200, '  creating ice converting to snow table')
      call qi_aut_qs

      endif

      CALL wrf_debug(150, ' ... DONE microphysical lookup tables')

      endif

      END SUBROUTINE thompson_init
!+---+-----------------------------------------------------------------+
!ctrlL
!+---+-----------------------------------------------------------------+
!..This is a wrapper routine designed to transfer values from 3D to 1D.
!+---+-----------------------------------------------------------------+
      SUBROUTINE mp_gt_driver(qv, qc, qr, qi, qs, qg, ni, nr, nc,       &
                              nwfa, nifa, nwfa2d,                       &
                              th, pii, p, w, dz, dt_in, itimestep,      &
                              RAINNC, RAINNCV, &
                              SNOWNC, SNOWNCV, &
                              GRAUPELNC, GRAUPELNCV, SR, &
#if ( WRF_CHEM == 1 )
                              rainprod, evapprod, &
#endif
                              refl_10cm, diagflag, do_radar_ref,      &
                              re_cloud, re_ice, re_snow,              &
                              has_reqc, has_reqi, has_reqs,           &
                              ids,ide, jds,jde, kds,kde, &             ! domain dims
                              ims,ime, jms,jme, kms,kme, &             ! memory dims
                              its,ite, jts,jte, kts,kte)               ! tile dims

      implicit none

!..Subroutine arguments
      INTEGER, INTENT(IN):: ids,ide, jds,jde, kds,kde, &
                            ims,ime, jms,jme, kms,kme, &
                            its,ite, jts,jte, kts,kte
      REAL, DIMENSION(ims:ime, kms:kme, jms:jme), INTENT(INOUT):: &
                          qv, qc, qr, qi, qs, qg, ni, nr, th
      REAL, DIMENSION(ims:ime, kms:kme, jms:jme), OPTIONAL, INTENT(INOUT):: &
                          nc, nwfa, nifa
      REAL, DIMENSION(ims:ime, jms:jme), OPTIONAL, INTENT(IN):: nwfa2d
      REAL, DIMENSION(ims:ime, kms:kme, jms:jme), INTENT(INOUT):: &
                          re_cloud, re_ice, re_snow
      INTEGER, INTENT(IN):: has_reqc, has_reqi, has_reqs
#if ( WRF_CHEM == 1 )
      REAL, DIMENSION(ims:ime, kms:kme, jms:jme), INTENT(INOUT):: &
                          rainprod, evapprod
#endif
      REAL, DIMENSION(ims:ime, kms:kme, jms:jme), INTENT(IN):: &
                          pii, p, w, dz
      REAL, DIMENSION(ims:ime, jms:jme), INTENT(INOUT):: &
                          RAINNC, RAINNCV, SR
      REAL, DIMENSION(ims:ime, jms:jme), OPTIONAL, INTENT(INOUT)::      &
                          SNOWNC, SNOWNCV, GRAUPELNC, GRAUPELNCV
      REAL, DIMENSION(ims:ime, kms:kme, jms:jme), INTENT(INOUT)::       &
                          refl_10cm
      REAL, INTENT(IN):: dt_in
      INTEGER, INTENT(IN):: itimestep

!..Local variables
      REAL, DIMENSION(kts:kte):: &
                          qv1d, qc1d, qi1d, qr1d, qs1d, qg1d, ni1d,     &
                          nr1d, nc1d, nwfa1d, nifa1d,                   &
                          t1d, p1d, w1d, dz1d, dBZ
      REAL, DIMENSION(kts:kte):: re_qc1d, re_qi1d, re_qs1d
#if ( WRF_CHEM == 1 )
      REAL, DIMENSION(kts:kte):: &
                          rainprod1d, evapprod1d
#endif
      REAL, DIMENSION(its:ite, jts:jte):: pcp_ra, pcp_sn, pcp_gr, pcp_ic
      REAL:: dt, pptrain, pptsnow, pptgraul, pptice
      REAL:: qc_max, qr_max, qs_max, qi_max, qg_max, ni_max, nr_max
      REAL:: nwfa1
      INTEGER:: i, j, k
      INTEGER:: imax_qc,imax_qr,imax_qi,imax_qs,imax_qg,imax_ni,imax_nr
      INTEGER:: jmax_qc,jmax_qr,jmax_qi,jmax_qs,jmax_qg,jmax_ni,jmax_nr
      INTEGER:: kmax_qc,kmax_qr,kmax_qi,kmax_qs,kmax_qg,kmax_ni,kmax_nr
      INTEGER:: i_start, j_start, i_end, j_end
      LOGICAL, OPTIONAL, INTENT(IN) :: diagflag
      INTEGER, OPTIONAL, INTENT(IN) :: do_radar_ref
      CHARACTER*256:: mp_debug

!+---+

      i_start = its
      j_start = jts
      i_end   = MIN(ite, ide-1)
      j_end   = MIN(jte, jde-1)

!..For idealized testing by developer.
!     if ( (ide-ids+1).gt.4 .and. (jde-jds+1).lt.4 .and.                &
!          ids.eq.its.and.ide.eq.ite.and.jds.eq.jts.and.jde.eq.jte) then
!        i_start = its + 2
!        i_end   = ite
!        j_start = jts
!        j_end   = jte
!     endif

      dt = dt_in
   
      qc_max = 0.
      qr_max = 0.
      qs_max = 0.
      qi_max = 0.
      qg_max = 0
      ni_max = 0.
      nr_max = 0.
      imax_qc = 0
      imax_qr = 0
      imax_qi = 0
      imax_qs = 0
      imax_qg = 0
      imax_ni = 0
      imax_nr = 0
      jmax_qc = 0
      jmax_qr = 0
      jmax_qi = 0
      jmax_qs = 0
      jmax_qg = 0
      jmax_ni = 0
      jmax_nr = 0
      kmax_qc = 0
      kmax_qr = 0
      kmax_qi = 0
      kmax_qs = 0
      kmax_qg = 0
      kmax_ni = 0
      kmax_nr = 0
      do i = 1, 256
         mp_debug(i:i) = char(0)
      enddo

      if (.NOT. is_aerosol_aware .AND. PRESENT(nc) .AND. PRESENT(nwfa)  &
                .AND. PRESENT(nifa) .AND. PRESENT(nwfa2d)) then
         write(mp_debug,*) 'WARNING, nc-nwfa-nifa-nwfa2d present but is_aerosol_aware is FALSE'
         CALL wrf_debug(0, mp_debug)
      endif

      j_loop:  do j = j_start, j_end
      i_loop:  do i = i_start, i_end

         pptrain = 0.
         pptsnow = 0.
         pptgraul = 0.
         pptice = 0.
         RAINNCV(i,j) = 0.
         IF ( PRESENT (snowncv) ) THEN
            SNOWNCV(i,j) = 0.
         ENDIF
         IF ( PRESENT (graupelncv) ) THEN
            GRAUPELNCV(i,j) = 0.
         ENDIF
         SR(i,j) = 0.

         do k = kts, kte
            t1d(k) = th(i,k,j)*pii(i,k,j)
            p1d(k) = p(i,k,j)
            w1d(k) = w(i,k,j)
            dz1d(k) = dz(i,k,j)
            qv1d(k) = qv(i,k,j)
            qc1d(k) = qc(i,k,j)
            qi1d(k) = qi(i,k,j)
            qr1d(k) = qr(i,k,j)
            qs1d(k) = qs(i,k,j)
            qg1d(k) = qg(i,k,j)
            ni1d(k) = ni(i,k,j)
            nr1d(k) = nr(i,k,j)
         enddo
         if (is_aerosol_aware) then
            do k = kts, kte
               nc1d(k) = nc(i,k,j)
               nwfa1d(k) = nwfa(i,k,j)
               nifa1d(k) = nifa(i,k,j)
            enddo
            nwfa1 = nwfa2d(i,j)
         else
            do k = kts, kte
               nc1d(k) = Nt_c
               nwfa1d(k) = 11.1E6
               nifa1d(k) = naIN1*0.01
            enddo
            nwfa1 = 11.1E6
         endif

         call mp_thompson(qv1d, qc1d, qi1d, qr1d, qs1d, qg1d, ni1d,     &
                      nr1d, nc1d, nwfa1d, nifa1d, t1d, p1d, w1d, dz1d,  &
                      pptrain, pptsnow, pptgraul, pptice, &
#if ( WRF_CHEM == 1 )
                      rainprod1d, evapprod1d, &
#endif
                      kts, kte, dt, i, j)

         pcp_ra(i,j) = pptrain
         pcp_sn(i,j) = pptsnow
         pcp_gr(i,j) = pptgraul
         pcp_ic(i,j) = pptice
         RAINNCV(i,j) = pptrain + pptsnow + pptgraul + pptice
         RAINNC(i,j) = RAINNC(i,j) + pptrain + pptsnow + pptgraul + pptice
         IF ( PRESENT(snowncv) .AND. PRESENT(snownc) ) THEN
            SNOWNCV(i,j) = pptsnow + pptice
            SNOWNC(i,j) = SNOWNC(i,j) + pptsnow + pptice
         ENDIF
         IF ( PRESENT(graupelncv) .AND. PRESENT(graupelnc) ) THEN
            GRAUPELNCV(i,j) = pptgraul
            GRAUPELNC(i,j) = GRAUPELNC(i,j) + pptgraul
         ENDIF
         SR(i,j) = (pptsnow + pptgraul + pptice)/(RAINNCV(i,j)+1.e-12)



!..Reset lowest model level to initial state aerosols (fake sfc source).
!.. Changed 13 May 2013 to fake emissions in which nwfa2d is aerosol
!.. number tendency (number per kg per second).
         if (is_aerosol_aware) then
!-GT        nwfa1d(kts) = nwfa1
            nwfa1d(kts) = nwfa1d(kts) + nwfa2d(i,j)*dt_in

            do k = kts, kte
               nc(i,k,j) = nc1d(k)
               nwfa(i,k,j) = nwfa1d(k)
               nifa(i,k,j) = nifa1d(k)
            enddo
         endif

         do k = kts, kte
            qv(i,k,j) = qv1d(k)
            qc(i,k,j) = qc1d(k)
            qi(i,k,j) = qi1d(k)
            qr(i,k,j) = qr1d(k)
            qs(i,k,j) = qs1d(k)
            qg(i,k,j) = qg1d(k)
            ni(i,k,j) = ni1d(k)
            nr(i,k,j) = nr1d(k)
            th(i,k,j) = t1d(k)/pii(i,k,j)
#if ( WRF_CHEM == 1 )
            rainprod(i,k,j) = rainprod1d(k)
            evapprod(i,k,j) = evapprod1d(k)
#endif
            if (qc1d(k) .gt. qc_max) then
             imax_qc = i
             jmax_qc = j
             kmax_qc = k
             qc_max = qc1d(k)
            elseif (qc1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative qc ', qc1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
            endif
            if (qr1d(k) .gt. qr_max) then
             imax_qr = i
             jmax_qr = j
             kmax_qr = k
             qr_max = qr1d(k)
            elseif (qr1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative qr ', qr1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
            endif
            if (nr1d(k) .gt. nr_max) then
             imax_nr = i
             jmax_nr = j
             kmax_nr = k
             nr_max = nr1d(k)
            elseif (nr1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative nr ', nr1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
            endif
            if (qs1d(k) .gt. qs_max) then
             imax_qs = i
             jmax_qs = j
             kmax_qs = k
             qs_max = qs1d(k)
            elseif (qs1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative qs ', qs1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
            endif
            if (qi1d(k) .gt. qi_max) then
             imax_qi = i
             jmax_qi = j
             kmax_qi = k
             qi_max = qi1d(k)
            elseif (qi1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative qi ', qi1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
            endif
            if (qg1d(k) .gt. qg_max) then
             imax_qg = i
             jmax_qg = j
             kmax_qg = k
             qg_max = qg1d(k)
            elseif (qg1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative qg ', qg1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
            endif
            if (ni1d(k) .gt. ni_max) then
             imax_ni = i
             jmax_ni = j
             kmax_ni = k
             ni_max = ni1d(k)
            elseif (ni1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative ni ', ni1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
            endif
            if (qv1d(k) .lt. 0.0) then
             write(mp_debug,*) 'WARNING, negative qv ', qv1d(k),        &
                        ' at i,j,k=', i,j,k
             CALL wrf_debug(150, mp_debug)
             if (k.lt.kte-2 .and. k.gt.kts+1) then
                write(mp_debug,*) '   below and above are: ', qv(i,k-1,j), qv(i,k+1,j)
                CALL wrf_debug(150, mp_debug)
                qv(i,k,j) = MAX(1.E-7, 0.5*(qv(i,k-1,j) + qv(i,k+1,j)))
             else
                qv(i,k,j) = 1.E-7
             endif
            endif
         enddo

         IF ( PRESENT (diagflag) ) THEN
         if (diagflag .and. do_radar_ref == 1) then
          call calc_refl10cm (qv1d, qc1d, qr1d, nr1d, qs1d, qg1d,       &
                      t1d, p1d, dBZ, kts, kte, i, j)
          do k = kts, kte
             refl_10cm(i,k,j) = MAX(-35., dBZ(k))
          enddo
         endif
         ENDIF

         IF (has_reqc.ne.0 .and. has_reqi.ne.0 .and. has_reqs.ne.0) THEN
          do k = kts, kte
             re_qc1d(k) = 2.51E-6
             re_qi1d(k) = 10.01E-6
             re_qs1d(k) = 10.01E-6
          enddo
          call calc_effectRad (t1d, p1d, qv1d, qc1d, nc1d, qi1d, ni1d, qs1d,  &
                      re_qc1d, re_qi1d, re_qs1d, kts, kte)
          do k = kts, kte
             re_cloud(i,k,j) = MAX( 2.51E-6, MIN(re_qc1d(k), 50.E-6))
             re_ice(i,k,j)   = MAX(10.01E-6, MIN(re_qi1d(k), 125.E-6))
             re_snow(i,k,j)  = MAX(10.01E-6, MIN(re_qs1d(k), 999.E-6))
          enddo
         ENDIF

      enddo i_loop
      enddo j_loop

! DEBUG - GT
      write(mp_debug,'(a,7(a,e13.6,1x,a,i3,a,i3,a,i3,a,1x))') 'MP-GT:', &
         'qc: ', qc_max, '(', imax_qc, ',', jmax_qc, ',', kmax_qc, ')', &
         'qr: ', qr_max, '(', imax_qr, ',', jmax_qr, ',', kmax_qr, ')', &
         'qi: ', qi_max, '(', imax_qi, ',', jmax_qi, ',', kmax_qi, ')', &
         'qs: ', qs_max, '(', imax_qs, ',', jmax_qs, ',', kmax_qs, ')', &
         'qg: ', qg_max, '(', imax_qg, ',', jmax_qg, ',', kmax_qg, ')', &
         'ni: ', ni_max, '(', imax_ni, ',', jmax_ni, ',', kmax_ni, ')', &
         'nr: ', nr_max, '(', imax_nr, ',', jmax_nr, ',', kmax_nr, ')'
      CALL wrf_debug(150, mp_debug)
! END DEBUG - GT

      do i = 1, 256
         mp_debug(i:i) = char(0)
      enddo

      END SUBROUTINE mp_gt_driver

!+---+-----------------------------------------------------------------+
!ctrlL
!+---+-----------------------------------------------------------------+
!+---+-----------------------------------------------------------------+
!.. This subroutine computes the moisture tendencies of water vapor,
!.. cloud droplets, rain, cloud ice (pristine), snow, and graupel.
!.. Previously this code was based on Reisner et al (1998), but few of
!.. those pieces remain.  A complete description is now found in
!.. Thompson et al. (2004, 2008).
!+---+-----------------------------------------------------------------+
!
      subroutine mp_thompson (qv1d, qc1d, qi1d, qr1d, qs1d, qg1d, ni1d, &
                          nr1d, nc1d, nwfa1d, nifa1d, t1d, p1d, w1d, dzq, &
                          pptrain, pptsnow, pptgraul, pptice, &
#if ( WRF_CHEM == 1 )
                          rainprod, evapprod, &
#endif
                          kts, kte, dt, ii, jj)

      implicit none

!..Sub arguments
      INTEGER, INTENT(IN):: kts, kte, ii, jj
      REAL, DIMENSION(kts:kte), INTENT(INOUT):: &
                          qv1d, qc1d, qi1d, qr1d, qs1d, qg1d, ni1d, &
                          nr1d, nc1d, nwfa1d, nifa1d, t1d
      REAL, DIMENSION(kts:kte), INTENT(IN):: p1d, w1d, dzq
      REAL, INTENT(INOUT):: pptrain, pptsnow, pptgraul, pptice
      REAL, INTENT(IN):: dt
#if ( WRF_CHEM == 1 )
      REAL, DIMENSION(kts:kte), INTENT(INOUT):: &
                          rainprod, evapprod
#endif

!..Local variables
      REAL, DIMENSION(kts:kte):: tten, qvten, qcten, qiten, &
           qrten, qsten, qgten, niten, nrten, ncten, nwfaten, nifaten

      DOUBLE PRECISION, DIMENSION(kts:kte):: prw_vcd

      DOUBLE PRECISION, DIMENSION(kts:kte):: pnc_wcd, pnc_wau, pnc_rcw, &
           pnc_scw, pnc_gcw

      DOUBLE PRECISION, DIMENSION(kts:kte):: pna_rca, pna_sca, pna_gca, &
           pnd_rcd, pnd_scd, pnd_gcd

      DOUBLE PRECISION, DIMENSION(kts:kte):: prr_wau, prr_rcw, prr_rcs, &
           prr_rcg, prr_sml, prr_gml, &
           prr_rci, prv_rev,          &
           pnr_wau, pnr_rcs, pnr_rcg, &
           pnr_rci, pnr_sml, pnr_gml, &
           pnr_rev, pnr_rcr, pnr_rfz

      DOUBLE PRECISION, DIMENSION(kts:kte):: pri_inu, pni_inu, pri_ihm, &
           pni_ihm, pri_wfz, pni_wfz, &
           pri_rfz, pni_rfz, pri_ide, &
           pni_ide, pri_rci, pni_rci, &
           pni_sci, pni_iau, pri_iha, pni_iha

      DOUBLE PRECISION, DIMENSION(kts:kte):: prs_iau, prs_sci, prs_rcs, &
           prs_scw, prs_sde, prs_ihm, &
           prs_ide

      DOUBLE PRECISION, DIMENSION(kts:kte):: prg_scw, prg_rfz, prg_gde, &
           prg_gcw, prg_rci, prg_rcs, &
           prg_rcg, prg_ihm

      DOUBLE PRECISION, PARAMETER:: zeroD0 = 0.0d0

      REAL, DIMENSION(kts:kte):: temp, pres, qv
      REAL, DIMENSION(kts:kte):: rc, ri, rr, rs, rg, ni, nr, nc, nwfa, nifa
      REAL, DIMENSION(kts:kte):: rho, rhof, rhof2
      REAL, DIMENSION(kts:kte):: qvs, qvsi, delQvs
      REAL, DIMENSION(kts:kte):: satw, sati, ssatw, ssati
      REAL, DIMENSION(kts:kte):: diffu, visco, vsc2, &
           tcond, lvap, ocp, lvt2

      DOUBLE PRECISION, DIMENSION(kts:kte):: ilamr, ilamg, N0_r, N0_g
      REAL, DIMENSION(kts:kte):: mvd_r, mvd_c
      REAL, DIMENSION(kts:kte):: smob, smo2, smo1, smo0, &
           smoc, smod, smoe, smof

      REAL, DIMENSION(kts:kte):: sed_r, sed_s, sed_g, sed_i, sed_n,sed_c

      REAL:: rgvm, delta_tp, orho, lfus2
      REAL, DIMENSION(5):: onstep
      DOUBLE PRECISION:: N0_exp, N0_min, lam_exp, lamc, lamr, lamg
      DOUBLE PRECISION:: lami, ilami, ilamc
      REAL:: xDc, Dc_b, Dc_g, xDi, xDr, xDs, xDg, Ds_m, Dg_m
      DOUBLE PRECISION:: Dr_star, Dc_star
      REAL:: zeta1, zeta, taud, tau
      REAL:: stoke_r, stoke_s, stoke_g, stoke_i
      REAL:: vti, vtr, vts, vtg, vtc
      REAL, DIMENSION(kts:kte+1):: vtik, vtnik, vtrk, vtnrk, vtsk, vtgk,  &
           vtck, vtnck
      REAL, DIMENSION(kts:kte):: vts_boost
      REAL:: Mrat, ils1, ils2, t1_vts, t2_vts, t3_vts, t4_vts, C_snow
      REAL:: a_, b_, loga_, A1, A2, tf
      REAL:: tempc, tc0, r_mvd1, r_mvd2, xkrat
      REAL:: xnc, xri, xni, xmi, oxmi, xrc, xrr, xnr
      REAL:: xsat, rate_max, sump, ratio
      REAL:: clap, fcd, dfcd
      REAL:: otemp, rvs, rvs_p, rvs_pp, gamsc, alphsc, t1_evap, t1_subl
      REAL:: r_frac, g_frac
      REAL:: Ef_rw, Ef_sw, Ef_gw, Ef_rr
      REAL:: Ef_ra, Ef_sa, Ef_ga
      REAL:: dtsave, odts, odt, odzq, hgt_agl
      REAL:: xslw1, ygra1, zans1, eva_factor
      INTEGER:: i, k, k2, n, nn, nstep, k_0, kbot, IT, iexfrq
      INTEGER, DIMENSION(5):: ksed1
      INTEGER:: nir, nis, nig, nii, nic, niin
      INTEGER:: idx_tc, idx_t, idx_s, idx_g1, idx_g, idx_r1, idx_r,     &
                idx_i1, idx_i, idx_c, idx, idx_d, idx_n, idx_in

      LOGICAL:: melti, no_micro
      LOGICAL, DIMENSION(kts:kte):: L_qc, L_qi, L_qr, L_qs, L_qg
      LOGICAL:: debug_flag
      CHARACTER*256:: mp_debug
      INTEGER:: nu_c

!+---+

      debug_flag = .false.
!     if (ii.eq.901 .and. jj.eq.379) debug_flag = .true.
      if(debug_flag) then
        write(mp_debug, *) 'DEBUG INFO, mp_thompson at (i,j) ', ii, ', ', jj
        CALL wrf_debug(550, mp_debug)
      endif

      no_micro = .true.
      dtsave = dt
      odt = 1./dt
      odts = 1./dtsave
      iexfrq = 1

!+---+-----------------------------------------------------------------+
!.. Source/sink terms.  First 2 chars: "pr" represents source/sink of
!.. mass while "pn" represents source/sink of number.  Next char is one
!.. of "v" for water vapor, "r" for rain, "i" for cloud ice, "w" for
!.. cloud water, "s" for snow, and "g" for graupel.  Next chars
!.. represent processes: "de" for sublimation/deposition, "ev" for
!.. evaporation, "fz" for freezing, "ml" for melting, "au" for
!.. autoconversion, "nu" for ice nucleation, "hm" for Hallet/Mossop
!.. secondary ice production, and "c" for collection followed by the
!.. character for the species being collected.  ALL of these terms are
!.. positive (except for deposition/sublimation terms which can switch
!.. signs based on super/subsaturation) and are treated as negatives
!.. where necessary in the tendency equations.
!+---+-----------------------------------------------------------------+

      do k = kts, kte
         tten(k) = 0.
         qvten(k) = 0.
         qcten(k) = 0.
         qiten(k) = 0.
         qrten(k) = 0.
         qsten(k) = 0.
         qgten(k) = 0.
         niten(k) = 0.
         nrten(k) = 0.
         ncten(k) = 0.
         nwfaten(k) = 0.
         nifaten(k) = 0.

         prw_vcd(k) = 0.

         pnc_wcd(k) = 0.
         pnc_wau(k) = 0.
         pnc_rcw(k) = 0.
         pnc_scw(k) = 0.
         pnc_gcw(k) = 0.

         prv_rev(k) = 0.
         prr_wau(k) = 0.
         prr_rcw(k) = 0.
         prr_rcs(k) = 0.
         prr_rcg(k) = 0.
         prr_sml(k) = 0.
         prr_gml(k) = 0.
         prr_rci(k) = 0.
         pnr_wau(k) = 0.
         pnr_rcs(k) = 0.
         pnr_rcg(k) = 0.
         pnr_rci(k) = 0.
         pnr_sml(k) = 0.
         pnr_gml(k) = 0.
         pnr_rev(k) = 0.
         pnr_rcr(k) = 0.
         pnr_rfz(k) = 0.

         pri_inu(k) = 0.
         pni_inu(k) = 0.
         pri_ihm(k) = 0.
         pni_ihm(k) = 0.
         pri_wfz(k) = 0.
         pni_wfz(k) = 0.
         pri_rfz(k) = 0.
         pni_rfz(k) = 0.
         pri_ide(k) = 0.
         pni_ide(k) = 0.
         pri_rci(k) = 0.
         pni_rci(k) = 0.
         pni_sci(k) = 0.
         pni_iau(k) = 0.
         pri_iha(k) = 0.
         pni_iha(k) = 0.

         prs_iau(k) = 0.
         prs_sci(k) = 0.
         prs_rcs(k) = 0.
         prs_scw(k) = 0.
         prs_sde(k) = 0.
         prs_ihm(k) = 0.
         prs_ide(k) = 0.

         prg_scw(k) = 0.
         prg_rfz(k) = 0.
         prg_gde(k) = 0.
         prg_gcw(k) = 0.
         prg_rci(k) = 0.
         prg_rcs(k) = 0.
         prg_rcg(k) = 0.
         prg_ihm(k) = 0.

         pna_rca(k) = 0.
         pna_sca(k) = 0.
         pna_gca(k) = 0.

         pnd_rcd(k) = 0.
         pnd_scd(k) = 0.
         pnd_gcd(k) = 0.
      enddo
#if ( WRF_CHEM == 1 )
      do k = kts, kte
         rainprod(k) = 0.
         evapprod(k) = 0.
      enddo
#endif

!+---+-----------------------------------------------------------------+
!..Put column of data into local arrays.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         temp(k) = t1d(k)
         qv(k) = MAX(1.E-10, qv1d(k))
         pres(k) = p1d(k)
         rho(k) = 0.622*pres(k)/(R*temp(k)*(qv(k)+0.622))
         nwfa(k) = MAX(11.1E6, MIN(9999.E6, nwfa1d(k)*rho(k)))
         nifa(k) = MAX(naIN1*0.01, MIN(9999.E6, nifa1d(k)*rho(k)))

         if (qc1d(k) .gt. R1) then
            no_micro = .false.
            rc(k) = qc1d(k)*rho(k)
            nc(k) = MAX(2., nc1d(k)*rho(k))
            L_qc(k) = .true.
            nu_c = MIN(15, NINT(1000.E6/nc(k)) + 2)
            lamc = (nc(k)*am_r*ccg(2,nu_c)*ocg1(nu_c)/rc(k))**obmr
            xDc = (bm_r + nu_c + 1.) / lamc
            if (xDc.lt. D0c) then
             lamc = cce(2,nu_c)/D0c
            elseif (xDc.gt. D0r*2.) then
             lamc = cce(2,nu_c)/(D0r*2.)
            endif
            nc(k) = MIN( DBLE(Nt_c_max), ccg(1,nu_c)*ocg2(nu_c)*rc(k)   &
                  / am_r*lamc**bm_r)
            if (.NOT. is_aerosol_aware) nc(k) = Nt_c
         else
            qc1d(k) = 0.0
            nc1d(k) = 0.0
            rc(k) = R1
            nc(k) = 2.
            L_qc(k) = .false.
         endif

         if (qi1d(k) .gt. R1) then
            no_micro = .false.
            ri(k) = qi1d(k)*rho(k)
            ni(k) = MAX(R2, ni1d(k)*rho(k))
            L_qi(k) = .true.
            lami = (am_i*cig(2)*oig1*ni(k)/ri(k))**obmi
            ilami = 1./lami
            xDi = (bm_i + mu_i + 1.) * ilami
            if (xDi.lt. 20.E-6) then
             lami = cie(2)/20.E-6
             ni(k) = MIN(499.D3, cig(1)*oig2*ri(k)/am_i*lami**bm_i)
            elseif (xDi.gt. 300.E-6) then
             lami = cie(2)/300.E-6
             ni(k) = cig(1)*oig2*ri(k)/am_i*lami**bm_i
            endif
         else
            qi1d(k) = 0.0
            ni1d(k) = 0.0
            ri(k) = R1
            ni(k) = R2
            L_qi(k) = .false.
         endif

         if (qr1d(k) .gt. R1) then
            no_micro = .false.
            rr(k) = qr1d(k)*rho(k)
            nr(k) = MAX(R2, nr1d(k)*rho(k))
            L_qr(k) = .true.
            lamr = (am_r*crg(3)*org2*nr(k)/rr(k))**obmr
            mvd_r(k) = (3.0 + mu_r + 0.672) / lamr
            if (mvd_r(k) .gt. 2.5E-3) then
               mvd_r(k) = 2.5E-3
               lamr = (3.0 + mu_r + 0.672) / mvd_r(k)
               nr(k) = crg(2)*org3*rr(k)*lamr**bm_r / am_r
            elseif (mvd_r(k) .lt. D0r*0.75) then
               mvd_r(k) = D0r*0.75
               lamr = (3.0 + mu_r + 0.672) / mvd_r(k)
               nr(k) = crg(2)*org3*rr(k)*lamr**bm_r / am_r
            endif
         else
            qr1d(k) = 0.0
            nr1d(k) = 0.0
            rr(k) = R1
            nr(k) = R2
            L_qr(k) = .false.
         endif
         if (qs1d(k) .gt. R1) then
            no_micro = .false.
            rs(k) = qs1d(k)*rho(k)
            L_qs(k) = .true.
         else
            qs1d(k) = 0.0
            rs(k) = R1
            L_qs(k) = .false.
         endif
         if (qg1d(k) .gt. R1) then
            no_micro = .false.
            rg(k) = qg1d(k)*rho(k)
            L_qg(k) = .true.
         else
            qg1d(k) = 0.0
            rg(k) = R1
            L_qg(k) = .false.
         endif
      enddo

!+---+-----------------------------------------------------------------+
!     if (debug_flag) then
!      write(mp_debug,*) 'DEBUG-VERBOSE at (i,j) ', ii, ', ', jj
!      CALL wrf_debug(550, mp_debug)
!      do k = kts, kte
!        write(mp_debug, '(a,i3,f8.2,1x,f7.2,1x, 11(1x,e13.6))')        &
!    &              'VERBOSE: ', k, pres(k)*0.01, temp(k)-273.15, qv(k), rc(k), rr(k), ri(k), rs(k), rg(k), nc(k), nr(k), ni(k), nwfa(k), nifa(k)
!        CALL wrf_debug(550, mp_debug)
!      enddo
!     endif
!+---+-----------------------------------------------------------------+

!+---+-----------------------------------------------------------------+
!..Derive various thermodynamic variables frequently used.
!.. Saturation vapor pressure (mixing ratio) over liquid/ice comes from
!.. Flatau et al. 1992; enthalpy (latent heat) of vaporization from
!.. Bohren & Albrecht 1998; others from Pruppacher & Klett 1978.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         tempc = temp(k) - 273.15
         rhof(k) = SQRT(RHO_NOT/rho(k))
         rhof2(k) = SQRT(rhof(k))
         qvs(k) = rslf(pres(k), temp(k))
         delQvs(k) = MAX(0.0, rslf(pres(k), 273.15)-qv(k))
         if (tempc .le. 0.0) then
          qvsi(k) = rsif(pres(k), temp(k))
         else
          qvsi(k) = qvs(k)
         endif
         satw(k) = qv(k)/qvs(k)
         sati(k) = qv(k)/qvsi(k)
         ssatw(k) = satw(k) - 1.
         ssati(k) = sati(k) - 1.
         if (abs(ssatw(k)).lt. eps) ssatw(k) = 0.0
         if (abs(ssati(k)).lt. eps) ssati(k) = 0.0
         if (no_micro .and. ssati(k).gt. 0.0) no_micro = .false.
         diffu(k) = 2.11E-5*(temp(k)/273.15)**1.94 * (101325./pres(k))
         if (tempc .ge. 0.0) then
            visco(k) = (1.718+0.0049*tempc)*1.0E-5
         else
            visco(k) = (1.718+0.0049*tempc-1.2E-5*tempc*tempc)*1.0E-5
         endif
         ocp(k) = 1./(Cp*(1.+0.887*qv(k)))
         vsc2(k) = SQRT(rho(k)/visco(k))
         lvap(k) = lvap0 + (2106.0 - 4218.0)*tempc
         tcond(k) = (5.69 + 0.0168*tempc)*1.0E-5 * 418.936
      enddo

!+---+-----------------------------------------------------------------+
!..If no existing hydrometeor species and no chance to initiate ice or
!.. condense cloud water, just exit quickly!
!+---+-----------------------------------------------------------------+

      if (no_micro) return

!+---+-----------------------------------------------------------------+
!..Calculate y-intercept, slope, and useful moments for snow.
!+---+-----------------------------------------------------------------+
      if (.not. iiwarm) then
      do k = kts, kte
         if (.not. L_qs(k)) CYCLE
         tc0 = MIN(-0.1, temp(k)-273.15)
         smob(k) = rs(k)*oams

!..All other moments based on reference, 2nd moment.  If bm_s.ne.2,
!.. then we must compute actual 2nd moment and use as reference.
         if (bm_s.gt.(2.0-1.e-3) .and. bm_s.lt.(2.0+1.e-3)) then
            smo2(k) = smob(k)
         else
            loga_ = sa(1) + sa(2)*tc0 + sa(3)*bm_s &
               + sa(4)*tc0*bm_s + sa(5)*tc0*tc0 &
               + sa(6)*bm_s*bm_s + sa(7)*tc0*tc0*bm_s &
               + sa(8)*tc0*bm_s*bm_s + sa(9)*tc0*tc0*tc0 &
               + sa(10)*bm_s*bm_s*bm_s
            a_ = 10.0**loga_
            b_ = sb(1) + sb(2)*tc0 + sb(3)*bm_s &
               + sb(4)*tc0*bm_s + sb(5)*tc0*tc0 &
               + sb(6)*bm_s*bm_s + sb(7)*tc0*tc0*bm_s &
               + sb(8)*tc0*bm_s*bm_s + sb(9)*tc0*tc0*tc0 &
               + sb(10)*bm_s*bm_s*bm_s
            smo2(k) = (smob(k)/a_)**(1./b_)
         endif

!..Calculate 0th moment.  Represents snow number concentration.
         loga_ = sa(1) + sa(2)*tc0 + sa(5)*tc0*tc0 + sa(9)*tc0*tc0*tc0
         a_ = 10.0**loga_
         b_ = sb(1) + sb(2)*tc0 + sb(5)*tc0*tc0 + sb(9)*tc0*tc0*tc0
         smo0(k) = a_ * smo2(k)**b_

!..Calculate 1st moment.  Useful for depositional growth and melting.
         loga_ = sa(1) + sa(2)*tc0 + sa(3) &
               + sa(4)*tc0 + sa(5)*tc0*tc0 &
               + sa(6) + sa(7)*tc0*tc0 &
               + sa(8)*tc0 + sa(9)*tc0*tc0*tc0 &
               + sa(10)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3) + sb(4)*tc0 &
              + sb(5)*tc0*tc0 + sb(6) &
              + sb(7)*tc0*tc0 + sb(8)*tc0 &
              + sb(9)*tc0*tc0*tc0 + sb(10)
         smo1(k) = a_ * smo2(k)**b_

!..Calculate bm_s+1 (th) moment.  Useful for diameter calcs.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(1) &
               + sa(4)*tc0*cse(1) + sa(5)*tc0*tc0 &
               + sa(6)*cse(1)*cse(1) + sa(7)*tc0*tc0*cse(1) &
               + sa(8)*tc0*cse(1)*cse(1) + sa(9)*tc0*tc0*tc0 &
               + sa(10)*cse(1)*cse(1)*cse(1)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(1) + sb(4)*tc0*cse(1) &
              + sb(5)*tc0*tc0 + sb(6)*cse(1)*cse(1) &
              + sb(7)*tc0*tc0*cse(1) + sb(8)*tc0*cse(1)*cse(1) &
              + sb(9)*tc0*tc0*tc0 + sb(10)*cse(1)*cse(1)*cse(1)
         smoc(k) = a_ * smo2(k)**b_

!..Calculate bv_s+2 (th) moment.  Useful for riming.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(13) &
               + sa(4)*tc0*cse(13) + sa(5)*tc0*tc0 &
               + sa(6)*cse(13)*cse(13) + sa(7)*tc0*tc0*cse(13) &
               + sa(8)*tc0*cse(13)*cse(13) + sa(9)*tc0*tc0*tc0 &
               + sa(10)*cse(13)*cse(13)*cse(13)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(13) + sb(4)*tc0*cse(13) &
              + sb(5)*tc0*tc0 + sb(6)*cse(13)*cse(13) &
              + sb(7)*tc0*tc0*cse(13) + sb(8)*tc0*cse(13)*cse(13) &
              + sb(9)*tc0*tc0*tc0 + sb(10)*cse(13)*cse(13)*cse(13)
         smoe(k) = a_ * smo2(k)**b_

!..Calculate 1+(bv_s+1)/2 (th) moment.  Useful for depositional growth.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(16) &
               + sa(4)*tc0*cse(16) + sa(5)*tc0*tc0 &
               + sa(6)*cse(16)*cse(16) + sa(7)*tc0*tc0*cse(16) &
               + sa(8)*tc0*cse(16)*cse(16) + sa(9)*tc0*tc0*tc0 &
               + sa(10)*cse(16)*cse(16)*cse(16)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(16) + sb(4)*tc0*cse(16) &
              + sb(5)*tc0*tc0 + sb(6)*cse(16)*cse(16) &
              + sb(7)*tc0*tc0*cse(16) + sb(8)*tc0*cse(16)*cse(16) &
              + sb(9)*tc0*tc0*tc0 + sb(10)*cse(16)*cse(16)*cse(16)
         smof(k) = a_ * smo2(k)**b_

      enddo

!+---+-----------------------------------------------------------------+
!..Calculate y-intercept, slope values for graupel.
!+---+-----------------------------------------------------------------+
      N0_min = gonv_max
      do k = kte, kts, -1
         if (temp(k).lt.270.65 .and. L_qr(k) .and. mvd_r(k).gt.100.E-6) then
            xslw1 = 4.01 + alog10(mvd_r(k))
         else
            xslw1 = 0.01
         endif
         ygra1 = 4.31 + alog10(max(5.E-5, rg(k)))
         zans1 = 3.1 + (100./(300.*xslw1*ygra1/(10./xslw1+1.+0.25*ygra1)+30.+10.*ygra1))
         N0_exp = 10.**(zans1)
         N0_exp = MAX(DBLE(gonv_min), MIN(N0_exp, DBLE(gonv_max)))
         N0_min = MIN(N0_exp, N0_min)
         N0_exp = N0_min
         lam_exp = (N0_exp*am_g*cgg(1)/rg(k))**oge1
         lamg = lam_exp * (cgg(3)*ogg2*ogg1)**obmg
         ilamg(k) = 1./lamg
         N0_g(k) = N0_exp/(cgg(2)*lam_exp) * lamg**cge(2)
      enddo

      endif

!+---+-----------------------------------------------------------------+
!..Calculate y-intercept, slope values for rain.
!+---+-----------------------------------------------------------------+
      do k = kte, kts, -1
         lamr = (am_r*crg(3)*org2*nr(k)/rr(k))**obmr
         ilamr(k) = 1./lamr
         mvd_r(k) = (3.0 + mu_r + 0.672) / lamr
         N0_r(k) = nr(k)*org2*lamr**cre(2)
      enddo

!+---+-----------------------------------------------------------------+
!..Compute warm-rain process terms (except evap done later).
!+---+-----------------------------------------------------------------+

      do k = kts, kte

!..Rain self-collection follows Seifert, 1994 and drop break-up
!.. follows Verlinde and Cotton, 1993.                                        RAIN2M
         if (L_qr(k) .and. mvd_r(k).gt. D0r) then
!-GT      Ef_rr = 1.0
!-GT      if (mvd_r(k) .gt. 1500.0E-6) then
             Ef_rr = 2.0 - EXP(2300.0*(mvd_r(k)-1600.0E-6))
!-GT      endif
          pnr_rcr(k) = Ef_rr * 0.5*nr(k)*rr(k)
         endif

         mvd_c(k) = D0c
         if (L_qc(k)) then
          nu_c = MIN(15, NINT(1000.E6/nc(k)) + 2)
          xDc = MAX(D0c*1.E6, ((rc(k)/(am_r*nc(k)))**obmr) * 1.E6)
          lamc = (nc(k)*am_r* ccg(2,nu_c) * ocg1(nu_c) / rc(k))**obmr
          mvd_c(k) = (3.0+nu_c+0.672) / lamc
         endif

!..Autoconversion follows Berry & Reinhardt (1974) with characteristic
!.. diameters correctly computed from gamma distrib of cloud droplets.
         if (rc(k).gt. 0.01e-3) then
          Dc_g = ((ccg(3,nu_c)*ocg2(nu_c))**obmr / lamc) * 1.E6
          Dc_b = (xDc*xDc*xDc*Dc_g*Dc_g*Dc_g - xDc*xDc*xDc*xDc*xDc*xDc) &
                 **(1./6.)
          zeta1 = 0.5*((6.25E-6*xDc*Dc_b*Dc_b*Dc_b - 0.4) &
                     + abs(6.25E-6*xDc*Dc_b*Dc_b*Dc_b - 0.4))
          zeta = 0.027*rc(k)*zeta1
          taud = 0.5*((0.5*Dc_b - 7.5) + abs(0.5*Dc_b - 7.5)) + R1
          tau  = 3.72/(rc(k)*taud)
          prr_wau(k) = zeta/tau
          prr_wau(k) = MIN(DBLE(rc(k)*odts), prr_wau(k))
          pnr_wau(k) = prr_wau(k) / (am_r*nu_c*D0r*D0r*D0r)              ! RAIN2M
          pnc_wau(k) = MIN(DBLE(nc(k)*odts), prr_wau(k)                 &
                     / (am_r*mvd_c(k)*mvd_c(k)*mvd_c(k)))                   ! Qc2M
         endif

!..Rain collecting cloud water.  In CE, assume Dc<<Dr and vtc=~0.
         if (L_qr(k) .and. mvd_r(k).gt. D0r .and. mvd_c(k).gt. D0c) then
          lamr = 1./ilamr(k)
          idx = 1 + INT(nbr*DLOG(mvd_r(k)/Dr(1))/DLOG(Dr(nbr)/Dr(1)))
          idx = MIN(idx, nbr)
          Ef_rw = t_Efrw(idx, INT(mvd_c(k)*1.E6))
          prr_rcw(k) = rhof(k)*t1_qr_qc*Ef_rw*rc(k)*N0_r(k) &
                         *((lamr+fv_r)**(-cre(9)))
          prr_rcw(k) = MIN(DBLE(rc(k)*odts), prr_rcw(k))
          pnc_rcw(k) = rhof(k)*t1_qr_qc*Ef_rw*nc(k)*N0_r(k)             &
                         *((lamr+fv_r)**(-cre(9)))                          ! Qc2M
          pnc_rcw(k) = MIN(DBLE(nc(k)*odts), pnc_rcw(k))
         endif

!..Rain collecting aerosols, wet scavenging.
         if (L_qr(k) .and. mvd_r(k).gt. D0r) then
          Ef_ra = Eff_aero(mvd_r(k),0.04E-6,visco(k),rho(k),temp(k),'r')
          lamr = 1./ilamr(k)
          pna_rca(k) = rhof(k)*t1_qr_qc*Ef_ra*nwfa(k)*N0_r(k)           &
                         *((lamr+fv_r)**(-cre(9)))
          pna_rca(k) = MIN(DBLE(nwfa(k)*odts), pna_rca(k))

          Ef_ra = Eff_aero(mvd_r(k),0.8E-6,visco(k),rho(k),temp(k),'r')
          pnd_rcd(k) = rhof(k)*t1_qr_qc*Ef_ra*nifa(k)*N0_r(k)           &
                         *((lamr+fv_r)**(-cre(9)))
          pnd_rcd(k) = MIN(DBLE(nifa(k)*odts), pnd_rcd(k))
         endif

      enddo

!+---+-----------------------------------------------------------------+
!..Compute all frozen hydrometeor species' process terms.
!+---+-----------------------------------------------------------------+
      if (.not. iiwarm) then
      do k = kts, kte
         vts_boost(k) = 1.5

!..Temperature lookup table indexes.
         tempc = temp(k) - 273.15
         idx_tc = MAX(1, MIN(NINT(-tempc), 45) )
         idx_t = INT( (tempc-2.5)/5. ) - 1
         idx_t = MAX(1, -idx_t)
         idx_t = MIN(idx_t, ntb_t)
         IT = MAX(1, MIN(NINT(-tempc), 31) )

!..Cloud water lookup table index.
         if (rc(k).gt. r_c(1)) then
          nic = NINT(ALOG10(rc(k)))
          do nn = nic-1, nic+1
             n = nn
             if ( (rc(k)/10.**nn).ge.1.0 .and. &
                  (rc(k)/10.**nn).lt.10.0) goto 141
          enddo
 141      continue
          idx_c = INT(rc(k)/10.**n) + 10*(n-nic2) - (n-nic2)
          idx_c = MAX(1, MIN(idx_c, ntb_c))
         else
          idx_c = 1
         endif

!..Cloud droplet number lookup table index.
         idx_n = NINT(1.0 + FLOAT(nbc) * DLOG(nc(k)/t_Nc(1)) / nic1)
         idx_n = MAX(1, MIN(idx_n, nbc))

!..Cloud ice lookup table indexes.
         if (ri(k).gt. r_i(1)) then
          nii = NINT(ALOG10(ri(k)))
          do nn = nii-1, nii+1
             n = nn
             if ( (ri(k)/10.**nn).ge.1.0 .and. &
                  (ri(k)/10.**nn).lt.10.0) goto 142
          enddo
 142      continue
          idx_i = INT(ri(k)/10.**n) + 10*(n-nii2) - (n-nii2)
          idx_i = MAX(1, MIN(idx_i, ntb_i))
         else
          idx_i = 1
         endif

         if (ni(k).gt. Nt_i(1)) then
          nii = NINT(ALOG10(ni(k)))
          do nn = nii-1, nii+1
             n = nn
             if ( (ni(k)/10.**nn).ge.1.0 .and. &
                  (ni(k)/10.**nn).lt.10.0) goto 143
          enddo
 143      continue
          idx_i1 = INT(ni(k)/10.**n) + 10*(n-nii3) - (n-nii3)
          idx_i1 = MAX(1, MIN(idx_i1, ntb_i1))
         else
          idx_i1 = 1
         endif

!..Rain lookup table indexes.
         if (rr(k).gt. r_r(1)) then
          nir = NINT(ALOG10(rr(k)))
          do nn = nir-1, nir+1
             n = nn
             if ( (rr(k)/10.**nn).ge.1.0 .and. &
                  (rr(k)/10.**nn).lt.10.0) goto 144
          enddo
 144      continue
          idx_r = INT(rr(k)/10.**n) + 10*(n-nir2) - (n-nir2)
          idx_r = MAX(1, MIN(idx_r, ntb_r))

          lamr = 1./ilamr(k)
          lam_exp = lamr * (crg(3)*org2*org1)**bm_r
          N0_exp = org1*rr(k)/am_r * lam_exp**cre(1)
          nir = NINT(DLOG10(N0_exp))
          do nn = nir-1, nir+1
             n = nn
             if ( (N0_exp/10.**nn).ge.1.0 .and. &
                  (N0_exp/10.**nn).lt.10.0) goto 145
          enddo
 145      continue
          idx_r1 = INT(N0_exp/10.**n) + 10*(n-nir3) - (n-nir3)
          idx_r1 = MAX(1, MIN(idx_r1, ntb_r1))
         else
          idx_r = 1
          idx_r1 = ntb_r1
         endif

!..Snow lookup table index.
         if (rs(k).gt. r_s(1)) then
          nis = NINT(ALOG10(rs(k)))
          do nn = nis-1, nis+1
             n = nn
             if ( (rs(k)/10.**nn).ge.1.0 .and. &
                  (rs(k)/10.**nn).lt.10.0) goto 146
          enddo
 146      continue
          idx_s = INT(rs(k)/10.**n) + 10*(n-nis2) - (n-nis2)
          idx_s = MAX(1, MIN(idx_s, ntb_s))
         else
          idx_s = 1
         endif

!..Graupel lookup table index.
         if (rg(k).gt. r_g(1)) then
          nig = NINT(ALOG10(rg(k)))
          do nn = nig-1, nig+1
             n = nn
             if ( (rg(k)/10.**nn).ge.1.0 .and. &
                  (rg(k)/10.**nn).lt.10.0) goto 147
          enddo
 147      continue
          idx_g = INT(rg(k)/10.**n) + 10*(n-nig2) - (n-nig2)
          idx_g = MAX(1, MIN(idx_g, ntb_g))

          lamg = 1./ilamg(k)
          lam_exp = lamg * (cgg(3)*ogg2*ogg1)**bm_g
          N0_exp = ogg1*rg(k)/am_g * lam_exp**cge(1)
          nig = NINT(DLOG10(N0_exp))
          do nn = nig-1, nig+1
             n = nn
             if ( (N0_exp/10.**nn).ge.1.0 .and. &
                  (N0_exp/10.**nn).lt.10.0) goto 148
          enddo
 148      continue
          idx_g1 = INT(N0_exp/10.**n) + 10*(n-nig3) - (n-nig3)
          idx_g1 = MAX(1, MIN(idx_g1, ntb_g1))
         else
          idx_g = 1
          idx_g1 = ntb_g1
         endif

!..Deposition/sublimation prefactor (from Srivastava & Coen 1992).
         otemp = 1./temp(k)
         rvs = rho(k)*qvsi(k)
         rvs_p = rvs*otemp*(lsub*otemp*oRv - 1.)
         rvs_pp = rvs * ( otemp*(lsub*otemp*oRv - 1.) &
                         *otemp*(lsub*otemp*oRv - 1.) &
                         + (-2.*lsub*otemp*otemp*otemp*oRv) &
                         + otemp*otemp)
         gamsc = lsub*diffu(k)/tcond(k) * rvs_p
         alphsc = 0.5*(gamsc/(1.+gamsc))*(gamsc/(1.+gamsc)) &
                    * rvs_pp/rvs_p * rvs/rvs_p
         alphsc = MAX(1.E-9, alphsc)
         xsat = ssati(k)
         if (abs(xsat).lt. 1.E-9) xsat=0.
         t1_subl = 4.*PI*( 1.0 - alphsc*xsat &
                + 2.*alphsc*alphsc*xsat*xsat &
                - 5.*alphsc*alphsc*alphsc*xsat*xsat*xsat ) &
                / (1.+gamsc)

!..Snow collecting cloud water.  In CE, assume Dc<<Ds and vtc=~0.
         if (L_qc(k) .and. mvd_c(k).gt. D0c) then
          xDs = 0.0
          if (L_qs(k)) xDs = smoc(k) / smob(k)
          if (xDs .gt. D0s) then
           idx = 1 + INT(nbs*DLOG(xDs/Ds(1))/DLOG(Ds(nbs)/Ds(1)))
           idx = MIN(idx, nbs)
           Ef_sw = t_Efsw(idx, INT(mvd_c(k)*1.E6))
           prs_scw(k) = rhof(k)*t1_qs_qc*Ef_sw*rc(k)*smoe(k)
           pnc_scw(k) = rhof(k)*t1_qs_qc*Ef_sw*nc(k)*smoe(k)                ! Qc2M
           pnc_scw(k) = MIN(DBLE(nc(k)*odts), pnc_scw(k))
          endif

!..Graupel collecting cloud water.  In CE, assume Dc<<Dg and vtc=~0.
          if (rg(k).ge. r_g(1) .and. mvd_c(k).gt. D0c) then
           xDg = (bm_g + mu_g + 1.) * ilamg(k)
           vtg = rhof(k)*av_g*cgg(6)*ogg3 * ilamg(k)**bv_g
           stoke_g = mvd_c(k)*mvd_c(k)*vtg*rho_w/(9.*visco(k)*xDg)
           if (xDg.gt. D0g) then
            if (stoke_g.ge.0.4 .and. stoke_g.le.10.) then
             Ef_gw = 0.55*ALOG10(2.51*stoke_g)
            elseif (stoke_g.lt.0.4) then
             Ef_gw = 0.0
            elseif (stoke_g.gt.10) then
             Ef_gw = 0.77
            endif
            prg_gcw(k) = rhof(k)*t1_qg_qc*Ef_gw*rc(k)*N0_g(k) &
                          *ilamg(k)**cge(9)
            pnc_gcw(k) = rhof(k)*t1_qg_qc*Ef_gw*nc(k)*N0_g(k)           &
                          *ilamg(k)**cge(9)                                 ! Qc2M
            pnc_gcw(k) = MIN(DBLE(nc(k)*odts), pnc_gcw(k))
           endif
          endif
         endif

!..Snow and graupel collecting aerosols, wet scavenging.
         if (rs(k) .gt. r_s(1)) then
          xDs = smoc(k) / smob(k)
          Ef_sa = Eff_aero(xDs,0.04E-6,visco(k),rho(k),temp(k),'s')
          pna_sca(k) = rhof(k)*t1_qs_qc*Ef_sa*nwfa(k)*smoe(k)
          pna_sca(k) = MIN(DBLE(nwfa(k)*odts), pna_sca(k))

          Ef_sa = Eff_aero(xDs,0.8E-6,visco(k),rho(k),temp(k),'s')
          pnd_scd(k) = rhof(k)*t1_qs_qc*Ef_sa*nifa(k)*smoe(k)
          pnd_scd(k) = MIN(DBLE(nifa(k)*odts), pnd_scd(k))
         endif
         if (rg(k) .gt. r_g(1)) then
          xDg = (bm_g + mu_g + 1.) * ilamg(k)
          Ef_ga = Eff_aero(xDg,0.04E-6,visco(k),rho(k),temp(k),'g')
          pna_gca(k) = rhof(k)*t1_qg_qc*Ef_ga*nwfa(k)*N0_g(k)           &
                        *ilamg(k)**cge(9)
          pna_gca(k) = MIN(DBLE(nwfa(k)*odts), pna_gca(k))

          Ef_ga = Eff_aero(xDg,0.8E-6,visco(k),rho(k),temp(k),'g')
          pnd_gcd(k) = rhof(k)*t1_qg_qc*Ef_ga*nifa(k)*N0_g(k)           &
                        *ilamg(k)**cge(9)
          pnd_gcd(k) = MIN(DBLE(nifa(k)*odts), pnd_gcd(k))
         endif

!..Rain collecting snow.  Cannot assume Wisner (1972) approximation
!.. or Mizuno (1990) approach so we solve the CE explicitly and store
!.. results in lookup table.
         if (rr(k).ge. r_r(1)) then
          if (rs(k).ge. r_s(1)) then
           if (temp(k).lt.T_0) then
            prr_rcs(k) = -(tmr_racs2(idx_s,idx_t,idx_r1,idx_r) &
                           + tcr_sacr2(idx_s,idx_t,idx_r1,idx_r) &
                           + tmr_racs1(idx_s,idx_t,idx_r1,idx_r) &
                           + tcr_sacr1(idx_s,idx_t,idx_r1,idx_r))
            prs_rcs(k) = tmr_racs2(idx_s,idx_t,idx_r1,idx_r) &
                         + tcr_sacr2(idx_s,idx_t,idx_r1,idx_r) &
                         - tcs_racs1(idx_s,idx_t,idx_r1,idx_r) &
                         - tms_sacr1(idx_s,idx_t,idx_r1,idx_r)
            prg_rcs(k) = tmr_racs1(idx_s,idx_t,idx_r1,idx_r) &
                         + tcr_sacr1(idx_s,idx_t,idx_r1,idx_r) &
                         + tcs_racs1(idx_s,idx_t,idx_r1,idx_r) &
                         + tms_sacr1(idx_s,idx_t,idx_r1,idx_r)
            prr_rcs(k) = MAX(DBLE(-rr(k)*odts), prr_rcs(k))
            prs_rcs(k) = MAX(DBLE(-rs(k)*odts), prs_rcs(k))
            prg_rcs(k) = MIN(DBLE((rr(k)+rs(k))*odts), prg_rcs(k))
            pnr_rcs(k) = tnr_racs1(idx_s,idx_t,idx_r1,idx_r)            &   ! RAIN2M
                         + tnr_racs2(idx_s,idx_t,idx_r1,idx_r)          &
                         + tnr_sacr1(idx_s,idx_t,idx_r1,idx_r)          &
                         + tnr_sacr2(idx_s,idx_t,idx_r1,idx_r)
           else
            prs_rcs(k) = -tcs_racs1(idx_s,idx_t,idx_r1,idx_r)           &
                         - tms_sacr1(idx_s,idx_t,idx_r1,idx_r)          &
                         + tmr_racs2(idx_s,idx_t,idx_r1,idx_r)          &
                         + tcr_sacr2(idx_s,idx_t,idx_r1,idx_r)
            prs_rcs(k) = MAX(DBLE(-rs(k)*odts), prs_rcs(k))
            prr_rcs(k) = -prs_rcs(k)
            pnr_rcs(k) = tnr_racs2(idx_s,idx_t,idx_r1,idx_r)            &   ! RAIN2M
                         + tnr_sacr2(idx_s,idx_t,idx_r1,idx_r)
           endif
           pnr_rcs(k) = MIN(DBLE(nr(k)*odts), pnr_rcs(k))
          endif

!..Rain collecting graupel.  Cannot assume Wisner (1972) approximation
!.. or Mizuno (1990) approach so we solve the CE explicitly and store
!.. results in lookup table.
          if (rg(k).ge. r_g(1)) then
           if (temp(k).lt.T_0) then
            prg_rcg(k) = tmr_racg(idx_g1,idx_g,idx_r1,idx_r) &
                         + tcr_gacr(idx_g1,idx_g,idx_r1,idx_r)
            prg_rcg(k) = MIN(DBLE(rr(k)*odts), prg_rcg(k))
            prr_rcg(k) = -prg_rcg(k)
            pnr_rcg(k) = tnr_racg(idx_g1,idx_g,idx_r1,idx_r)            &   ! RAIN2M
                         + tnr_gacr(idx_g1,idx_g,idx_r1,idx_r)
            pnr_rcg(k) = MIN(DBLE(nr(k)*odts), pnr_rcg(k))
           else
            prr_rcg(k) = tcg_racg(idx_g1,idx_g,idx_r1,idx_r)
            prr_rcg(k) = MIN(DBLE(rg(k)*odts), prr_rcg(k))
            prg_rcg(k) = -prr_rcg(k)
!..Put in explicit drop break-up due to collisions.
            pnr_rcg(k) = -5.*tnr_gacr(idx_g1,idx_g,idx_r1,idx_r)         ! RAIN2M
           endif
          endif
         endif

!+---+-----------------------------------------------------------------+
!..Next IF block handles only those processes below 0C.
!+---+-----------------------------------------------------------------+

         if (temp(k).lt.T_0) then

          vts_boost(k) = 1.0
          rate_max = (qv(k)-qvsi(k))*rho(k)*odts*0.999

!+---+---------------- BEGIN NEW ICE NUCLEATION -----------------------+
!..Freezing of supercooled water (rain or cloud) is influenced by dust
!.. but still using Bigg 1953 with a temperature adjustment of a few
!.. degrees depending on dust concentration.  A default value by way
!.. of idx_IN is 1.0 per Liter of air is used when dustyIce flag is
!.. false.  Next, a combination of deposition/condensation freezing
!.. using DeMott et al (2010) dust nucleation when water saturated or
!.. Phillips et al (2008) when below water saturation; else, without
!.. dustyIce flag, use the previous Cooper (1986) temperature-dependent
!.. value.  Lastly, allow homogeneous freezing of deliquesced aerosols
!.. following Koop et al. (2001, Nature).
!.. Implemented by T. Eidhammer and G. Thompson 2012Dec18
!+---+-----------------------------------------------------------------+

          if (dustyIce .AND. is_aerosol_aware) then
           xni = iceDeMott(tempc,qvs(k),qvs(k),qvsi(k),rho(k),nifa(k))
          else
           xni = 1.0 *1000.                                               ! Default is 1.0 per Liter
          endif

!..Ice nuclei lookup table index.
          if (xni.gt. Nt_IN(1)) then
           niin = NINT(ALOG10(xni))
           do nn = niin-1, niin+1
              n = nn
              if ( (xni/10.**nn).ge.1.0 .and. &
                   (xni/10.**nn).lt.10.0) goto 149
           enddo
 149       continue
           idx_IN = INT(xni/10.**n) + 10*(n-niin2) - (n-niin2)
           idx_IN = MAX(1, MIN(idx_IN, ntb_IN))
          else
           idx_IN = 1
          endif

!..Freezing of water drops into graupel/cloud ice (Bigg 1953).
          if (rr(k).gt. r_r(1)) then
           prg_rfz(k) = tpg_qrfz(idx_r,idx_r1,idx_tc,idx_IN)*odts
           pri_rfz(k) = tpi_qrfz(idx_r,idx_r1,idx_tc,idx_IN)*odts
           pni_rfz(k) = tni_qrfz(idx_r,idx_r1,idx_tc,idx_IN)*odts
           pnr_rfz(k) = tnr_qrfz(idx_r,idx_r1,idx_tc,idx_IN)*odts          ! RAIN2M
           pnr_rfz(k) = MIN(DBLE(nr(k)*odts), pnr_rfz(k))
          elseif (rr(k).gt. R1 .and. temp(k).lt.HGFR) then
           pri_rfz(k) = rr(k)*odts
           pnr_rfz(k) = nr(k)*odts                                         ! RAIN2M
           pni_rfz(k) = pnr_rfz(k)
          endif

          if (rc(k).gt. r_c(1)) then
           pri_wfz(k) = tpi_qcfz(idx_c,idx_n,idx_tc,idx_IN)*odts
           pri_wfz(k) = MIN(DBLE(rc(k)*odts), pri_wfz(k))
           pni_wfz(k) = tni_qcfz(idx_c,idx_n,idx_tc,idx_IN)*odts
           pni_wfz(k) = MIN(DBLE(nc(k)*odts), pri_wfz(k)/(2.*xm0i),     &
                                pni_wfz(k))
          elseif (rc(k).gt. R1 .and. temp(k).lt.HGFR) then
           pri_wfz(k) = rc(k)*odts
           pni_wfz(k) = nc(k)*odts
          endif

!..Deposition nucleation of dust/mineral from DeMott et al (2010)
!.. we may need to relax the temperature and ssati constraints.
          if ( (ssati(k).ge. 0.25) .or. (ssatw(k).gt. eps &
                                .and. temp(k).lt.261.15) ) then
           if (dustyIce .AND. is_aerosol_aware) then
            xnc = iceDeMott(tempc,qv(k),qvs(k),qvsi(k),rho(k),nifa(k))
           else
            xnc = MIN(250.E3, TNO*EXP(ATO*(T_0-temp(k))))
           endif
           xni = ni(k) + (pni_rfz(k)+pni_wfz(k))*dtsave
           pni_inu(k) = 0.5*(xnc-xni + abs(xnc-xni))*odts
           pri_inu(k) = MIN(DBLE(rate_max), xm0i*pni_inu(k))
           pni_inu(k) = pri_inu(k)/xm0i
          endif

!..Freezing of aqueous aerosols based on Koop et al (2001, Nature)
          xni = smo0(k)+ni(k) + (pni_rfz(k)+pni_wfz(k)+pni_inu(k))*dtsave
          if (is_aerosol_aware .AND. homogIce .AND. (xni.le.500.E3)     &
     &                .AND.(temp(k).lt.238).AND.(ssati(k).ge.0.4) ) then
            xnc = iceKoop(temp(k),qv(k),qvs(k),nwfa(k), dtsave)
            pni_iha(k) = xnc*odts
            pri_iha(k) = MIN(DBLE(rate_max), xm0i*0.1*pni_iha(k))
            pni_iha(k) = pri_iha(k)/(xm0i*0.1)
          endif
!+---+------------------ END NEW ICE NUCLEATION -----------------------+


!..Deposition/sublimation of cloud ice (Srivastava & Coen 1992).
          if (L_qi(k)) then
           lami = (am_i*cig(2)*oig1*ni(k)/ri(k))**obmi
           ilami = 1./lami
           xDi = MAX(DBLE(D0i), (bm_i + mu_i + 1.) * ilami)
           xmi = am_i*xDi**bm_i
           oxmi = 1./xmi
           pri_ide(k) = C_cube*t1_subl*diffu(k)*ssati(k)*rvs &
                  *oig1*cig(5)*ni(k)*ilami

           if (pri_ide(k) .lt. 0.0) then
            pri_ide(k) = MAX(DBLE(-ri(k)*odts), pri_ide(k), DBLE(rate_max))
            pni_ide(k) = pri_ide(k)*oxmi
            pni_ide(k) = MAX(DBLE(-ni(k)*odts), pni_ide(k))
           else
            pri_ide(k) = MIN(pri_ide(k), DBLE(rate_max))
            prs_ide(k) = (1.0D0-tpi_ide(idx_i,idx_i1))*pri_ide(k)
            pri_ide(k) = tpi_ide(idx_i,idx_i1)*pri_ide(k)
           endif

!..Some cloud ice needs to move into the snow category.  Use lookup
!.. table that resulted from explicit bin representation of distrib.
           if ( (idx_i.eq. ntb_i) .or. (xDi.gt. 5.0*D0s) ) then
            prs_iau(k) = ri(k)*.99*odts
            pni_iau(k) = ni(k)*.95*odts
           elseif (xDi.lt. 0.1*D0s) then
            prs_iau(k) = 0.
            pni_iau(k) = 0.
           else
            prs_iau(k) = tps_iaus(idx_i,idx_i1)*odts
            prs_iau(k) = MIN(DBLE(ri(k)*.99*odts), prs_iau(k))
            pni_iau(k) = tni_iaus(idx_i,idx_i1)*odts
            pni_iau(k) = MIN(DBLE(ni(k)*.95*odts), pni_iau(k))
           endif
          endif

!..Deposition/sublimation of snow/graupel follows Srivastava & Coen
!.. (1992).
          if (L_qs(k)) then
           C_snow = C_sqrd + (tempc+15.)*(C_cube-C_sqrd)/(-30.+15.)
           C_snow = MAX(C_sqrd, MIN(C_snow, C_cube))
           prs_sde(k) = C_snow*t1_subl*diffu(k)*ssati(k)*rvs &
                        * (t1_qs_sd*smo1(k) &
                         + t2_qs_sd*rhof2(k)*vsc2(k)*smof(k))
           if (prs_sde(k).lt. 0.) then
            prs_sde(k) = MAX(DBLE(-rs(k)*odts), prs_sde(k), DBLE(rate_max))
           else
            prs_sde(k) = MIN(prs_sde(k), DBLE(rate_max))
           endif
          endif

          if (L_qg(k) .and. ssati(k).lt. -eps) then
           prg_gde(k) = C_cube*t1_subl*diffu(k)*ssati(k)*rvs &
               * N0_g(k) * (t1_qg_sd*ilamg(k)**cge(10) &
               + t2_qg_sd*vsc2(k)*rhof2(k)*ilamg(k)**cge(11))
           if (prg_gde(k).lt. 0.) then
            prg_gde(k) = MAX(DBLE(-rg(k)*odts), prg_gde(k), DBLE(rate_max))
           else
            prg_gde(k) = MIN(prg_gde(k), DBLE(rate_max))
           endif
          endif

!..Snow collecting cloud ice.  In CE, assume Di<<Ds and vti=~0.
          if (L_qi(k)) then
           lami = (am_i*cig(2)*oig1*ni(k)/ri(k))**obmi
           ilami = 1./lami
           xDi = MAX(DBLE(D0i), (bm_i + mu_i + 1.) * ilami)
           xmi = am_i*xDi**bm_i
           oxmi = 1./xmi
           if (rs(k).ge. r_s(1)) then
            prs_sci(k) = t1_qs_qi*rhof(k)*Ef_si*ri(k)*smoe(k)
            pni_sci(k) = prs_sci(k) * oxmi
           endif

!..Rain collecting cloud ice.  In CE, assume Di<<Dr and vti=~0.
           if (rr(k).ge. r_r(1) .and. mvd_r(k).gt. 4.*xDi) then
            lamr = 1./ilamr(k)
            pri_rci(k) = rhof(k)*t1_qr_qi*Ef_ri*ri(k)*N0_r(k) &
                           *((lamr+fv_r)**(-cre(9)))
            pnr_rci(k) = rhof(k)*t1_qr_qi*Ef_ri*ni(k)*N0_r(k)           &   ! RAIN2M
                           *((lamr+fv_r)**(-cre(9)))
            pni_rci(k) = pri_rci(k) * oxmi
            prr_rci(k) = rhof(k)*t2_qr_qi*Ef_ri*ni(k)*N0_r(k) &
                           *((lamr+fv_r)**(-cre(8)))
            prr_rci(k) = MIN(DBLE(rr(k)*odts), prr_rci(k))
            prg_rci(k) = pri_rci(k) + prr_rci(k)
           endif
          endif

!..Ice multiplication from rime-splinters (Hallet & Mossop 1974).
          if (prg_gcw(k).gt. eps .and. tempc.gt.-8.0) then
           tf = 0.
           if (tempc.ge.-5.0 .and. tempc.lt.-3.0) then
            tf = 0.5*(-3.0 - tempc)
           elseif (tempc.gt.-8.0 .and. tempc.lt.-5.0) then
            tf = 0.33333333*(8.0 + tempc)
           endif
           pni_ihm(k) = 3.5E8*tf*prg_gcw(k)
           pri_ihm(k) = xm0i*pni_ihm(k)
           prs_ihm(k) = prs_scw(k)/(prs_scw(k)+prg_gcw(k)) &
                          * pri_ihm(k)
           prg_ihm(k) = prg_gcw(k)/(prs_scw(k)+prg_gcw(k)) &
                          * pri_ihm(k)
          endif

!..A portion of rimed snow converts to graupel but some remains snow.
!.. Interp from 5 to 75% as riming factor increases from 5.0 to 30.0
!.. 0.028 came from (.75-.05)/(30.-5.).  This remains ad-hoc and should
!.. be revisited.
          if (prs_scw(k).gt.5.0*prs_sde(k) .and. &
                         prs_sde(k).gt.eps) then
           r_frac = MIN(30.0D0, prs_scw(k)/prs_sde(k))
           g_frac = MIN(0.75, 0.05 + (r_frac-5.)*.028)
           vts_boost(k) = MIN(1.5, 1.1 + (r_frac-5.)*.016)
           prg_scw(k) = g_frac*prs_scw(k)
           prs_scw(k) = (1. - g_frac)*prs_scw(k)
          endif

         else

!..Melt snow and graupel and enhance from collisions with liquid.
!.. We also need to sublimate snow and graupel if subsaturated.
          if (L_qs(k)) then
           prr_sml(k) = (tempc*tcond(k)-lvap0*diffu(k)*delQvs(k))       &
                      * (t1_qs_me*smo1(k) + t2_qs_me*rhof2(k)*vsc2(k)*smof(k))
           prr_sml(k) = prr_sml(k) + 4218.*olfus*tempc &
                                   * (prr_rcs(k)+prs_scw(k))
           prr_sml(k) = MIN(DBLE(rs(k)*odts), MAX(0.D0, prr_sml(k)))
           pnr_sml(k) = smo0(k)/rs(k)*prr_sml(k) * 10.0**(-0.75*tempc)      ! RAIN2M
           pnr_sml(k) = MIN(DBLE(smo0(k)*odts), pnr_sml(k))
           if (tempc.gt.3.5 .or. rs(k).lt.0.005E-3) pnr_sml(k)=0.0

           if (ssati(k).lt. 0.) then
            prs_sde(k) = C_cube*t1_subl*diffu(k)*ssati(k)*rvs &
                         * (t1_qs_sd*smo1(k) &
                          + t2_qs_sd*rhof2(k)*vsc2(k)*smof(k))
            prs_sde(k) = MAX(DBLE(-rs(k)*odts), prs_sde(k))
           endif
          endif

          if (L_qg(k)) then
           prr_gml(k) = (tempc*tcond(k)-lvap0*diffu(k)*delQvs(k))       &
                      * N0_g(k)*(t1_qg_me*ilamg(k)**cge(10)             &
                      + t2_qg_me*rhof2(k)*vsc2(k)*ilamg(k)**cge(11))
!-GT       prr_gml(k) = prr_gml(k) + 4218.*olfus*tempc &
!-GT                               * (prr_rcg(k)+prg_gcw(k))
           prr_gml(k) = MIN(DBLE(rg(k)*odts), MAX(0.D0, prr_gml(k)))
           pnr_gml(k) = N0_g(k)*cgg(2)*ilamg(k)**cge(2) / rg(k)         &   ! RAIN2M
                      * prr_gml(k) * 10.0**(-0.25*tempc)
           if (tempc.gt.7.5 .or. rg(k).lt.0.005E-3) pnr_gml(k)=0.0

           if (ssati(k).lt. 0.) then
            prg_gde(k) = C_cube*t1_subl*diffu(k)*ssati(k)*rvs &
                * N0_g(k) * (t1_qg_sd*ilamg(k)**cge(10) &
                + t2_qg_sd*vsc2(k)*rhof2(k)*ilamg(k)**cge(11))
            prg_gde(k) = MAX(DBLE(-rg(k)*odts), prg_gde(k))
           endif
          endif

!.. This change will be required if users run adaptive time step that
!.. results in delta-t that is generally too long to allow cloud water
!.. collection by snow/graupel above melting temperature.
!.. Credit to Bjorn-Egil Nygaard for discovering.
          if (dt .gt. 120.) then
             prr_rcw(k)=prr_rcw(k)+prs_scw(k)+prg_gcw(k)
             prs_scw(k)=0.
             prg_gcw(k)=0.
          endif

         endif

      enddo
      endif

!+---+-----------------------------------------------------------------+
!..Ensure we do not deplete more hydrometeor species than exists.
!+---+-----------------------------------------------------------------+
      do k = kts, kte

!..If ice supersaturated, ensure sum of depos growth terms does not
!.. deplete more vapor than possibly exists.  If subsaturated, limit
!.. sum of sublimation terms such that vapor does not reproduce ice
!.. supersat again.
         sump = pri_inu(k) + pri_ide(k) + prs_ide(k) &
              + prs_sde(k) + prg_gde(k) + pri_iha(k)
         rate_max = (qv(k)-qvsi(k))*odts*0.999
         if ( (sump.gt. eps .and. sump.gt. rate_max) .or. &
              (sump.lt. -eps .and. sump.lt. rate_max) ) then
          ratio = rate_max/sump
          pri_inu(k) = pri_inu(k) * ratio
          pri_ide(k) = pri_ide(k) * ratio
          pni_ide(k) = pni_ide(k) * ratio
          prs_ide(k) = prs_ide(k) * ratio
          prs_sde(k) = prs_sde(k) * ratio
          prg_gde(k) = prg_gde(k) * ratio
          pri_iha(k) = pri_iha(k) * ratio
         endif

!..Cloud water conservation.
         sump = -prr_wau(k) - pri_wfz(k) - prr_rcw(k) &
                - prs_scw(k) - prg_scw(k) - prg_gcw(k)
         rate_max = -rc(k)*odts
         if (sump.lt. rate_max .and. L_qc(k)) then
          ratio = rate_max/sump
          prr_wau(k) = prr_wau(k) * ratio
          pri_wfz(k) = pri_wfz(k) * ratio
          prr_rcw(k) = prr_rcw(k) * ratio
          prs_scw(k) = prs_scw(k) * ratio
          prg_scw(k) = prg_scw(k) * ratio
          prg_gcw(k) = prg_gcw(k) * ratio
         endif

!..Cloud ice conservation.
         sump = pri_ide(k) - prs_iau(k) - prs_sci(k) &
                - pri_rci(k)
         rate_max = -ri(k)*odts
         if (sump.lt. rate_max .and. L_qi(k)) then
          ratio = rate_max/sump
          pri_ide(k) = pri_ide(k) * ratio
          prs_iau(k) = prs_iau(k) * ratio
          prs_sci(k) = prs_sci(k) * ratio
          pri_rci(k) = pri_rci(k) * ratio
         endif

!..Rain conservation.
         sump = -prg_rfz(k) - pri_rfz(k) - prr_rci(k) &
                + prr_rcs(k) + prr_rcg(k)
         rate_max = -rr(k)*odts
         if (sump.lt. rate_max .and. L_qr(k)) then
          ratio = rate_max/sump
          prg_rfz(k) = prg_rfz(k) * ratio
          pri_rfz(k) = pri_rfz(k) * ratio
          prr_rci(k) = prr_rci(k) * ratio
          prr_rcs(k) = prr_rcs(k) * ratio
          prr_rcg(k) = prr_rcg(k) * ratio
         endif

!..Snow conservation.
         sump = prs_sde(k) - prs_ihm(k) - prr_sml(k) &
                + prs_rcs(k)
         rate_max = -rs(k)*odts
         if (sump.lt. rate_max .and. L_qs(k)) then
          ratio = rate_max/sump
          prs_sde(k) = prs_sde(k) * ratio
          prs_ihm(k) = prs_ihm(k) * ratio
          prr_sml(k) = prr_sml(k) * ratio
          prs_rcs(k) = prs_rcs(k) * ratio
         endif

!..Graupel conservation.
         sump = prg_gde(k) - prg_ihm(k) - prr_gml(k) &
              + prg_rcg(k)
         rate_max = -rg(k)*odts
         if (sump.lt. rate_max .and. L_qg(k)) then
          ratio = rate_max/sump
          prg_gde(k) = prg_gde(k) * ratio
          prg_ihm(k) = prg_ihm(k) * ratio
          prr_gml(k) = prr_gml(k) * ratio
          prg_rcg(k) = prg_rcg(k) * ratio
         endif

!..Re-enforce proper mass conservation for subsequent elements in case
!.. any of the above terms were altered.  Thanks P. Blossey. 2009Sep28
         pri_ihm(k) = prs_ihm(k) + prg_ihm(k)
         ratio = MIN( ABS(prr_rcg(k)), ABS(prg_rcg(k)) )
         prr_rcg(k) = ratio * SIGN(1.0, SNGL(prr_rcg(k)))
         prg_rcg(k) = -prr_rcg(k)
         if (temp(k).gt.T_0) then
            ratio = MIN( ABS(prr_rcs(k)), ABS(prs_rcs(k)) )
            prr_rcs(k) = ratio * SIGN(1.0, SNGL(prr_rcs(k)))
            prs_rcs(k) = -prr_rcs(k)
         endif

      enddo

!+---+-----------------------------------------------------------------+
!..Calculate tendencies of all species but constrain the number of ice
!.. to reasonable values.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         orho = 1./rho(k)
         lfus2 = lsub - lvap(k)

!..Aerosol number tendency
         if (is_aerosol_aware) then
            nwfaten(k) = nwfaten(k) - (pna_rca(k) + pna_sca(k)          &
                       + pna_gca(k) + pni_iha(k)) * orho
            nifaten(k) = nifaten(k) - (pnd_rcd(k) + pnd_scd(k)          &
                       + pnd_gcd(k)) * orho
            if (dustyIce) then
               nifaten(k) = nifaten(k) - pni_inu(k)*orho
            else
               nifaten(k) = 0.
            endif
         endif

!..Water vapor tendency
         qvten(k) = qvten(k) + (-pri_inu(k) - pri_iha(k) - pri_ide(k)   &
                      - prs_ide(k) - prs_sde(k) - prg_gde(k)) &
                      * orho

!..Cloud water tendency
         qcten(k) = qcten(k) + (-prr_wau(k) - pri_wfz(k) &
                      - prr_rcw(k) - prs_scw(k) - prg_scw(k) &
                      - prg_gcw(k)) &
                      * orho

!..Cloud water number tendency
         ncten(k) = ncten(k) + (-pnc_wau(k) - pnc_rcw(k) &
                      - pni_wfz(k) - pnc_scw(k) - pnc_gcw(k)) &
                      * orho

!..Cloud water mass/number balance; keep mass-wt mean size between
!.. 1 and 50 microns.  Also no more than Nt_c_max drops total.
         xrc=MAX(R1, (qc1d(k) + qcten(k)*dtsave)*rho(k))
         xnc=MAX(2., (nc1d(k) + ncten(k)*dtsave)*rho(k))
         if (xrc .gt. R1) then
          nu_c = MIN(15, NINT(1000.E6/xnc) + 2)
          lamc = (xnc*am_r*ccg(2,nu_c)*ocg1(nu_c)/rc(k))**obmr
          xDc = (bm_r + nu_c + 1.) / lamc
          if (xDc.lt. D0c) then
           lamc = cce(2,nu_c)/D0c
           xnc = ccg(1,nu_c)*ocg2(nu_c)*xrc/am_r*lamc**bm_r
           ncten(k) = (xnc-nc1d(k)*rho(k))*odts*orho
          elseif (xDc.gt. D0r*2.) then
           lamc = cce(2,nu_c)/(D0r*2.)
           xnc = ccg(1,nu_c)*ocg2(nu_c)*xrc/am_r*lamc**bm_r
           ncten(k) = (xnc-nc1d(k)*rho(k))*odts*orho
          endif
         else
          ncten(k) = -nc1d(k)*odts
         endif
         xnc=MAX(0.,(nc1d(k) + ncten(k)*dtsave)*rho(k))
         if (xnc.gt.Nt_c_max) &
                ncten(k) = (Nt_c_max-nc1d(k)*rho(k))*odts*orho

!..Cloud ice mixing ratio tendency
         qiten(k) = qiten(k) + (pri_inu(k) + pri_iha(k) + pri_ihm(k)    &
                      + pri_wfz(k) + pri_rfz(k) + pri_ide(k) &
                      - prs_iau(k) - prs_sci(k) - pri_rci(k)) &
                      * orho

!..Cloud ice number tendency.
         niten(k) = niten(k) + (pni_inu(k) + pni_iha(k) + pni_ihm(k)    &
                      + pni_wfz(k) + pni_rfz(k) + pni_ide(k) &
                      - pni_iau(k) - pni_sci(k) - pni_rci(k)) &
                      * orho

!..Cloud ice mass/number balance; keep mass-wt mean size between
!.. 20 and 300 microns.  Also no more than 250 xtals per liter.
         xri=MAX(R1,(qi1d(k) + qiten(k)*dtsave)*rho(k))
         xni=MAX(R2,(ni1d(k) + niten(k)*dtsave)*rho(k))
         if (xri.gt. R1) then
           lami = (am_i*cig(2)*oig1*xni/xri)**obmi
           ilami = 1./lami
           xDi = (bm_i + mu_i + 1.) * ilami
           if (xDi.lt. 20.E-6) then
            lami = cie(2)/20.E-6
            xni = MIN(499.D3, cig(1)*oig2*xri/am_i*lami**bm_i)
            niten(k) = (xni-ni1d(k)*rho(k))*odts*orho
           elseif (xDi.gt. 300.E-6) then
            lami = cie(2)/300.E-6
            xni = cig(1)*oig2*xri/am_i*lami**bm_i
            niten(k) = (xni-ni1d(k)*rho(k))*odts*orho
           endif
         else
          niten(k) = -ni1d(k)*odts
         endif
         xni=MAX(0.,(ni1d(k) + niten(k)*dtsave)*rho(k))
         if (xni.gt.499.E3) &
                niten(k) = (499.E3-ni1d(k)*rho(k))*odts*orho

!..Rain tendency
         qrten(k) = qrten(k) + (prr_wau(k) + prr_rcw(k) &
                      + prr_sml(k) + prr_gml(k) + prr_rcs(k) &
                      + prr_rcg(k) - prg_rfz(k) &
                      - pri_rfz(k) - prr_rci(k)) &
                      * orho

!..Rain number tendency
         nrten(k) = nrten(k) + (pnr_wau(k) + pnr_sml(k) + pnr_gml(k)    &
                      - (pnr_rfz(k) + pnr_rcr(k) + pnr_rcg(k)           &
                      + pnr_rcs(k) + pnr_rci(k)) )                      &
                      * orho

!..Rain mass/number balance; keep median volume diameter between
!.. 37 microns (D0r*0.75) and 2.5 mm.
         xrr=MAX(R1,(qr1d(k) + qrten(k)*dtsave)*rho(k))
         xnr=MAX(R2,(nr1d(k) + nrten(k)*dtsave)*rho(k))
         if (xrr.gt. R1) then
           lamr = (am_r*crg(3)*org2*xnr/xrr)**obmr
           mvd_r(k) = (3.0 + mu_r + 0.672) / lamr
           if (mvd_r(k) .gt. 2.5E-3) then
              mvd_r(k) = 2.5E-3
              lamr = (3.0 + mu_r + 0.672) / mvd_r(k)
              xnr = crg(2)*org3*xrr*lamr**bm_r / am_r
              nrten(k) = (xnr-nr1d(k)*rho(k))*odts*orho
           elseif (mvd_r(k) .lt. D0r*0.75) then
              mvd_r(k) = D0r*0.75
              lamr = (3.0 + mu_r + 0.672) / mvd_r(k)
              xnr = crg(2)*org3*xrr*lamr**bm_r / am_r
              nrten(k) = (xnr-nr1d(k)*rho(k))*odts*orho
           endif
         else
           qrten(k) = -qr1d(k)*odts
           nrten(k) = -nr1d(k)*odts
         endif

!..Snow tendency
         qsten(k) = qsten(k) + (prs_iau(k) + prs_sde(k) &
                      + prs_sci(k) + prs_scw(k) + prs_rcs(k) &
                      + prs_ide(k) - prs_ihm(k) - prr_sml(k)) &
                      * orho

!..Graupel tendency
         qgten(k) = qgten(k) + (prg_scw(k) + prg_rfz(k) &
                      + prg_gde(k) + prg_rcg(k) + prg_gcw(k) &
                      + prg_rci(k) + prg_rcs(k) - prg_ihm(k) &
                      - prr_gml(k)) &
                      * orho

!..Temperature tendency
         if (temp(k).lt.T_0) then
          tten(k) = tten(k) &
                    + ( lsub*ocp(k)*(pri_inu(k) + pri_ide(k) &
                                     + prs_ide(k) + prs_sde(k) &
                                     + prg_gde(k) + pri_iha(k)) &
                     + lfus2*ocp(k)*(pri_wfz(k) + pri_rfz(k) &
                                     + prg_rfz(k) + prs_scw(k) &
                                     + prg_scw(k) + prg_gcw(k) &
                                     + prg_rcs(k) + prs_rcs(k) &
                                     + prr_rci(k) + prg_rcg(k)) &
                       )*orho * (1-IFDRY)
         else
          tten(k) = tten(k) &
                    + ( lfus*ocp(k)*(-prr_sml(k) - prr_gml(k) &
                                     - prr_rcg(k) - prr_rcs(k)) &
                      + lsub*ocp(k)*(prs_sde(k) + prg_gde(k)) &
                       )*orho * (1-IFDRY)
         endif

      enddo

!+---+-----------------------------------------------------------------+
!..Update variables for TAU+1 before condensation & sedimention.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         temp(k) = t1d(k) + DT*tten(k)
         otemp = 1./temp(k)
         tempc = temp(k) - 273.15
         qv(k) = MAX(1.E-10, qv1d(k) + DT*qvten(k))
         rho(k) = 0.622*pres(k)/(R*temp(k)*(qv(k)+0.622))
         rhof(k) = SQRT(RHO_NOT/rho(k))
         rhof2(k) = SQRT(rhof(k))
         qvs(k) = rslf(pres(k), temp(k))
         ssatw(k) = qv(k)/qvs(k) - 1.
         if (abs(ssatw(k)).lt. eps) ssatw(k) = 0.0
         diffu(k) = 2.11E-5*(temp(k)/273.15)**1.94 * (101325./pres(k))
         if (tempc .ge. 0.0) then
            visco(k) = (1.718+0.0049*tempc)*1.0E-5
         else
            visco(k) = (1.718+0.0049*tempc-1.2E-5*tempc*tempc)*1.0E-5
         endif
         vsc2(k) = SQRT(rho(k)/visco(k))
         lvap(k) = lvap0 + (2106.0 - 4218.0)*tempc
         tcond(k) = (5.69 + 0.0168*tempc)*1.0E-5 * 418.936
         ocp(k) = 1./(Cp*(1.+0.887*qv(k)))
         lvt2(k)=lvap(k)*lvap(k)*ocp(k)*oRv*otemp*otemp

         nwfa(k) = MAX(11.1E6, (nwfa1d(k) + nwfaten(k)*DT)*rho(k))

         if ((qc1d(k) + qcten(k)*DT) .gt. R1) then
            rc(k) = (qc1d(k) + qcten(k)*DT)*rho(k)
            nc(k) = MAX(2., (nc1d(k) + ncten(k)*DT)*rho(k))
            if (.NOT. is_aerosol_aware) nc(k) = Nt_c
            L_qc(k) = .true.
         else
            rc(k) = R1
            nc(k) = 2.
            L_qc(k) = .false.
         endif

         if ((qi1d(k) + qiten(k)*DT) .gt. R1) then
            ri(k) = (qi1d(k) + qiten(k)*DT)*rho(k)
            ni(k) = MAX(R2, (ni1d(k) + niten(k)*DT)*rho(k))
            L_qi(k) = .true. 
         else
            ri(k) = R1
            ni(k) = R2
            L_qi(k) = .false.
         endif

         if ((qr1d(k) + qrten(k)*DT) .gt. R1) then
            rr(k) = (qr1d(k) + qrten(k)*DT)*rho(k)
            nr(k) = MAX(R2, (nr1d(k) + nrten(k)*DT)*rho(k))
            L_qr(k) = .true.
            lamr = (am_r*crg(3)*org2*nr(k)/rr(k))**obmr
            mvd_r(k) = (3.0 + mu_r + 0.672) / lamr
            if (mvd_r(k) .gt. 2.5E-3) then
               mvd_r(k) = 2.5E-3
               lamr = (3.0 + mu_r + 0.672) / mvd_r(k)
               nr(k) = crg(2)*org3*rr(k)*lamr**bm_r / am_r
            elseif (mvd_r(k) .lt. D0r*0.75) then
               mvd_r(k) = D0r*0.75
               lamr = (3.0 + mu_r + 0.672) / mvd_r(k)
               nr(k) = crg(2)*org3*rr(k)*lamr**bm_r / am_r
            endif
         else
            rr(k) = R1
            nr(k) = R2
            L_qr(k) = .false.
         endif
               
         if ((qs1d(k) + qsten(k)*DT) .gt. R1) then
            rs(k) = (qs1d(k) + qsten(k)*DT)*rho(k)
            L_qs(k) = .true.
         else
            rs(k) = R1
            L_qs(k) = .false.
         endif

         if ((qg1d(k) + qgten(k)*DT) .gt. R1) then
            rg(k) = (qg1d(k) + qgten(k)*DT)*rho(k)
            L_qg(k) = .true.
         else
            rg(k) = R1
            L_qg(k) = .false.
         endif
      enddo

!+---+-----------------------------------------------------------------+
!..With tendency-updated mixing ratios, recalculate snow moments and
!.. intercepts/slopes of graupel and rain.
!+---+-----------------------------------------------------------------+
      if (.not. iiwarm) then
      do k = kts, kte
         if (.not. L_qs(k)) CYCLE
         tc0 = MIN(-0.1, temp(k)-273.15)
         smob(k) = rs(k)*oams

!..All other moments based on reference, 2nd moment.  If bm_s.ne.2,
!.. then we must compute actual 2nd moment and use as reference.
         if (bm_s.gt.(2.0-1.e-3) .and. bm_s.lt.(2.0+1.e-3)) then
            smo2(k) = smob(k)
         else
            loga_ = sa(1) + sa(2)*tc0 + sa(3)*bm_s &
               + sa(4)*tc0*bm_s + sa(5)*tc0*tc0 &
               + sa(6)*bm_s*bm_s + sa(7)*tc0*tc0*bm_s &
               + sa(8)*tc0*bm_s*bm_s + sa(9)*tc0*tc0*tc0 &
               + sa(10)*bm_s*bm_s*bm_s
            a_ = 10.0**loga_
            b_ = sb(1) + sb(2)*tc0 + sb(3)*bm_s &
               + sb(4)*tc0*bm_s + sb(5)*tc0*tc0 &
               + sb(6)*bm_s*bm_s + sb(7)*tc0*tc0*bm_s &
               + sb(8)*tc0*bm_s*bm_s + sb(9)*tc0*tc0*tc0 &
               + sb(10)*bm_s*bm_s*bm_s
            smo2(k) = (smob(k)/a_)**(1./b_)
         endif

!..Calculate bm_s+1 (th) moment.  Useful for diameter calcs.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(1) &
               + sa(4)*tc0*cse(1) + sa(5)*tc0*tc0 &
               + sa(6)*cse(1)*cse(1) + sa(7)*tc0*tc0*cse(1) &
               + sa(8)*tc0*cse(1)*cse(1) + sa(9)*tc0*tc0*tc0 &
               + sa(10)*cse(1)*cse(1)*cse(1)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(1) + sb(4)*tc0*cse(1) &
              + sb(5)*tc0*tc0 + sb(6)*cse(1)*cse(1) &
              + sb(7)*tc0*tc0*cse(1) + sb(8)*tc0*cse(1)*cse(1) &
              + sb(9)*tc0*tc0*tc0 + sb(10)*cse(1)*cse(1)*cse(1)
         smoc(k) = a_ * smo2(k)**b_

!..Calculate bm_s+bv_s (th) moment.  Useful for sedimentation.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(14) &
               + sa(4)*tc0*cse(14) + sa(5)*tc0*tc0 &
               + sa(6)*cse(14)*cse(14) + sa(7)*tc0*tc0*cse(14) &
               + sa(8)*tc0*cse(14)*cse(14) + sa(9)*tc0*tc0*tc0 &
               + sa(10)*cse(14)*cse(14)*cse(14)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(14) + sb(4)*tc0*cse(14) &
              + sb(5)*tc0*tc0 + sb(6)*cse(14)*cse(14) &
              + sb(7)*tc0*tc0*cse(14) + sb(8)*tc0*cse(14)*cse(14) &
              + sb(9)*tc0*tc0*tc0 + sb(10)*cse(14)*cse(14)*cse(14)
         smod(k) = a_ * smo2(k)**b_
      enddo

!+---+-----------------------------------------------------------------+
!..Calculate y-intercept, slope values for graupel.
!+---+-----------------------------------------------------------------+
      N0_min = gonv_max
      do k = kte, kts, -1
         if (temp(k).lt.270.65 .and. L_qr(k) .and. mvd_r(k).gt.100.E-6) then
            xslw1 = 4.01 + alog10(mvd_r(k))
         else
            xslw1 = 0.01
         endif
         ygra1 = 4.31 + alog10(max(5.E-5, rg(k)))
         zans1 = 3.1 + (100./(300.*xslw1*ygra1/(10./xslw1+1.+0.25*ygra1)+30.+10.*ygra1))
         N0_exp = 10.**(zans1)
         N0_exp = MAX(DBLE(gonv_min), MIN(N0_exp, DBLE(gonv_max)))
         N0_min = MIN(N0_exp, N0_min)
         N0_exp = N0_min
         lam_exp = (N0_exp*am_g*cgg(1)/rg(k))**oge1
         lamg = lam_exp * (cgg(3)*ogg2*ogg1)**obmg
         ilamg(k) = 1./lamg
         N0_g(k) = N0_exp/(cgg(2)*lam_exp) * lamg**cge(2)
      enddo

      endif

!+---+-----------------------------------------------------------------+
!..Calculate y-intercept, slope values for rain.
!+---+-----------------------------------------------------------------+
      do k = kte, kts, -1
         lamr = (am_r*crg(3)*org2*nr(k)/rr(k))**obmr
         ilamr(k) = 1./lamr
         mvd_r(k) = (3.0 + mu_r + 0.672) / lamr
         N0_r(k) = nr(k)*org2*lamr**cre(2)
      enddo

!+---+-----------------------------------------------------------------+
!..Cloud water condensation and evaporation.  Nucleate cloud droplets
!.. using explicit CCN aerosols with hygroscopicity like sulfates using
!.. parcel model lookup table results provided by T. Eidhammer.  Evap
!.. drops using calculation of max drop size capable of evaporating in
!.. single timestep and explicit number of drops smaller than Dc_star
!.. from lookup table.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         orho = 1./rho(k)
         if ( (ssatw(k).gt. eps) .or. (ssatw(k).lt. -eps .and. &
                   L_qc(k)) ) then
          clap = (qv(k)-qvs(k))/(1. + lvt2(k)*qvs(k))
          do n = 1, 3
             fcd = qvs(k)* EXP(lvt2(k)*clap) - qv(k) + clap
             dfcd = qvs(k)*lvt2(k)* EXP(lvt2(k)*clap) + 1.
             clap = clap - fcd/dfcd
          enddo
          xrc = rc(k) + clap*rho(k)
          xnc = 0.
          if (xrc.gt. R1) then
           prw_vcd(k) = clap*odt
!+---+-----------------------------------------------------------------+ !  DROPLET NUCLEATION
           if (clap .gt. eps) then
            if (is_aerosol_aware) then
               xnc = MAX(2., activ_ncloud(temp(k), w1d(k), nwfa(k)))
            else
               xnc = Nt_c
            endif
            pnc_wcd(k) = 0.5*(xnc-nc(k) + abs(xnc-nc(k)))*odts*orho

!+---+-----------------------------------------------------------------+ !  EVAPORATION
           elseif (clap .lt. -eps .AND. ssatw(k).lt.-1.E-6 .AND. is_aerosol_aware) then
            tempc = temp(k) - 273.15
            otemp = 1./temp(k)
            rvs = rho(k)*qvs(k)
            rvs_p = rvs*otemp*(lvap(k)*otemp*oRv - 1.)
            rvs_pp = rvs * ( otemp*(lvap(k)*otemp*oRv - 1.) &
                            *otemp*(lvap(k)*otemp*oRv - 1.) &
                            + (-2.*lvap(k)*otemp*otemp*otemp*oRv) &
                            + otemp*otemp)
            gamsc = lvap(k)*diffu(k)/tcond(k) * rvs_p
            alphsc = 0.5*(gamsc/(1.+gamsc))*(gamsc/(1.+gamsc)) &
                       * rvs_pp/rvs_p * rvs/rvs_p
            alphsc = MAX(1.E-9, alphsc)
            xsat = ssatw(k)
            if (abs(xsat).lt. 1.E-9) xsat=0.
            t1_evap = 2.*PI*( 1.0 - alphsc*xsat  &
                   + 2.*alphsc*alphsc*xsat*xsat  &
                   - 5.*alphsc*alphsc*alphsc*xsat*xsat*xsat ) &
                   / (1.+gamsc)

            Dc_star = DSQRT(-2.D0*DT * t1_evap/(2.*PI) &
                    * 4.*diffu(k)*ssatw(k)*rvs/rho_w)
            idx_d = MAX(1, MIN(INT(1.E6*Dc_star), nbc))

            idx_n = NINT(1.0 + FLOAT(nbc) * DLOG(nc(k)/t_Nc(1)) / nic1)
            idx_n = MAX(1, MIN(idx_n, nbc))

!..Cloud water lookup table index.
            if (rc(k).gt. r_c(1)) then
             nic = NINT(ALOG10(rc(k)))
             do nn = nic-1, nic+1
                n = nn
                if ( (rc(k)/10.**nn).ge.1.0 .and. &
                     (rc(k)/10.**nn).lt.10.0) goto 159
             enddo
 159         continue
             idx_c = INT(rc(k)/10.**n) + 10*(n-nic2) - (n-nic2)
             idx_c = MAX(1, MIN(idx_c, ntb_c))
            else
             idx_c = 1
            endif

           !prw_vcd(k) = MAX(DBLE(-rc(k)*orho*odt),                     &
           !           -tpc_wev(idx_d, idx_c, idx_n)*orho*odt)
            prw_vcd(k) = MAX(DBLE(-rc(k)*0.99*orho*odt), prw_vcd(k))
            pnc_wcd(k) = MAX(DBLE(-nc(k)*0.99*orho*odt),                &
                       -tnc_wev(idx_d, idx_c, idx_n)*orho*odt)

           endif
          else
           prw_vcd(k) = -rc(k)*orho*odt
           pnc_wcd(k) = -nc(k)*orho*odt
          endif

!+---+-----------------------------------------------------------------+

          qvten(k) = qvten(k) - prw_vcd(k)
          qcten(k) = qcten(k) + prw_vcd(k)
          ncten(k) = ncten(k) + pnc_wcd(k)
          nwfaten(k) = nwfaten(k) - pnc_wcd(k)
          tten(k) = tten(k) + lvap(k)*ocp(k)*prw_vcd(k)*(1-IFDRY)
          rc(k) = MAX(R1, (qc1d(k) + DT*qcten(k))*rho(k))
          nc(k) = MAX(2., (nc1d(k) + DT*ncten(k))*rho(k))
          if (.NOT. is_aerosol_aware) nc(k) = Nt_c
          qv(k) = MAX(1.E-10, qv1d(k) + DT*qvten(k))
          temp(k) = t1d(k) + DT*tten(k)
          rho(k) = 0.622*pres(k)/(R*temp(k)*(qv(k)+0.622))
          qvs(k) = rslf(pres(k), temp(k))
          ssatw(k) = qv(k)/qvs(k) - 1.
         endif
      enddo

!+---+-----------------------------------------------------------------+
!.. If still subsaturated, allow rain to evaporate, following
!.. Srivastava & Coen (1992).
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         if ( (ssatw(k).lt. -eps) .and. L_qr(k) &
                     .and. (.not.(prw_vcd(k).gt. 0.)) ) then
          tempc = temp(k) - 273.15
          otemp = 1./temp(k)
          orho = 1./rho(k)
          rhof(k) = SQRT(RHO_NOT*orho)
          rhof2(k) = SQRT(rhof(k))
          diffu(k) = 2.11E-5*(temp(k)/273.15)**1.94 * (101325./pres(k))
          if (tempc .ge. 0.0) then
             visco(k) = (1.718+0.0049*tempc)*1.0E-5
          else
             visco(k) = (1.718+0.0049*tempc-1.2E-5*tempc*tempc)*1.0E-5
          endif
          vsc2(k) = SQRT(rho(k)/visco(k))
          lvap(k) = lvap0 + (2106.0 - 4218.0)*tempc
          tcond(k) = (5.69 + 0.0168*tempc)*1.0E-5 * 418.936
          ocp(k) = 1./(Cp*(1.+0.887*qv(k)))

          rvs = rho(k)*qvs(k)
          rvs_p = rvs*otemp*(lvap(k)*otemp*oRv - 1.)
          rvs_pp = rvs * ( otemp*(lvap(k)*otemp*oRv - 1.) &
                          *otemp*(lvap(k)*otemp*oRv - 1.) &
                          + (-2.*lvap(k)*otemp*otemp*otemp*oRv) &
                          + otemp*otemp)
          gamsc = lvap(k)*diffu(k)/tcond(k) * rvs_p
          alphsc = 0.5*(gamsc/(1.+gamsc))*(gamsc/(1.+gamsc)) &
                     * rvs_pp/rvs_p * rvs/rvs_p
          alphsc = MAX(1.E-9, alphsc)
          xsat   = MIN(-1.E-9, ssatw(k))
          t1_evap = 2.*PI*( 1.0 - alphsc*xsat  &
                 + 2.*alphsc*alphsc*xsat*xsat  &
                 - 5.*alphsc*alphsc*alphsc*xsat*xsat*xsat ) &
                 / (1.+gamsc)

          lamr = 1./ilamr(k)
!..Rapidly eliminate near zero values when low humidity (<95%)
          if (qv(k)/qvs(k) .lt. 0.95 .AND. rr(k)*orho.le.1.E-8) then
          prv_rev(k) = rr(k)*orho*odts
          else
          prv_rev(k) = t1_evap*diffu(k)*(-ssatw(k))*N0_r(k)*rvs &
              * (t1_qr_ev*ilamr(k)**cre(10) &
              + t2_qr_ev*vsc2(k)*rhof2(k)*((lamr+0.5*fv_r)**(-cre(11))))
          rate_max = MIN((rr(k)*orho*odts), (qvs(k)-qv(k))*odts)
          prv_rev(k) = MIN(DBLE(rate_max), prv_rev(k)*orho)

!..TEST: G. Thompson  10 May 2013
!..Reduce the rain evaporation in same places as melting graupel occurs. 
!..Rationale: falling and simultaneous melting graupel in subsaturated
!..regions will not melt as fast because particle temperature stays
!..at 0C.  Also not much shedding of the water from the graupel so
!..likely that the water-coated graupel evaporating much slower than
!..if the water was immediately shed off.
          IF (prr_gml(k).gt.0.0) THEN
             eva_factor = MIN(1.0, 0.01+(0.99-0.01)*(tempc/20.0))
             prv_rev(k) = prv_rev(k)*eva_factor
          ENDIF
          endif

          pnr_rev(k) = MIN(DBLE(nr(k)*0.99*orho*odts),                  &   ! RAIN2M
                       prv_rev(k) * nr(k)/rr(k))

          qrten(k) = qrten(k) - prv_rev(k)
          qvten(k) = qvten(k) + prv_rev(k)
          nrten(k) = nrten(k) - pnr_rev(k)
          nwfaten(k) = nwfaten(k) + pnr_rev(k)
          tten(k) = tten(k) - lvap(k)*ocp(k)*prv_rev(k)*(1-IFDRY)

          rr(k) = MAX(R1, (qr1d(k) + DT*qrten(k))*rho(k))
          qv(k) = MAX(1.E-10, qv1d(k) + DT*qvten(k))
          nr(k) = MAX(R2, (nr1d(k) + DT*nrten(k))*rho(k))
          temp(k) = t1d(k) + DT*tten(k)
          rho(k) = 0.622*pres(k)/(R*temp(k)*(qv(k)+0.622))
         endif
      enddo
#if ( WRF_CHEM == 1 )
      do k = kts, kte
         evapprod(k) = prv_rev(k) - (min(zeroD0,prs_sde(k)) + &
                                     min(zeroD0,prg_gde(k)))
         rainprod(k) = prr_wau(k) + prr_rcw(k) + prs_scw(k) + &
                                    prg_scw(k) + prs_iau(k) + &
                                    prg_gcw(k) + prs_sci(k) + &
                                    pri_rci(k)
      enddo
#endif

!+---+-----------------------------------------------------------------+
!..Find max terminal fallspeed (distribution mass-weighted mean
!.. velocity) and use it to determine if we need to split the timestep
!.. (var nstep>1).  Either way, only bother to do sedimentation below
!.. 1st level that contains any sedimenting particles (k=ksed1 on down).
!.. New in v3.0+ is computing separate for rain, ice, snow, and
!.. graupel species thus making code faster with credit to J. Schmidt.
!+---+-----------------------------------------------------------------+
      nstep = 0
      onstep(:) = 1.0
      ksed1(:) = 1
      do k = kte+1, kts, -1
         vtrk(k) = 0.
         vtnrk(k) = 0.
         vtik(k) = 0.
         vtnik(k) = 0.
         vtsk(k) = 0.
         vtgk(k) = 0.
         vtck(k) = 0.
         vtnck(k) = 0.
      enddo
      do k = kte, kts, -1
         vtr = 0.
         rhof(k) = SQRT(RHO_NOT/rho(k))

         if (rr(k).gt. R1) then
          lamr = (am_r*crg(3)*org2*nr(k)/rr(k))**obmr
          vtr = rhof(k)*av_r*crg(6)*org3 * lamr**cre(3)                 &
                      *((lamr+fv_r)**(-cre(6)))
          vtrk(k) = vtr
! First below is technically correct:
!         vtr = rhof(k)*av_r*crg(5)*org2 * lamr**cre(2)                 &
!                     *((lamr+fv_r)**(-cre(5)))
! Test: make number fall faster (but still slower than mass)
! Goal: less prominent size sorting
          vtr = rhof(k)*av_r*crg(7)/crg(12) * lamr**cre(12)             &
                      *((lamr+fv_r)**(-cre(7)))
          vtnrk(k) = vtr
         else
          vtrk(k) = vtrk(k+1)
          vtnrk(k) = vtnrk(k+1)
         endif

         if (MAX(vtrk(k),vtnrk(k)) .gt. 1.E-3) then
            ksed1(1) = MAX(ksed1(1), k)
            delta_tp = dzq(k)/(MAX(vtrk(k),vtnrk(k)))
            nstep = MAX(nstep, INT(DT/delta_tp + 1.))
         endif
      enddo
      if (ksed1(1) .eq. kte) ksed1(1) = kte-1
      if (nstep .gt. 0) onstep(1) = 1./REAL(nstep)

!+---+-----------------------------------------------------------------+

      hgt_agl = 0.
      do k = kts, kte-1
         if (rc(k) .gt. R2) ksed1(5) = k
         hgt_agl = hgt_agl + dzq(k)
         if (hgt_agl .gt. 500.0) goto 151
      enddo
 151  continue

      do k = ksed1(5), kts, -1
         vtc = 0.
         if (rc(k) .gt. R1 .and. w1d(k) .lt. 1.E-1) then
          nu_c = MIN(15, NINT(1000.E6/nc(k)) + 2)
          lamc = (nc(k)*am_r*ccg(2,nu_c)*ocg1(nu_c)/rc(k))**obmr
          ilamc = 1./lamc
          vtc = rhof(k)*av_c*ccg(5,nu_c)*ocg2(nu_c) * ilamc**bv_c
          vtck(k) = vtc
          vtc = rhof(k)*av_c*ccg(4,nu_c)*ocg1(nu_c) * ilamc**bv_c
          vtnck(k) = vtc
         endif
      enddo

!+---+-----------------------------------------------------------------+

      if (.not. iiwarm) then

       nstep = 0
       do k = kte, kts, -1
          vti = 0.

          if (ri(k).gt. R1) then
           lami = (am_i*cig(2)*oig1*ni(k)/ri(k))**obmi
           ilami = 1./lami
           vti = rhof(k)*av_i*cig(3)*oig2 * ilami**bv_i
           vtik(k) = vti
! First below is technically correct:
!          vti = rhof(k)*av_i*cig(4)*oig1 * ilami**bv_i
! Goal: less prominent size sorting
           vti = rhof(k)*av_i*cig(6)/cig(7) * ilami**bv_i
           vtnik(k) = vti
          else
           vtik(k) = vtik(k+1)
           vtnik(k) = vtnik(k+1)
          endif

          if (vtik(k) .gt. 1.E-3) then
             ksed1(2) = MAX(ksed1(2), k)
             delta_tp = dzq(k)/vtik(k)
             nstep = MAX(nstep, INT(DT/delta_tp + 1.))
          endif
       enddo
       if (ksed1(2) .eq. kte) ksed1(2) = kte-1
       if (nstep .gt. 0) onstep(2) = 1./REAL(nstep)

!+---+-----------------------------------------------------------------+

       nstep = 0
       do k = kte, kts, -1
          vts = 0.

          if (rs(k).gt. R1) then
           xDs = smoc(k) / smob(k)
           Mrat = 1./xDs
           ils1 = 1./(Mrat*Lam0 + fv_s)
           ils2 = 1./(Mrat*Lam1 + fv_s)
           t1_vts = Kap0*csg(4)*ils1**cse(4)
           t2_vts = Kap1*Mrat**mu_s*csg(10)*ils2**cse(10)
           ils1 = 1./(Mrat*Lam0)
           ils2 = 1./(Mrat*Lam1)
           t3_vts = Kap0*csg(1)*ils1**cse(1)
           t4_vts = Kap1*Mrat**mu_s*csg(7)*ils2**cse(7)
           vts = rhof(k)*av_s * (t1_vts+t2_vts)/(t3_vts+t4_vts)
           if (temp(k).gt. T_0) then
            vtsk(k) = MAX(vts*vts_boost(k), vtrk(k))
           else
            vtsk(k) = vts*vts_boost(k)
           endif
          else
            vtsk(k) = vtsk(k+1)
          endif

          if (vtsk(k) .gt. 1.E-3) then
             ksed1(3) = MAX(ksed1(3), k)
             delta_tp = dzq(k)/vtsk(k)
             nstep = MAX(nstep, INT(DT/delta_tp + 1.))
          endif
       enddo
       if (ksed1(3) .eq. kte) ksed1(3) = kte-1
       if (nstep .gt. 0) onstep(3) = 1./REAL(nstep)

!+---+-----------------------------------------------------------------+

       nstep = 0
       do k = kte, kts, -1
          vtg = 0.

          if (rg(k).gt. R1) then
           vtg = rhof(k)*av_g*cgg(6)*ogg3 * ilamg(k)**bv_g
           if (temp(k).gt. T_0) then
            vtgk(k) = MAX(vtg, vtrk(k))
           else
            vtgk(k) = vtg
           endif
          else
            vtgk(k) = vtgk(k+1)
          endif

          if (vtgk(k) .gt. 1.E-3) then
             ksed1(4) = MAX(ksed1(4), k)
             delta_tp = dzq(k)/vtgk(k)
             nstep = MAX(nstep, INT(DT/delta_tp + 1.))
          endif
       enddo
       if (ksed1(4) .eq. kte) ksed1(4) = kte-1
       if (nstep .gt. 0) onstep(4) = 1./REAL(nstep)
      endif

!+---+-----------------------------------------------------------------+
!..Sedimentation of mixing ratio is the integral of v(D)*m(D)*N(D)*dD,
!.. whereas neglect m(D) term for number concentration.  Therefore,
!.. cloud ice has proper differential sedimentation.
!.. New in v3.0+ is computing separate for rain, ice, snow, and
!.. graupel species thus making code faster with credit to J. Schmidt.
!.. Bug fix, 2013Nov01 to tendencies using rho(k+1) correction thanks to
!.. Eric Skyllingstad.
!+---+-----------------------------------------------------------------+

      nstep = NINT(1./onstep(1))
      do n = 1, nstep
         do k = kte, kts, -1
            sed_r(k) = vtrk(k)*rr(k)
            sed_n(k) = vtnrk(k)*nr(k)
         enddo
         k = kte
         odzq = 1./dzq(k)
         orho = 1./rho(k)
         qrten(k) = qrten(k) - sed_r(k)*odzq*onstep(1)*orho
         nrten(k) = nrten(k) - sed_n(k)*odzq*onstep(1)*orho
         rr(k) = MAX(R1, rr(k) - sed_r(k)*odzq*DT*onstep(1))
         nr(k) = MAX(R2, nr(k) - sed_n(k)*odzq*DT*onstep(1))
         do k = ksed1(1), kts, -1
            odzq = 1./dzq(k)
            orho = 1./rho(k)
            qrten(k) = qrten(k) + (sed_r(k+1)-sed_r(k))                 &
                                               *odzq*onstep(1)*orho
            nrten(k) = nrten(k) + (sed_n(k+1)-sed_n(k))                 &
                                               *odzq*onstep(1)*orho
            rr(k) = MAX(R1, rr(k) + (sed_r(k+1)-sed_r(k)) &
                                           *odzq*DT*onstep(1))
            nr(k) = MAX(R2, nr(k) + (sed_n(k+1)-sed_n(k)) &
                                           *odzq*DT*onstep(1))
         enddo

         if (rr(kts).gt.R1*10.) &
         pptrain = pptrain + sed_r(kts)*DT*onstep(1)
      enddo

!+---+-----------------------------------------------------------------+

      do k = kte, kts, -1
         sed_c(k) = vtck(k)*rc(k)
         sed_n(k) = vtnck(k)*nc(k)
      enddo
      do k = ksed1(5), kts, -1
         odzq = 1./dzq(k)
         orho = 1./rho(k)
         qcten(k) = qcten(k) + (sed_c(k+1)-sed_c(k)) *odzq*orho
         ncten(k) = ncten(k) + (sed_n(k+1)-sed_n(k)) *odzq*orho
         rc(k) = MAX(R1, rc(k) + (sed_c(k+1)-sed_c(k)) *odzq*DT)
         nc(k) = MAX(10., nc(k) + (sed_n(k+1)-sed_n(k)) *odzq*DT)
      enddo

!+---+-----------------------------------------------------------------+

      nstep = NINT(1./onstep(2))
      do n = 1, nstep
         do k = kte, kts, -1
            sed_i(k) = vtik(k)*ri(k)
            sed_n(k) = vtnik(k)*ni(k)
         enddo
         k = kte
         odzq = 1./dzq(k)
         orho = 1./rho(k)
         qiten(k) = qiten(k) - sed_i(k)*odzq*onstep(2)*orho
         niten(k) = niten(k) - sed_n(k)*odzq*onstep(2)*orho
         ri(k) = MAX(R1, ri(k) - sed_i(k)*odzq*DT*onstep(2))
         ni(k) = MAX(R2, ni(k) - sed_n(k)*odzq*DT*onstep(2))
         do k = ksed1(2), kts, -1
            odzq = 1./dzq(k)
            orho = 1./rho(k)
            qiten(k) = qiten(k) + (sed_i(k+1)-sed_i(k))                 &
                                               *odzq*onstep(2)*orho
            niten(k) = niten(k) + (sed_n(k+1)-sed_n(k))                 &
                                               *odzq*onstep(2)*orho
            ri(k) = MAX(R1, ri(k) + (sed_i(k+1)-sed_i(k)) &
                                           *odzq*DT*onstep(2))
            ni(k) = MAX(R2, ni(k) + (sed_n(k+1)-sed_n(k)) &
                                           *odzq*DT*onstep(2))
         enddo

         if (ri(kts).gt.R1*10.) &
         pptice = pptice + sed_i(kts)*DT*onstep(2)
      enddo

!+---+-----------------------------------------------------------------+

      nstep = NINT(1./onstep(3))
      do n = 1, nstep
         do k = kte, kts, -1
            sed_s(k) = vtsk(k)*rs(k)
         enddo
         k = kte
         odzq = 1./dzq(k)
         orho = 1./rho(k)
         qsten(k) = qsten(k) - sed_s(k)*odzq*onstep(3)*orho
         rs(k) = MAX(R1, rs(k) - sed_s(k)*odzq*DT*onstep(3))
         do k = ksed1(3), kts, -1
            odzq = 1./dzq(k)
            orho = 1./rho(k)
            qsten(k) = qsten(k) + (sed_s(k+1)-sed_s(k))                 &
                                               *odzq*onstep(3)*orho
            rs(k) = MAX(R1, rs(k) + (sed_s(k+1)-sed_s(k)) &
                                           *odzq*DT*onstep(3))
         enddo

         if (rs(kts).gt.R1*10.) &
         pptsnow = pptsnow + sed_s(kts)*DT*onstep(3)
      enddo

!+---+-----------------------------------------------------------------+

      nstep = NINT(1./onstep(4))
      do n = 1, nstep
         do k = kte, kts, -1
            sed_g(k) = vtgk(k)*rg(k)
         enddo
         k = kte
         odzq = 1./dzq(k)
         orho = 1./rho(k)
         qgten(k) = qgten(k) - sed_g(k)*odzq*onstep(4)*orho
         rg(k) = MAX(R1, rg(k) - sed_g(k)*odzq*DT*onstep(4))
         do k = ksed1(4), kts, -1
            odzq = 1./dzq(k)
            orho = 1./rho(k)
            qgten(k) = qgten(k) + (sed_g(k+1)-sed_g(k))                 &
                                               *odzq*onstep(4)*orho
            rg(k) = MAX(R1, rg(k) + (sed_g(k+1)-sed_g(k)) &
                                           *odzq*DT*onstep(4))
         enddo

         if (rg(kts).gt.R1*10.) &
         pptgraul = pptgraul + sed_g(kts)*DT*onstep(4)
      enddo

!+---+-----------------------------------------------------------------+
!.. Instantly melt any cloud ice into cloud water if above 0C and
!.. instantly freeze any cloud water found below HGFR.
!+---+-----------------------------------------------------------------+
      if (.not. iiwarm) then
      do k = kts, kte
         xri = MAX(0.0, qi1d(k) + qiten(k)*DT)
         if ( (temp(k).gt. T_0) .and. (xri.gt. 0.0) ) then
          qcten(k) = qcten(k) + xri*odt
          ncten(k) = ncten(k) + ni1d(k)*odt
          qiten(k) = qiten(k) - xri*odt
          niten(k) = -ni1d(k)*odt
          tten(k) = tten(k) - lfus*ocp(k)*xri*odt*(1-IFDRY)
         endif

         xrc = MAX(0.0, qc1d(k) + qcten(k)*DT)
         if ( (temp(k).lt. HGFR) .and. (xrc.gt. 0.0) ) then
          lfus2 = lsub - lvap(k)
          xnc = nc1d(k) + ncten(k)*DT
          qiten(k) = qiten(k) + xrc*odt
          niten(k) = niten(k) + xnc*odt
          qcten(k) = qcten(k) - xrc*odt
          ncten(k) = ncten(k) - xnc*odt
          tten(k) = tten(k) + lfus2*ocp(k)*xrc*odt*(1-IFDRY)
         endif
      enddo
      endif

!+---+-----------------------------------------------------------------+
!.. All tendencies computed, apply and pass back final values to parent.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         t1d(k)  = t1d(k) + tten(k)*DT
         qv1d(k) = MAX(1.E-10, qv1d(k) + qvten(k)*DT)
         qc1d(k) = qc1d(k) + qcten(k)*DT
         nc1d(k) = MAX(2./rho(k), nc1d(k) + ncten(k)*DT)
         nwfa1d(k) = MAX(11.1E6/rho(k), MIN(9999.E6/rho(k),             &
                       (nwfa1d(k)+nwfaten(k)*DT)))
         nifa1d(k) = MAX(naIN1*0.01, MIN(9999.E6/rho(k),                &
                       (nifa1d(k)+nifaten(k)*DT)))

         if (qc1d(k) .le. R1) then
           qc1d(k) = 0.0
           nc1d(k) = 0.0
         else
           nu_c = MIN(15, NINT(1000.E6/(nc1d(k)*rho(k))) + 2)
           lamc = (am_r*ccg(2,nu_c)*ocg1(nu_c)*nc1d(k)/qc1d(k))**obmr
           xDc = (bm_r + nu_c + 1.) / lamc
           if (xDc.lt. D0c) then
            lamc = cce(2,nu_c)/D0c
           elseif (xDc.gt. D0r*2.) then
            lamc = cce(2,nu_c)/(D0r*2.)
           endif
           nc1d(k) = MIN(ccg(1,nu_c)*ocg2(nu_c)*qc1d(k)/am_r*lamc**bm_r,&
                         DBLE(Nt_c_max)/rho(k))
         endif

         qi1d(k) = qi1d(k) + qiten(k)*DT
         ni1d(k) = MAX(R2/rho(k), ni1d(k) + niten(k)*DT)
         if (qi1d(k) .le. R1) then
           qi1d(k) = 0.0
           ni1d(k) = 0.0
         else
           lami = (am_i*cig(2)*oig1*ni1d(k)/qi1d(k))**obmi
           ilami = 1./lami
           xDi = (bm_i + mu_i + 1.) * ilami
           if (xDi.lt. 20.E-6) then
            lami = cie(2)/20.E-6
           elseif (xDi.gt. 300.E-6) then
            lami = cie(2)/300.E-6
           endif
           ni1d(k) = MIN(cig(1)*oig2*qi1d(k)/am_i*lami**bm_i,           &
                         499.D3/rho(k))
         endif
         qr1d(k) = qr1d(k) + qrten(k)*DT
         nr1d(k) = MAX(R2/rho(k), nr1d(k) + nrten(k)*DT)
         if (qr1d(k) .le. R1) then
           qr1d(k) = 0.0
           nr1d(k) = 0.0
         else
           lamr = (am_r*crg(3)*org2*nr1d(k)/qr1d(k))**obmr
           mvd_r(k) = (3.0 + mu_r + 0.672) / lamr
           if (mvd_r(k) .gt. 2.5E-3) then
              mvd_r(k) = 2.5E-3
           elseif (mvd_r(k) .lt. D0r*0.75) then
              mvd_r(k) = D0r*0.75
           endif
           lamr = (3.0 + mu_r + 0.672) / mvd_r(k)
           nr1d(k) = crg(2)*org3*qr1d(k)*lamr**bm_r / am_r
         endif
         qs1d(k) = qs1d(k) + qsten(k)*DT
         if (qs1d(k) .le. R1) qs1d(k) = 0.0
         qg1d(k) = qg1d(k) + qgten(k)*DT
         if (qg1d(k) .le. R1) qg1d(k) = 0.0
      enddo

      end subroutine mp_thompson
!+---+-----------------------------------------------------------------+
!ctrlL
!+---+-----------------------------------------------------------------+
!..Creation of the lookup tables and support functions found below here.
!+---+-----------------------------------------------------------------+
!..Rain collecting graupel (and inverse).  Explicit CE integration.
!+---+-----------------------------------------------------------------+

      subroutine qr_acr_qg

      implicit none

!..Local variables
      INTEGER:: i, j, k, m, n, n2
      INTEGER:: km, km_s, km_e
      DOUBLE PRECISION, DIMENSION(nbg):: vg, N_g
      DOUBLE PRECISION, DIMENSION(nbr):: vr, N_r
      DOUBLE PRECISION:: N0_r, N0_g, lam_exp, lamg, lamr
      DOUBLE PRECISION:: massg, massr, dvg, dvr, t1, t2, z1, z2, y1, y2
      LOGICAL force_read_thompson, write_thompson_tables
      LOGICAL lexist,lopen
      INTEGER good
      LOGICAL, EXTERNAL :: wrf_dm_on_monitor

!+---+

      CALL nl_get_force_read_thompson(1,force_read_thompson)
      CALL nl_get_write_thompson_tables(1,write_thompson_tables)

      good = 0
      IF ( wrf_dm_on_monitor() ) THEN
        INQUIRE(FILE="qr_acr_qg.dat",EXIST=lexist)
        IF ( lexist ) THEN
          CALL wrf_message("ThompMP: read qr_acr_qg.dat stead of computing")
          OPEN(63,file="qr_acr_qg.dat",form="unformatted",err=1234)
          READ(63,err=1234) tcg_racg
          READ(63,err=1234) tmr_racg
          READ(63,err=1234) tcr_gacr
          READ(63,err=1234) tmg_gacr
          READ(63,err=1234) tnr_racg
          READ(63,err=1234) tnr_gacr
          good = 1
 1234     CONTINUE
          IF ( good .NE. 1 ) THEN
            INQUIRE(63,opened=lopen)
            IF (lopen) THEN
              IF( force_read_thompson ) THEN
                CALL wrf_error_fatal("Error reading qr_acr_qg.dat. Aborting because force_read_thompson is .true.")
              ENDIF
              CLOSE(63)
            ELSE
              IF( force_read_thompson ) THEN
                CALL wrf_error_fatal("Error opening qr_acr_qg.dat. Aborting because force_read_thompson is .true.")
              ENDIF
            ENDIF
          ENDIF
        ELSE
          IF( force_read_thompson ) THEN
            CALL wrf_error_fatal("Non-existent qr_acr_qg.dat. Aborting because force_read_thompson is .true.")
          ENDIF
        ENDIF
      ENDIF
#if defined(DM_PARALLEL) && !defined(STUBMPI)
      CALL wrf_dm_bcast_integer(good,1)
#endif

      IF ( good .EQ. 1 ) THEN
#if defined(DM_PARALLEL) && !defined(STUBMPI)
        CALL wrf_dm_bcast_double(tcg_racg,SIZE(tcg_racg))
        CALL wrf_dm_bcast_double(tmr_racg,SIZE(tmr_racg))
        CALL wrf_dm_bcast_double(tcr_gacr,SIZE(tcr_gacr))
        CALL wrf_dm_bcast_double(tmg_gacr,SIZE(tmg_gacr))
        CALL wrf_dm_bcast_double(tnr_racg,SIZE(tnr_racg))
        CALL wrf_dm_bcast_double(tnr_gacr,SIZE(tnr_gacr))
#endif
      ELSE
        CALL wrf_message("ThompMP: computing qr_acr_qg")
        do n2 = 1, nbr
!        vr(n2) = av_r*Dr(n2)**bv_r * DEXP(-fv_r*Dr(n2))
         vr(n2) = -0.1021 + 4.932E3*Dr(n2) - 0.9551E6*Dr(n2)*Dr(n2)     &
              + 0.07934E9*Dr(n2)*Dr(n2)*Dr(n2)                          &
              - 0.002362E12*Dr(n2)*Dr(n2)*Dr(n2)*Dr(n2)
        enddo
        do n = 1, nbg
         vg(n) = av_g*Dg(n)**bv_g
        enddo

!..Note values returned from wrf_dm_decomp1d are zero-based, add 1 for
!.. fortran indices.  J. Michalakes, 2009Oct30.

#if ( defined( DM_PARALLEL ) && ( ! defined( STUBMPI ) ) )
        CALL wrf_dm_decomp1d ( ntb_r*ntb_r1, km_s, km_e )
#else
        km_s = 0
        km_e = ntb_r*ntb_r1 - 1
#endif

        do km = km_s, km_e
         m = km / ntb_r1 + 1
         k = mod( km , ntb_r1 ) + 1

         lam_exp = (N0r_exp(k)*am_r*crg(1)/r_r(m))**ore1
         lamr = lam_exp * (crg(3)*org2*org1)**obmr
         N0_r = N0r_exp(k)/(crg(2)*lam_exp) * lamr**cre(2)
         do n2 = 1, nbr
            N_r(n2) = N0_r*Dr(n2)**mu_r *DEXP(-lamr*Dr(n2))*dtr(n2)
         enddo

         do j = 1, ntb_g
         do i = 1, ntb_g1
            lam_exp = (N0g_exp(i)*am_g*cgg(1)/r_g(j))**oge1
            lamg = lam_exp * (cgg(3)*ogg2*ogg1)**obmg
            N0_g = N0g_exp(i)/(cgg(2)*lam_exp) * lamg**cge(2)
            do n = 1, nbg
               N_g(n) = N0_g*Dg(n)**mu_g * DEXP(-lamg*Dg(n))*dtg(n)
            enddo

            t1 = 0.0d0
            t2 = 0.0d0
            z1 = 0.0d0
            z2 = 0.0d0
            y1 = 0.0d0
            y2 = 0.0d0
            do n2 = 1, nbr
               massr = am_r * Dr(n2)**bm_r
               do n = 1, nbg
                  massg = am_g * Dg(n)**bm_g

                  dvg = 0.5d0*((vr(n2) - vg(n)) + DABS(vr(n2)-vg(n)))
                  dvr = 0.5d0*((vg(n) - vr(n2)) + DABS(vg(n)-vr(n2)))

                  t1 = t1+ PI*.25*Ef_rg*(Dg(n)+Dr(n2))*(Dg(n)+Dr(n2)) &
                      *dvg*massg * N_g(n)* N_r(n2)
                  z1 = z1+ PI*.25*Ef_rg*(Dg(n)+Dr(n2))*(Dg(n)+Dr(n2)) &
                      *dvg*massr * N_g(n)* N_r(n2)
                  y1 = y1+ PI*.25*Ef_rg*(Dg(n)+Dr(n2))*(Dg(n)+Dr(n2)) &
                      *dvg       * N_g(n)* N_r(n2)

                  t2 = t2+ PI*.25*Ef_rg*(Dg(n)+Dr(n2))*(Dg(n)+Dr(n2)) &
                      *dvr*massr * N_g(n)* N_r(n2)
                  y2 = y2+ PI*.25*Ef_rg*(Dg(n)+Dr(n2))*(Dg(n)+Dr(n2)) &
                      *dvr       * N_g(n)* N_r(n2)
                  z2 = z2+ PI*.25*Ef_rg*(Dg(n)+Dr(n2))*(Dg(n)+Dr(n2)) &
                      *dvr*massg * N_g(n)* N_r(n2)
               enddo
 97            continue
            enddo
            tcg_racg(i,j,k,m) = t1
            tmr_racg(i,j,k,m) = DMIN1(z1, r_r(m)*1.0d0)
            tcr_gacr(i,j,k,m) = t2
            tmg_gacr(i,j,k,m) = z2
            tnr_racg(i,j,k,m) = y1
            tnr_gacr(i,j,k,m) = y2
         enddo
         enddo
        enddo

!..Note wrf_dm_gatherv expects zero-based km_s, km_e (J. Michalakes, 2009Oct30).

#if ( defined( DM_PARALLEL ) && ( ! defined( STUBMPI ) ) )
        CALL wrf_dm_gatherv(tcg_racg, ntb_g*ntb_g1, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tmr_racg, ntb_g*ntb_g1, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tcr_gacr, ntb_g*ntb_g1, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tmg_gacr, ntb_g*ntb_g1, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tnr_racg, ntb_g*ntb_g1, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tnr_gacr, ntb_g*ntb_g1, km_s, km_e, R8SIZE)
#endif

        IF ( write_thompson_tables .AND. wrf_dm_on_monitor() ) THEN
          CALL wrf_message("Writing qr_acr_qg.dat in Thompson MP init")
          OPEN(63,file="qr_acr_qg.dat",form="unformatted",err=9234)
          WRITE(63,err=9234) tcg_racg
          WRITE(63,err=9234) tmr_racg
          WRITE(63,err=9234) tcr_gacr
          WRITE(63,err=9234) tmg_gacr
          WRITE(63,err=9234) tnr_racg
          WRITE(63,err=9234) tnr_gacr
          CLOSE(63)
          RETURN    ! ----- RETURN
 9234     CONTINUE
          CALL wrf_error_fatal("Error writing qr_acr_qg.dat")
        ENDIF
      ENDIF

      end subroutine qr_acr_qg
!+---+-----------------------------------------------------------------+
!ctrlL
!+---+-----------------------------------------------------------------+
!..Rain collecting snow (and inverse).  Explicit CE integration.
!+---+-----------------------------------------------------------------+

      subroutine qr_acr_qs

      implicit none

!..Local variables
      INTEGER:: i, j, k, m, n, n2
      INTEGER:: km, km_s, km_e
      DOUBLE PRECISION, DIMENSION(nbr):: vr, D1, N_r
      DOUBLE PRECISION, DIMENSION(nbs):: vs, N_s
      DOUBLE PRECISION:: loga_, a_, b_, second, M0, M2, M3, Mrat, oM3
      DOUBLE PRECISION:: N0_r, lam_exp, lamr, slam1, slam2
      DOUBLE PRECISION:: dvs, dvr, masss, massr
      DOUBLE PRECISION:: t1, t2, t3, t4, z1, z2, z3, z4
      DOUBLE PRECISION:: y1, y2, y3, y4
      LOGICAL force_read_thompson, write_thompson_tables
      LOGICAL lexist,lopen
      INTEGER good
      LOGICAL, EXTERNAL :: wrf_dm_on_monitor

!+---+

      CALL nl_get_force_read_thompson(1,force_read_thompson)
      CALL nl_get_write_thompson_tables(1,write_thompson_tables)

      good = 0
      IF ( wrf_dm_on_monitor() ) THEN
        INQUIRE(FILE="qr_acr_qs.dat",EXIST=lexist)
        IF ( lexist ) THEN
          CALL wrf_message("ThompMP: read qr_acr_qs.dat instead of computing")
          OPEN(63,file="qr_acr_qs.dat",form="unformatted",err=1234)
          READ(63,err=1234)tcs_racs1
          READ(63,err=1234)tmr_racs1
          READ(63,err=1234)tcs_racs2
          READ(63,err=1234)tmr_racs2
          READ(63,err=1234)tcr_sacr1
          READ(63,err=1234)tms_sacr1
          READ(63,err=1234)tcr_sacr2
          READ(63,err=1234)tms_sacr2
          READ(63,err=1234)tnr_racs1
          READ(63,err=1234)tnr_racs2
          READ(63,err=1234)tnr_sacr1
          READ(63,err=1234)tnr_sacr2
          good = 1
 1234     CONTINUE
          IF ( good .NE. 1 ) THEN
            INQUIRE(63,opened=lopen)
            IF (lopen) THEN
              IF( force_read_thompson ) THEN
                CALL wrf_error_fatal("Error reading qr_acr_qs.dat. Aborting because force_read_thompson is .true.")
              ENDIF
              CLOSE(63)
            ELSE
              IF( force_read_thompson ) THEN
                CALL wrf_error_fatal("Error opening qr_acr_qs.dat. Aborting because force_read_thompson is .true.")
              ENDIF
            ENDIF
          ENDIF
        ELSE
          IF( force_read_thompson ) THEN
            CALL wrf_error_fatal("Non-existent qr_acr_qs.dat. Aborting because force_read_thompson is .true.")
          ENDIF
        ENDIF
      ENDIF
#if defined(DM_PARALLEL) && !defined(STUBMPI)
      CALL wrf_dm_bcast_integer(good,1)
#endif

      IF ( good .EQ. 1 ) THEN
#if defined(DM_PARALLEL) && !defined(STUBMPI)
        CALL wrf_dm_bcast_double(tcs_racs1,SIZE(tcs_racs1))
        CALL wrf_dm_bcast_double(tmr_racs1,SIZE(tmr_racs1))
        CALL wrf_dm_bcast_double(tcs_racs2,SIZE(tcs_racs2))
        CALL wrf_dm_bcast_double(tmr_racs2,SIZE(tmr_racs2))
        CALL wrf_dm_bcast_double(tcr_sacr1,SIZE(tcr_sacr1))
        CALL wrf_dm_bcast_double(tms_sacr1,SIZE(tms_sacr1))
        CALL wrf_dm_bcast_double(tcr_sacr2,SIZE(tcr_sacr2))
        CALL wrf_dm_bcast_double(tms_sacr2,SIZE(tms_sacr2))
        CALL wrf_dm_bcast_double(tnr_racs1,SIZE(tnr_racs1))
        CALL wrf_dm_bcast_double(tnr_racs2,SIZE(tnr_racs2))
        CALL wrf_dm_bcast_double(tnr_sacr1,SIZE(tnr_sacr1))
        CALL wrf_dm_bcast_double(tnr_sacr2,SIZE(tnr_sacr2))
#endif
      ELSE
        CALL wrf_message("ThompMP: computing qr_acr_qs")
        do n2 = 1, nbr
!        vr(n2) = av_r*Dr(n2)**bv_r * DEXP(-fv_r*Dr(n2))
         vr(n2) = -0.1021 + 4.932E3*Dr(n2) - 0.9551E6*Dr(n2)*Dr(n2)     &
              + 0.07934E9*Dr(n2)*Dr(n2)*Dr(n2)                          &
              - 0.002362E12*Dr(n2)*Dr(n2)*Dr(n2)*Dr(n2)
         D1(n2) = (vr(n2)/av_s)**(1./bv_s)
        enddo
        do n = 1, nbs
         vs(n) = 1.5*av_s*Ds(n)**bv_s * DEXP(-fv_s*Ds(n))
        enddo

!..Note values returned from wrf_dm_decomp1d are zero-based, add 1 for
!.. fortran indices.  J. Michalakes, 2009Oct30.

#if ( defined( DM_PARALLEL ) && ( ! defined( STUBMPI ) ) )
        CALL wrf_dm_decomp1d ( ntb_r*ntb_r1, km_s, km_e )
#else
        km_s = 0
        km_e = ntb_r*ntb_r1 - 1
#endif

        do km = km_s, km_e
         m = km / ntb_r1 + 1
         k = mod( km , ntb_r1 ) + 1

         lam_exp = (N0r_exp(k)*am_r*crg(1)/r_r(m))**ore1
         lamr = lam_exp * (crg(3)*org2*org1)**obmr
         N0_r = N0r_exp(k)/(crg(2)*lam_exp) * lamr**cre(2)
         do n2 = 1, nbr
            N_r(n2) = N0_r*Dr(n2)**mu_r * DEXP(-lamr*Dr(n2))*dtr(n2)
         enddo

         do j = 1, ntb_t
            do i = 1, ntb_s

!..From the bm_s moment, compute plus one moment.  If we are not
!.. using bm_s=2, then we must transform to the pure 2nd moment
!.. (variable called "second") and then to the bm_s+1 moment.

               M2 = r_s(i)*oams *1.0d0
               if (bm_s.gt.2.0-1.E-3 .and. bm_s.lt.2.0+1.E-3) then
                  loga_ = sa(1) + sa(2)*Tc(j) + sa(3)*bm_s &
                     + sa(4)*Tc(j)*bm_s + sa(5)*Tc(j)*Tc(j) &
                     + sa(6)*bm_s*bm_s + sa(7)*Tc(j)*Tc(j)*bm_s &
                     + sa(8)*Tc(j)*bm_s*bm_s + sa(9)*Tc(j)*Tc(j)*Tc(j) &
                     + sa(10)*bm_s*bm_s*bm_s
                  a_ = 10.0**loga_
                  b_ = sb(1) + sb(2)*Tc(j) + sb(3)*bm_s &
                     + sb(4)*Tc(j)*bm_s + sb(5)*Tc(j)*Tc(j) &
                     + sb(6)*bm_s*bm_s + sb(7)*Tc(j)*Tc(j)*bm_s &
                     + sb(8)*Tc(j)*bm_s*bm_s + sb(9)*Tc(j)*Tc(j)*Tc(j) &
                     + sb(10)*bm_s*bm_s*bm_s
                  second = (M2/a_)**(1./b_)
               else
                  second = M2
               endif

               loga_ = sa(1) + sa(2)*Tc(j) + sa(3)*cse(1) &
                  + sa(4)*Tc(j)*cse(1) + sa(5)*Tc(j)*Tc(j) &
                  + sa(6)*cse(1)*cse(1) + sa(7)*Tc(j)*Tc(j)*cse(1) &
                  + sa(8)*Tc(j)*cse(1)*cse(1) + sa(9)*Tc(j)*Tc(j)*Tc(j) &
                  + sa(10)*cse(1)*cse(1)*cse(1)
               a_ = 10.0**loga_
               b_ = sb(1)+sb(2)*Tc(j)+sb(3)*cse(1) + sb(4)*Tc(j)*cse(1) &
                  + sb(5)*Tc(j)*Tc(j) + sb(6)*cse(1)*cse(1) &
                  + sb(7)*Tc(j)*Tc(j)*cse(1) + sb(8)*Tc(j)*cse(1)*cse(1) &
                  + sb(9)*Tc(j)*Tc(j)*Tc(j)+sb(10)*cse(1)*cse(1)*cse(1)
               M3 = a_ * second**b_

               oM3 = 1./M3
               Mrat = M2*(M2*oM3)*(M2*oM3)*(M2*oM3)
               M0   = (M2*oM3)**mu_s
               slam1 = M2 * oM3 * Lam0
               slam2 = M2 * oM3 * Lam1

               do n = 1, nbs
                  N_s(n) = Mrat*(Kap0*DEXP(-slam1*Ds(n)) &
                      + Kap1*M0*Ds(n)**mu_s * DEXP(-slam2*Ds(n)))*dts(n)
               enddo

               t1 = 0.0d0
               t2 = 0.0d0
               t3 = 0.0d0
               t4 = 0.0d0
               z1 = 0.0d0
               z2 = 0.0d0
               z3 = 0.0d0
               z4 = 0.0d0
               y1 = 0.0d0
               y2 = 0.0d0
               y3 = 0.0d0
               y4 = 0.0d0
               do n2 = 1, nbr
                  massr = am_r * Dr(n2)**bm_r
                  do n = 1, nbs
                     masss = am_s * Ds(n)**bm_s
      
                     dvs = 0.5d0*((vr(n2) - vs(n)) + DABS(vr(n2)-vs(n)))
                     dvr = 0.5d0*((vs(n) - vr(n2)) + DABS(vs(n)-vr(n2)))

                     if (massr .gt. 1.5*masss) then
                     t1 = t1+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvs*masss * N_s(n)* N_r(n2)
                     z1 = z1+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvs*massr * N_s(n)* N_r(n2)
                     y1 = y1+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvs       * N_s(n)* N_r(n2)
                     else
                     t3 = t3+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvs*masss * N_s(n)* N_r(n2)
                     z3 = z3+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvs*massr * N_s(n)* N_r(n2)
                     y3 = y3+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvs       * N_s(n)* N_r(n2)
                     endif

                     if (massr .gt. 1.5*masss) then
                     t2 = t2+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvr*massr * N_s(n)* N_r(n2)
                     y2 = y2+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvr       * N_s(n)* N_r(n2)
                     z2 = z2+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvr*masss * N_s(n)* N_r(n2)
                     else
                     t4 = t4+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvr*massr * N_s(n)* N_r(n2)
                     y4 = y4+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvr       * N_s(n)* N_r(n2)
                     z4 = z4+ PI*.25*Ef_rs*(Ds(n)+Dr(n2))*(Ds(n)+Dr(n2)) &
                         *dvr*masss * N_s(n)* N_r(n2)
                     endif

                  enddo
               enddo
               tcs_racs1(i,j,k,m) = t1
               tmr_racs1(i,j,k,m) = DMIN1(z1, r_r(m)*1.0d0)
               tcs_racs2(i,j,k,m) = t3
               tmr_racs2(i,j,k,m) = z3
               tcr_sacr1(i,j,k,m) = t2
               tms_sacr1(i,j,k,m) = z2
               tcr_sacr2(i,j,k,m) = t4
               tms_sacr2(i,j,k,m) = z4
               tnr_racs1(i,j,k,m) = y1
               tnr_racs2(i,j,k,m) = y3
               tnr_sacr1(i,j,k,m) = y2
               tnr_sacr2(i,j,k,m) = y4
            enddo
         enddo
        enddo

!..Note wrf_dm_gatherv expects zero-based km_s, km_e (J. Michalakes, 2009Oct30).

#if ( defined( DM_PARALLEL ) && ( ! defined( STUBMPI ) ) )
        CALL wrf_dm_gatherv(tcs_racs1, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tmr_racs1, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tcs_racs2, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tmr_racs2, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tcr_sacr1, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tms_sacr1, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tcr_sacr2, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tms_sacr2, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tnr_racs1, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tnr_racs2, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tnr_sacr1, ntb_s*ntb_t, km_s, km_e, R8SIZE)
        CALL wrf_dm_gatherv(tnr_sacr2, ntb_s*ntb_t, km_s, km_e, R8SIZE)
#endif

        IF ( write_thompson_tables .AND. wrf_dm_on_monitor() ) THEN
          CALL wrf_message("Writing qr_acr_qs.dat in Thompson MP init")
          OPEN(63,file="qr_acr_qs.dat",form="unformatted",err=9234)
          WRITE(63,err=9234)tcs_racs1
          WRITE(63,err=9234)tmr_racs1
          WRITE(63,err=9234)tcs_racs2
          WRITE(63,err=9234)tmr_racs2
          WRITE(63,err=9234)tcr_sacr1
          WRITE(63,err=9234)tms_sacr1
          WRITE(63,err=9234)tcr_sacr2
          WRITE(63,err=9234)tms_sacr2
          WRITE(63,err=9234)tnr_racs1
          WRITE(63,err=9234)tnr_racs2
          WRITE(63,err=9234)tnr_sacr1
          WRITE(63,err=9234)tnr_sacr2
          CLOSE(63)
          RETURN    ! ----- RETURN
 9234     CONTINUE
          CALL wrf_error_fatal("Error writing qr_acr_qs.dat")
        ENDIF
      ENDIF

      end subroutine qr_acr_qs
!+---+-----------------------------------------------------------------+
!ctrlL
!+---+-----------------------------------------------------------------+
!..This is a literal adaptation of Bigg (1954) probability of drops of
!..a particular volume freezing.  Given this probability, simply freeze
!..the proportion of drops summing their masses.
!+---+-----------------------------------------------------------------+

      subroutine freezeH2O

      implicit none

!..Local variables
      INTEGER:: i, j, k, m, n, n2
      DOUBLE PRECISION, DIMENSION(nbr):: N_r, massr
      DOUBLE PRECISION, DIMENSION(nbc):: N_c, massc
      DOUBLE PRECISION:: sum1, sum2, sumn1, sumn2, &
                         prob, vol, Texp, orho_w, &
                         lam_exp, lamr, N0_r, lamc, N0_c, y
      INTEGER:: nu_c
      REAL:: T_adjust
      LOGICAL force_read_thompson, write_thompson_tables
      LOGICAL lexist,lopen
      INTEGER good
      LOGICAL, EXTERNAL :: wrf_dm_on_monitor

!+---+
      CALL nl_get_force_read_thompson(1,force_read_thompson)
      CALL nl_get_write_thompson_tables(1,write_thompson_tables)

      good = 0
      IF ( wrf_dm_on_monitor() ) THEN
        INQUIRE(FILE="freezeH2O.dat",EXIST=lexist)
        IF ( lexist ) THEN
          CALL wrf_message("ThompMP: read freezeH2O.dat stead of computing")
          OPEN(63,file="freezeH2O.dat",form="unformatted",err=1234)
          READ(63,err=1234)tpi_qrfz
          READ(63,err=1234)tni_qrfz
          READ(63,err=1234)tpg_qrfz
          READ(63,err=1234)tnr_qrfz
          READ(63,err=1234)tpi_qcfz
          READ(63,err=1234)tni_qcfz
          good = 1
 1234     CONTINUE
          IF ( good .NE. 1 ) THEN
            INQUIRE(63,opened=lopen)
            IF (lopen) THEN
              IF( force_read_thompson ) THEN
                CALL wrf_error_fatal("Error reading freezeH2O.dat. Aborting because force_read_thompson is .true.")
              ENDIF
              CLOSE(63)
            ELSE
              IF( force_read_thompson ) THEN
                CALL wrf_error_fatal("Error opening freezeH2O.dat. Aborting because force_read_thompson is .true.")
              ENDIF
            ENDIF
          ENDIF
        ELSE
          IF( force_read_thompson ) THEN
            CALL wrf_error_fatal("Non-existent freezeH2O.dat. Aborting because force_read_thompson is .true.")
          ENDIF
        ENDIF
      ENDIF

#if defined(DM_PARALLEL) && !defined(STUBMPI)
      CALL wrf_dm_bcast_integer(good,1)
#endif

      IF ( good .EQ. 1 ) THEN
#if defined(DM_PARALLEL) && !defined(STUBMPI)
        CALL wrf_dm_bcast_double(tpi_qrfz,SIZE(tpi_qrfz))
        CALL wrf_dm_bcast_double(tni_qrfz,SIZE(tni_qrfz))
        CALL wrf_dm_bcast_double(tpg_qrfz,SIZE(tpg_qrfz))
        CALL wrf_dm_bcast_double(tnr_qrfz,SIZE(tnr_qrfz))
        CALL wrf_dm_bcast_double(tpi_qcfz,SIZE(tpi_qcfz))
        CALL wrf_dm_bcast_double(tni_qcfz,SIZE(tni_qcfz))
#endif
      ELSE
        CALL wrf_message("ThompMP: computing freezeH2O")

        orho_w = 1./rho_w

        do n2 = 1, nbr
         massr(n2) = am_r*Dr(n2)**bm_r
        enddo
        do n = 1, nbc
         massc(n) = am_r*Dc(n)**bm_r
        enddo

!..Freeze water (smallest drops become cloud ice, otherwise graupel).
        do m = 1, ntb_IN
        T_adjust = MAX(-3.0, MIN(3.0 - ALOG10(Nt_IN(m)), 3.0))
        do k = 1, 45
!         print*, ' Freezing water for temp = ', -k
         Texp = DEXP( DFLOAT(k) - T_adjust*1.0D0 ) - 1.0D0
         do j = 1, ntb_r1
            do i = 1, ntb_r
               lam_exp = (N0r_exp(j)*am_r*crg(1)/r_r(i))**ore1
               lamr = lam_exp * (crg(3)*org2*org1)**obmr
               N0_r = N0r_exp(j)/(crg(2)*lam_exp) * lamr**cre(2)
               sum1 = 0.0d0
               sum2 = 0.0d0
               sumn1 = 0.0d0
               sumn2 = 0.0d0
               do n2 = nbr, 1, -1
                  N_r(n2) = N0_r*Dr(n2)**mu_r*DEXP(-lamr*Dr(n2))*dtr(n2)
                  vol = massr(n2)*orho_w
                  prob = 1.0D0 - DEXP(-120.0D0*vol*5.2D-4 * Texp)
                  if (massr(n2) .lt. xm0g) then
                     sumn1 = sumn1 + prob*N_r(n2)
                     sum1 = sum1 + prob*N_r(n2)*massr(n2)
                  else
                     sumn2 = sumn2 + prob*N_r(n2)
                     sum2 = sum2 + prob*N_r(n2)*massr(n2)
                  endif
                  if ((sum1+sum2).ge.r_r(i)) EXIT
               enddo
               tpi_qrfz(i,j,k,m) = sum1
               tni_qrfz(i,j,k,m) = sumn1
               tpg_qrfz(i,j,k,m) = sum2
               tnr_qrfz(i,j,k,m) = sumn2
            enddo
         enddo

         do j = 1, nbc
            nu_c = MIN(15, NINT(1000.E6/t_Nc(j)) + 2)
            do i = 1, ntb_c
               lamc = (t_Nc(j)*am_r* ccg(2,nu_c) * ocg1(nu_c) / r_c(i))**obmr
               N0_c = t_Nc(j)*ocg1(nu_c) * lamc**cce(1,nu_c)
               sum1 = 0.0d0
               sumn2 = 0.0d0
               do n = nbc, 1, -1
                  vol = massc(n)*orho_w
                  prob = 1.0D0 - DEXP(-120.0D0*vol*5.2D-4 * Texp)
                  N_c(n) = N0_c*Dc(n)**nu_c*EXP(-lamc*Dc(n))*dtc(n)
                  sumn2 = MIN(t_Nc(j), sumn2 + prob*N_c(n))
                  sum1 = sum1 + prob*N_c(n)*massc(n)
                  if (sum1 .ge. r_c(i)) EXIT
               enddo
               tpi_qcfz(i,j,k,m) = sum1
               tni_qcfz(i,j,k,m) = sumn2
            enddo
         enddo
        enddo
        enddo

        IF ( write_thompson_tables .AND. wrf_dm_on_monitor() ) THEN
          CALL wrf_message("Writing freezeH2O.dat in Thompson MP init")
          OPEN(63,file="freezeH2O.dat",form="unformatted",err=9234)
          WRITE(63,err=9234)tpi_qrfz
          WRITE(63,err=9234)tni_qrfz
          WRITE(63,err=9234)tpg_qrfz
          WRITE(63,err=9234)tnr_qrfz
          WRITE(63,err=9234)tpi_qcfz
          WRITE(63,err=9234)tni_qcfz
          CLOSE(63)
          RETURN    ! ----- RETURN
 9234     CONTINUE
          CALL wrf_error_fatal("Error writing freezeH2O.dat")
        ENDIF
      ENDIF

      end subroutine freezeH2O
!+---+-----------------------------------------------------------------+
!ctrlL
!+---+-----------------------------------------------------------------+
!..Cloud ice converting to snow since portion greater than min snow
!.. size.  Given cloud ice content (kg/m**3), number concentration
!.. (#/m**3) and gamma shape parameter, mu_i, break the distrib into
!.. bins and figure out the mass/number of ice with sizes larger than
!.. D0s.  Also, compute incomplete gamma function for the integration
!.. of ice depositional growth from diameter=0 to D0s.  Amount of
!.. ice depositional growth is this portion of distrib while larger
!.. diameters contribute to snow growth (as in Harrington et al. 1995).
!+---+-----------------------------------------------------------------+

      subroutine qi_aut_qs

      implicit none

!..Local variables
      INTEGER:: i, j, n2
      DOUBLE PRECISION, DIMENSION(nbi):: N_i
      DOUBLE PRECISION:: N0_i, lami, Di_mean, t1, t2
      REAL:: xlimit_intg

!+---+

      do j = 1, ntb_i1
         do i = 1, ntb_i
            lami = (am_i*cig(2)*oig1*Nt_i(j)/r_i(i))**obmi
            Di_mean = (bm_i + mu_i + 1.) / lami
            N0_i = Nt_i(j)*oig1 * lami**cie(1)
            t1 = 0.0d0
            t2 = 0.0d0
            if (SNGL(Di_mean) .gt. 5.*D0s) then
             t1 = r_i(i)
             t2 = Nt_i(j)
             tpi_ide(i,j) = 0.0D0
            elseif (SNGL(Di_mean) .lt. D0i) then
             t1 = 0.0D0
             t2 = 0.0D0
             tpi_ide(i,j) = 1.0D0
            else
             xlimit_intg = lami*D0s
             tpi_ide(i,j) = GAMMP(mu_i+2.0, xlimit_intg) * 1.0D0
             do n2 = 1, nbi
               N_i(n2) = N0_i*Di(n2)**mu_i * DEXP(-lami*Di(n2))*dti(n2)
               if (Di(n2).ge.D0s) then
                  t1 = t1 + N_i(n2) * am_i*Di(n2)**bm_i
                  t2 = t2 + N_i(n2)
               endif
             enddo
            endif
            tps_iaus(i,j) = t1
            tni_iaus(i,j) = t2
         enddo
      enddo

      end subroutine qi_aut_qs
!ctrlL
!+---+-----------------------------------------------------------------+
!..Variable collision efficiency for rain collecting cloud water using
!.. method of Beard and Grover, 1974 if a/A less than 0.25; otherwise
!.. uses polynomials to get close match of Pruppacher & Klett Fig 14-9.
!+---+-----------------------------------------------------------------+

      subroutine table_Efrw

      implicit none

!..Local variables
      DOUBLE PRECISION:: vtr, stokes, reynolds, Ef_rw
      DOUBLE PRECISION:: p, yc0, F, G, H, z, K0, X
      INTEGER:: i, j

      do j = 1, nbc
      do i = 1, nbr
         Ef_rw = 0.0
         p = Dc(j)/Dr(i)
         if (Dr(i).lt.50.E-6 .or. Dc(j).lt.3.E-6) then
          t_Efrw(i,j) = 0.0
         elseif (p.gt.0.25) then
          X = Dc(j)*1.D6
          if (Dr(i) .lt. 75.e-6) then
             Ef_rw = 0.026794*X - 0.20604
          elseif (Dr(i) .lt. 125.e-6) then
             Ef_rw = -0.00066842*X*X + 0.061542*X - 0.37089
          elseif (Dr(i) .lt. 175.e-6) then
             Ef_rw = 4.091e-06*X*X*X*X - 0.00030908*X*X*X               &
                   + 0.0066237*X*X - 0.0013687*X - 0.073022
          elseif (Dr(i) .lt. 250.e-6) then
             Ef_rw = 9.6719e-5*X*X*X - 0.0068901*X*X + 0.17305*X        &
                   - 0.65988
          elseif (Dr(i) .lt. 350.e-6) then
             Ef_rw = 9.0488e-5*X*X*X - 0.006585*X*X + 0.16606*X         &
                   - 0.56125
          else
             Ef_rw = 0.00010721*X*X*X - 0.0072962*X*X + 0.1704*X        &
                   - 0.46929
          endif
         else
          vtr = -0.1021 + 4.932E3*Dr(i) - 0.9551E6*Dr(i)*Dr(i) &
              + 0.07934E9*Dr(i)*Dr(i)*Dr(i) &
              - 0.002362E12*Dr(i)*Dr(i)*Dr(i)*Dr(i)
          stokes = Dc(j)*Dc(j)*vtr*rho_w/(9.*1.718E-5*Dr(i))
          reynolds = 9.*stokes/(p*p*rho_w)

          F = DLOG(reynolds)
          G = -0.1007D0 - 0.358D0*F + 0.0261D0*F*F
          K0 = DEXP(G)
          z = DLOG(stokes/(K0+1.D-15))
          H = 0.1465D0 + 1.302D0*z - 0.607D0*z*z + 0.293D0*z*z*z
          yc0 = 2.0D0/PI * ATAN(H)
          Ef_rw = (yc0+p)*(yc0+p) / ((1.+p)*(1.+p))

         endif

         t_Efrw(i,j) = MAX(0.0, MIN(SNGL(Ef_rw), 0.95))

      enddo
      enddo

      end subroutine table_Efrw
!ctrlL
!+---+-----------------------------------------------------------------+
!..Variable collision efficiency for snow collecting cloud water using
!.. method of Wang and Ji, 2000 except equate melted snow diameter to
!.. their "effective collision cross-section."
!+---+-----------------------------------------------------------------+

      subroutine table_Efsw

      implicit none

!..Local variables
      DOUBLE PRECISION:: Ds_m, vts, vtc, stokes, reynolds, Ef_sw
      DOUBLE PRECISION:: p, yc0, F, G, H, z, K0
      INTEGER:: i, j

      do j = 1, nbc
      vtc = 1.19D4 * (1.0D4*Dc(j)*Dc(j)*0.25D0)
      do i = 1, nbs
         vts = av_s*Ds(i)**bv_s * DEXP(-fv_s*Ds(i)) - vtc
         Ds_m = (am_s*Ds(i)**bm_s / am_r)**obmr
         p = Dc(j)/Ds_m
         if (p.gt.0.25 .or. Ds(i).lt.D0s .or. Dc(j).lt.6.E-6 &
               .or. vts.lt.1.E-3) then
          t_Efsw(i,j) = 0.0
         else
          stokes = Dc(j)*Dc(j)*vts*rho_w/(9.*1.718E-5*Ds_m)
          reynolds = 9.*stokes/(p*p*rho_w)

          F = DLOG(reynolds)
          G = -0.1007D0 - 0.358D0*F + 0.0261D0*F*F
          K0 = DEXP(G)
          z = DLOG(stokes/(K0+1.D-15))
          H = 0.1465D0 + 1.302D0*z - 0.607D0*z*z + 0.293D0*z*z*z
          yc0 = 2.0D0/PI * ATAN(H)
          Ef_sw = (yc0+p)*(yc0+p) / ((1.+p)*(1.+p))

          t_Efsw(i,j) = MAX(0.0, MIN(SNGL(Ef_sw), 0.95))
         endif

      enddo
      enddo

      end subroutine table_Efsw
!ctrlL
!+---+-----------------------------------------------------------------+
!..Function to compute collision efficiency of collector species (rain,
!.. snow, graupel) of aerosols.  Follows Wang et al, 2010, ACP, which
!.. follows Slinn (1983).
!+---+-----------------------------------------------------------------+

      real function Eff_aero(D, Da, visc,rhoa,Temp,species)

      implicit none
      real:: D, Da, visc, rhoa, Temp
      character(LEN=1):: species
      real:: aval, Cc, diff, Re, Sc, St, St2, vt, Eff
      real, parameter:: boltzman = 1.3806503E-23
      real, parameter:: meanPath = 0.0256E-6

      vt = 1.
      if (species .eq. 'r') then
         vt = -0.1021 + 4.932E3*D - 0.9551E6*D*D                        &
              + 0.07934E9*D*D*D - 0.002362E12*D*D*D*D
      elseif (species .eq. 's') then
         vt = av_s*D**bv_s
      elseif (species .eq. 'g') then
         vt = av_g*D**bv_g
      endif

      Cc    = 1. + 2.*meanPath/Da *(1.257+0.4*exp(-0.55*Da/meanPath))
      diff  = boltzman*Temp*Cc/(3.*PI*visc*Da)

      Re    = 0.5*rhoa*D*vt/visc
      Sc    = visc/(rhoa*diff)

      St    = Da*Da*vt*1000./(9.*visc*D)
      aval  = 1.+LOG(1.+Re)
      St2   = (1.2 + 1./12.*aval)/(1.+aval)

      Eff = 4./(Re*Sc) * (1. + 0.4*SQRT(Re)*Sc**0.3333                  &
                             + 0.16*SQRT(Re)*SQRT(Sc))                  &
               + 4.*Da/D * (0.02 + Da/D*(1.+2.*SQRT(Re)))

      if (St.gt.St2) Eff = Eff  + ( (St-St2)/(St-St2+0.666667))**1.5
      Eff_aero = MAX(1.E-5, MIN(Eff, 1.0))

      end function Eff_aero

!ctrlL
!+---+-----------------------------------------------------------------+
!..Integrate rain size distribution from zero to D-star to compute the
!.. number of drops smaller than D-star that evaporate in a single
!.. timestep.  Drops larger than D-star dont evaporate entirely so do
!.. not affect number concentration.
!+---+-----------------------------------------------------------------+

      subroutine table_dropEvap

      implicit none

!..Local variables
      INTEGER:: i, j, k, n
      DOUBLE PRECISION, DIMENSION(nbc):: N_c, massc
      DOUBLE PRECISION:: summ, summ2, lamc, N0_c
      INTEGER:: nu_c
!      DOUBLE PRECISION:: Nt_r, N0, lam_exp, lam
!      REAL:: xlimit_intg

      do n = 1, nbc
         massc(n) = am_r*Dc(n)**bm_r
      enddo

      do k = 1, nbc
         nu_c = MIN(15, NINT(1000.E6/t_Nc(k)) + 2)
         do j = 1, ntb_c
            lamc = (t_Nc(k)*am_r* ccg(2,nu_c)*ocg1(nu_c) / r_c(j))**obmr
            N0_c = t_Nc(k)*ocg1(nu_c) * lamc**cce(1,nu_c)
            do i = 1, nbc
!-GT           tnc_wev(i,j,k) = GAMMP(nu_c+1., SNGL(Dc(i)*lamc))*t_Nc(k)
               N_c(i) = N0_c* Dc(i)**nu_c*EXP(-lamc*Dc(i))*dtc(i)
!     if(j.eq.18 .and. k.eq.50) print*, ' N_c = ', N_c(i)
               summ = 0.
               summ2 = 0.
               do n = 1, i
                  summ = summ + massc(n)*N_c(n)
                  summ2 = summ2 + N_c(n)
               enddo
!      if(j.eq.18 .and. k.eq.50) print*, '  DEBUG-TABLE: ', r_c(j), t_Nc(k), summ2, summ
               tpc_wev(i,j,k) = summ
               tnc_wev(i,j,k) = summ2
            enddo
         enddo
      enddo

!
!..To do the same thing for rain.
!
!     do k = 1, ntb_r
!     do j = 1, ntb_r1
!        lam_exp = (N0r_exp(j)*am_r*crg(1)/r_r(k))**ore1
!        lam = lam_exp * (crg(3)*org2*org1)**obmr
!        N0 = N0r_exp(j)/(crg(2)*lam_exp) * lam**cre(2)
!        Nt_r = N0 * crg(2) / lam**cre(2)
!        do i = 1, nbr
!           xlimit_intg = lam*Dr(i)
!           tnr_rev(i,j,k) = GAMMP(mu_r+1.0, xlimit_intg) * Nt_r
!        enddo
!     enddo
!     enddo

! TO APPLY TABLE ABOVE
!..Rain lookup table indexes.
!         Dr_star = DSQRT(-2.D0*DT * t1_evap/(2.*PI) &
!                 * 0.78*4.*diffu(k)*xsat*rvs/rho_w)
!         idx_d = NINT(1.0 + FLOAT(nbr) * DLOG(Dr_star/D0r)             &
!               / DLOG(Dr(nbr)/D0r))
!         idx_d = MAX(1, MIN(idx_d, nbr))
!
!         nir = NINT(ALOG10(rr(k)))
!         do nn = nir-1, nir+1
!            n = nn
!            if ( (rr(k)/10.**nn).ge.1.0 .and. &
!                 (rr(k)/10.**nn).lt.10.0) goto 154
!         enddo
!154      continue
!         idx_r = INT(rr(k)/10.**n) + 10*(n-nir2) - (n-nir2)
!         idx_r = MAX(1, MIN(idx_r, ntb_r))
!
!         lamr = (am_r*crg(3)*org2*nr(k)/rr(k))**obmr
!         lam_exp = lamr * (crg(3)*org2*org1)**bm_r
!         N0_exp = org1*rr(k)/am_r * lam_exp**cre(1)
!         nir = NINT(DLOG10(N0_exp))
!         do nn = nir-1, nir+1
!            n = nn
!            if ( (N0_exp/10.**nn).ge.1.0 .and. &
!                 (N0_exp/10.**nn).lt.10.0) goto 155
!         enddo
!155      continue
!         idx_r1 = INT(N0_exp/10.**n) + 10*(n-nir3) - (n-nir3)
!         idx_r1 = MAX(1, MIN(idx_r1, ntb_r1))
!
!         pnr_rev(k) = MIN(nr(k)*odts, SNGL(tnr_rev(idx_d,idx_r1,idx_r) &   ! RAIN2M
!                    * odts))

      end subroutine table_dropEvap
!
!ctrlL
!+---+-----------------------------------------------------------------+
!..Fill the table of CCN activation data created from parcel model run
!.. by Trude Eidhammer with inputs of aerosol number concentration,
!.. vertical velocity, temperature, lognormal mean aerosol radius, and
!.. hygroscopicity, kappa.  The data are read from external file and
!.. contain activated fraction of CCN for given conditions.
!+---+-----------------------------------------------------------------+

      subroutine table_ccnAct

      USE module_domain
      USE module_dm
      implicit none

      LOGICAL, EXTERNAL:: wrf_dm_on_monitor

!..Local variables
      INTEGER:: iunit_mp_th1, i
      LOGICAL:: opened
      CHARACTER*64 errmess

      iunit_mp_th1 = -1
      IF ( wrf_dm_on_monitor() ) THEN
        DO i = 20,99
          INQUIRE ( i , OPENED = opened )
          IF ( .NOT. opened ) THEN
            iunit_mp_th1 = i
            GOTO 2010
          ENDIF
        ENDDO
 2010   CONTINUE
      ENDIF
#if defined(DM_PARALLEL) && !defined(STUBMPI)
      CALL wrf_dm_bcast_bytes ( iunit_mp_th1 , IWORDSIZE )
#endif
      IF ( iunit_mp_th1 < 0 ) THEN
        CALL wrf_error_fatal ( 'module_mp_thompson: table_ccnAct: '//   &
           'Can not find unused fortran unit to read in lookup table.')
      ENDIF

      IF ( wrf_dm_on_monitor() ) THEN
        WRITE(errmess, '(A,I2)') 'module_mp_thompson: opening CCN_ACTIVATE.BIN on unit ',iunit_mp_th1
        CALL wrf_debug(150, errmess)
        OPEN(iunit_mp_th1,FILE='CCN_ACTIVATE.BIN',                      &
             FORM='UNFORMATTED',STATUS='OLD',ERR=9009)
      ENDIF

#define DM_BCAST_MACRO(A) CALL wrf_dm_bcast_bytes(A, size(A)*R4SIZE)

      IF ( wrf_dm_on_monitor() ) READ(iunit_mp_th1,ERR=9010) tnccn_act
#if defined(DM_PARALLEL) && !defined(STUBMPI)
      DM_BCAST_MACRO(tnccn_act)
#endif


      RETURN
 9009 CONTINUE
      WRITE( errmess , '(A,I2)' ) 'module_mp_thompson: error opening CCN_ACTIVATE.BIN on unit ',iunit_mp_th1
      CALL wrf_error_fatal(errmess)
      RETURN
 9010 CONTINUE
      WRITE( errmess , '(A,I2)' ) 'module_mp_thompson: error reading CCN_ACTIVATE.BIN on unit ',iunit_mp_th1
      CALL wrf_error_fatal(errmess)

      end subroutine table_ccnAct
!^L
!+---+-----------------------------------------------------------------+
!..Retrieve fraction of CCN that gets activated given the model temp,
!.. vertical velocity, and available CCN concentration.  The lookup
!.. table (read from external file) has CCN concentration varying the
!.. quickest, then updraft, then temperature, then mean aerosol radius,
!.. and finally hygroscopicity, kappa.
!.. TO_DO ITEM:  For radiation cooling producing fog, in which case the
!.. updraft velocity could easily be negative, we could use the temp
!.. and its tendency to diagnose a pretend postive updraft velocity.
!+---+-----------------------------------------------------------------+
      real function activ_ncloud(Tt, Ww, NCCN)

      implicit none
      REAL, INTENT(IN):: Tt, Ww, NCCN
      REAL:: n_local, w_local
      INTEGER:: i, j, k, l, m, n
      REAL:: A, B, C, D, t, u, x1, x2, y1, y2, nx, wy, fraction


!     ta_Na = (/10.0, 31.6, 100.0, 316.0, 1000.0, 3160.0, 10000.0/)  ntb_arc
!     ta_Ww = (/0.01, 0.0316, 0.1, 0.316, 1.0, 3.16, 10.0, 31.6, 100.0/)  ntb_arw
!     ta_Tk = (/243.15, 253.15, 263.15, 273.15, 283.15, 293.15, 303.15/)  ntb_art
!     ta_Ra = (/0.01, 0.02, 0.04, 0.08, 0.16/)  ntb_arr
!     ta_Ka = (/0.2, 0.4, 0.6, 0.8/)  ntb_ark

      n_local = NCCN * 1.E-6
      w_local = Ww

      if (n_local .ge. ta_Na(ntb_arc)) then
         n_local = ta_Na(ntb_arc) - 1.0
      elseif (n_local .le. ta_Na(1)) then
         n_local = ta_Na(1) + 1.0
      endif
      do n = 2, ntb_arc
         if (n_local.ge.ta_Na(n-1) .and. n_local.lt.ta_Na(n)) goto 8003
      enddo
 8003 continue
      i = n
      x1 = LOG(ta_Na(i-1))
      x2 = LOG(ta_Na(i))

      if (w_local .ge. ta_Ww(ntb_arw)) then
         w_local = ta_Ww(ntb_arw) - 1.0
      elseif (w_local .le. ta_Ww(1)) then
         w_local = ta_Ww(1) + 0.001
      endif
      do n = 2, ntb_arw
         if (w_local.ge.ta_Ww(n-1) .and. w_local.lt.ta_Ww(n)) goto 8005
      enddo
 8005 continue
      j = n
      y1 = LOG(ta_Ww(j-1))
      y2 = LOG(ta_Ww(j))

      k = MAX(1, MIN( NINT( (Tt - ta_Tk(1))*0.1) + 1, ntb_art))

!..The next two values are indexes of mean aerosol radius and
!.. hygroscopicity.  Currently these are constant but a future version
!.. should implement other variables to allow more freedom such as
!.. at least simple separation of tiny size sulfates from larger
!.. sea salts.
      l = 3
      m = 2

      A = tnccn_act(i-1,j-1,k,l,m)
      B = tnccn_act(i,j-1,k,l,m)
      C = tnccn_act(i,j,k,l,m)
      D = tnccn_act(i-1,j,k,l,m)
      nx = LOG(n_local)
      wy = LOG(w_local)

      t = (nx-x1)/(x2-x1)
      u = (wy-y1)/(y2-y1)

!     t = (n_local-ta(Na(i-1))/(ta_Na(i)-ta_Na(i-1))
!     u = (w_local-ta_Ww(j-1))/(ta_Ww(j)-ta_Ww(j-1))

      fraction = (1.0-t)*(1.0-u)*A + t*(1.0-u)*B + t*u*C + (1.0-t)*u*D

!     if (NCCN*fraction .gt. 0.75*Nt_c_max) then
!        write(*,*) ' DEBUG-GT ', n_local, w_local, Tt, i, j, k
!     endif

      activ_ncloud = NCCN*fraction

      end function activ_ncloud

!+---+-----------------------------------------------------------------+
!+---+-----------------------------------------------------------------+
      SUBROUTINE GCF(GAMMCF,A,X,GLN)
!     --- RETURNS THE INCOMPLETE GAMMA FUNCTION Q(A,X) EVALUATED BY ITS
!     --- CONTINUED FRACTION REPRESENTATION AS GAMMCF.  ALSO RETURNS
!     --- LN(GAMMA(A)) AS GLN.  THE CONTINUED FRACTION IS EVALUATED BY
!     --- A MODIFIED LENTZ METHOD.
!     --- USES GAMMLN
      IMPLICIT NONE
      INTEGER, PARAMETER:: ITMAX=100
      REAL, PARAMETER:: gEPS=3.E-7
      REAL, PARAMETER:: FPMIN=1.E-30
      REAL, INTENT(IN):: A, X
      REAL:: GAMMCF,GLN
      INTEGER:: I
      REAL:: AN,B,C,D,DEL,H
      GLN=GAMMLN(A)
      B=X+1.-A
      C=1./FPMIN
      D=1./B
      H=D
      DO 11 I=1,ITMAX
        AN=-I*(I-A)
        B=B+2.
        D=AN*D+B
        IF(ABS(D).LT.FPMIN)D=FPMIN
        C=B+AN/C
        IF(ABS(C).LT.FPMIN)C=FPMIN
        D=1./D
        DEL=D*C
        H=H*DEL
        IF(ABS(DEL-1.).LT.gEPS)GOTO 1
 11   CONTINUE
      PRINT *, 'A TOO LARGE, ITMAX TOO SMALL IN GCF'
 1    GAMMCF=EXP(-X+A*LOG(X)-GLN)*H
      END SUBROUTINE GCF
!  (C) Copr. 1986-92 Numerical Recipes Software 2.02
!+---+-----------------------------------------------------------------+
      SUBROUTINE GSER(GAMSER,A,X,GLN)
!     --- RETURNS THE INCOMPLETE GAMMA FUNCTION P(A,X) EVALUATED BY ITS
!     --- ITS SERIES REPRESENTATION AS GAMSER.  ALSO RETURNS LN(GAMMA(A)) 
!     --- AS GLN.
!     --- USES GAMMLN
      IMPLICIT NONE
      INTEGER, PARAMETER:: ITMAX=100
      REAL, PARAMETER:: gEPS=3.E-7
      REAL, INTENT(IN):: A, X
      REAL:: GAMSER,GLN
      INTEGER:: N
      REAL:: AP,DEL,SUM
      GLN=GAMMLN(A)
      IF(X.LE.0.)THEN
        IF(X.LT.0.) PRINT *, 'X < 0 IN GSER'
        GAMSER=0.
        RETURN
      ENDIF
      AP=A
      SUM=1./A
      DEL=SUM
      DO 11 N=1,ITMAX
        AP=AP+1.
        DEL=DEL*X/AP
        SUM=SUM+DEL
        IF(ABS(DEL).LT.ABS(SUM)*gEPS)GOTO 1
 11   CONTINUE
      PRINT *,'A TOO LARGE, ITMAX TOO SMALL IN GSER'
 1    GAMSER=SUM*EXP(-X+A*LOG(X)-GLN)
      END SUBROUTINE GSER
!  (C) Copr. 1986-92 Numerical Recipes Software 2.02
!+---+-----------------------------------------------------------------+
      REAL FUNCTION GAMMLN(XX)
!     --- RETURNS THE VALUE LN(GAMMA(XX)) FOR XX > 0.
      IMPLICIT NONE
      REAL, INTENT(IN):: XX
      DOUBLE PRECISION, PARAMETER:: STP = 2.5066282746310005D0
      DOUBLE PRECISION, DIMENSION(6), PARAMETER:: &
               COF = (/76.18009172947146D0, -86.50532032941677D0, &
                       24.01409824083091D0, -1.231739572450155D0, &
                      .1208650973866179D-2, -.5395239384953D-5/)
      DOUBLE PRECISION:: SER,TMP,X,Y
      INTEGER:: J

      X=XX
      Y=X
      TMP=X+5.5D0
      TMP=(X+0.5D0)*LOG(TMP)-TMP
      SER=1.000000000190015D0
      DO 11 J=1,6
        Y=Y+1.D0
        SER=SER+COF(J)/Y
11    CONTINUE
      GAMMLN=TMP+LOG(STP*SER/X)
      END FUNCTION GAMMLN
!  (C) Copr. 1986-92 Numerical Recipes Software 2.02
!+---+-----------------------------------------------------------------+
      REAL FUNCTION GAMMP(A,X)
!     --- COMPUTES THE INCOMPLETE GAMMA FUNCTION P(A,X)
!     --- SEE ABRAMOWITZ AND STEGUN 6.5.1
!     --- USES GCF,GSER
      IMPLICIT NONE
      REAL, INTENT(IN):: A,X
      REAL:: GAMMCF,GAMSER,GLN
      GAMMP = 0.
      IF((X.LT.0.) .OR. (A.LE.0.)) THEN
        PRINT *, 'BAD ARGUMENTS IN GAMMP'
        RETURN
      ELSEIF(X.LT.A+1.)THEN
        CALL GSER(GAMSER,A,X,GLN)
        GAMMP=GAMSER
      ELSE
        CALL GCF(GAMMCF,A,X,GLN)
        GAMMP=1.-GAMMCF
      ENDIF
      END FUNCTION GAMMP
!  (C) Copr. 1986-92 Numerical Recipes Software 2.02
!+---+-----------------------------------------------------------------+
      REAL FUNCTION WGAMMA(y)

      IMPLICIT NONE
      REAL, INTENT(IN):: y

      WGAMMA = EXP(GAMMLN(y))

      END FUNCTION WGAMMA
!+---+-----------------------------------------------------------------+
! THIS FUNCTION CALCULATES THE LIQUID SATURATION VAPOR MIXING RATIO AS
! A FUNCTION OF TEMPERATURE AND PRESSURE
!
      REAL FUNCTION RSLF(P,T)

      IMPLICIT NONE
      REAL, INTENT(IN):: P, T
      REAL:: ESL,X
      REAL, PARAMETER:: C0= .611583699E03
      REAL, PARAMETER:: C1= .444606896E02
      REAL, PARAMETER:: C2= .143177157E01
      REAL, PARAMETER:: C3= .264224321E-1
      REAL, PARAMETER:: C4= .299291081E-3
      REAL, PARAMETER:: C5= .203154182E-5
      REAL, PARAMETER:: C6= .702620698E-8
      REAL, PARAMETER:: C7= .379534310E-11
      REAL, PARAMETER:: C8=-.321582393E-13

      X=MAX(-80.,T-273.16)

!      ESL=612.2*EXP(17.67*X/(T-29.65))
      ESL=C0+X*(C1+X*(C2+X*(C3+X*(C4+X*(C5+X*(C6+X*(C7+X*C8)))))))
      RSLF=.622*ESL/(P-ESL)

!    ALTERNATIVE
!  ; Source: Murphy and Koop, Review of the vapour pressure of ice and
!             supercooled water for atmospheric applications, Q. J. R.
!             Meteorol. Soc (2005), 131, pp. 1539-1565.
!    ESL = EXP(54.842763 - 6763.22 / T - 4.210 * ALOG(T) + 0.000367 * T
!        + TANH(0.0415 * (T - 218.8)) * (53.878 - 1331.22
!        / T - 9.44523 * ALOG(T) + 0.014025 * T))

      END FUNCTION RSLF
!+---+-----------------------------------------------------------------+
! THIS FUNCTION CALCULATES THE ICE SATURATION VAPOR MIXING RATIO AS A
! FUNCTION OF TEMPERATURE AND PRESSURE
!
      REAL FUNCTION RSIF(P,T)

      IMPLICIT NONE
      REAL, INTENT(IN):: P, T
      REAL:: ESI,X
      REAL, PARAMETER:: C0= .609868993E03
      REAL, PARAMETER:: C1= .499320233E02
      REAL, PARAMETER:: C2= .184672631E01
      REAL, PARAMETER:: C3= .402737184E-1
      REAL, PARAMETER:: C4= .565392987E-3
      REAL, PARAMETER:: C5= .521693933E-5
      REAL, PARAMETER:: C6= .307839583E-7
      REAL, PARAMETER:: C7= .105785160E-9
      REAL, PARAMETER:: C8= .161444444E-12

      X=MAX(-80.,T-273.16)
      ESI=C0+X*(C1+X*(C2+X*(C3+X*(C4+X*(C5+X*(C6+X*(C7+X*C8)))))))
      RSIF=.622*ESI/(P-ESI)

!    ALTERNATIVE
!  ; Source: Murphy and Koop, Review of the vapour pressure of ice and
!             supercooled water for atmospheric applications, Q. J. R.
!             Meteorol. Soc (2005), 131, pp. 1539-1565.
!     ESI = EXP(9.550426 - 5723.265/T + 3.53068*ALOG(T) - 0.00728332*T)

      END FUNCTION RSIF

!+---+-----------------------------------------------------------------+
      real function iceDeMott(tempc, qv, qvs, qvsi, rho, nifa)
      implicit none

      REAL, INTENT(IN):: tempc, qv, qvs, qvsi, rho, nifa

!..Local vars
      REAL:: satw, sati, siw, p_x, si0x, dtt, dsi, dsw, dab, fc, hx
      REAL:: ntilde, n_in, nmax, nhat, mux, xni, nifa_cc
      REAL, PARAMETER:: p_c1    = 1000.
      REAL, PARAMETER:: p_rho_c = 0.76
      REAL, PARAMETER:: p_alpha = 1.0
      REAL, PARAMETER:: p_gam   = 2.
      REAL, PARAMETER:: delT    = 5.
      REAL, PARAMETER:: T0x     = -40.
      REAL, PARAMETER:: Sw0x    = 0.97
      REAL, PARAMETER:: delSi   = 0.1
      REAL, PARAMETER:: hdm     = 0.15
      REAL, PARAMETER:: p_psi   = 0.058707*p_gam/p_rho_c
      REAL, PARAMETER:: aap     = 1.
      REAL, PARAMETER:: bbp     = 0.
      REAL, PARAMETER:: y1p     = -35.
      REAL, PARAMETER:: y2p     = -25.
      REAL, PARAMETER:: rho_not0 = 101325./(287.05*273.15)

!+---+

      xni = 0.0
      satw = qv/qvs
      sati = qv/qvsi
      siw = qvs/qvsi
      p_x = -1.0261+(3.1656e-3*tempc)+(5.3938e-4*(tempc*tempc))         &
                 +  (8.2584e-6*(tempc*tempc*tempc))
      si0x = 1.+(10.**p_x)
      if (sati.ge.si0x .and. satw.lt.0.985) then
         dtt = delta_p (tempc, T0x, T0x+delT, 1., hdm)
         dsi = delta_p (sati, Si0x, Si0x+delSi, 0., 1.)
         dsw = delta_p (satw, Sw0x, 1., 0., 1.)
         fc = dtt*dsi*0.5
         hx = min(fc+((1.-fc)*dsw), 1.)
         ntilde = p_c1*p_gam*((exp(12.96*(sati-1.1)))**0.3) / p_rho_c
         if (tempc .le. y1p) then
            n_in = ntilde
         elseif (tempc .ge. y2p) then
            n_in = p_psi*p_c1*exp(12.96*(sati-1.)-0.639)
         else
            if (tempc .le. -30.) then
               nmax = p_c1*p_gam*(exp(12.96*(siw-1.1)))**0.3/p_rho_c
            else
               nmax = p_psi*p_c1*exp(12.96*(siw-1.)-0.639)
            endif
            ntilde = MIN(ntilde, nmax)
            nhat = MIN(p_psi*p_c1*exp(12.96*(sati-1.)-0.639), nmax)
            dab = delta_p (tempc, y1p, y2p, aap, bbp)
            n_in = MIN(nhat*(ntilde/nhat)**dab, nmax)
         endif
         mux = hx*p_alpha*n_in*rho
         xni = mux*((6700.*nifa)-200.)/((6700.*5.E5)-200.)
      elseif (satw.ge.0.985 .and. tempc.gt.HGFR-273.15) then
         nifa_cc = nifa*RHO_NOT0*1.E-6/rho
         xni  = 3.*nifa_cc**(1.25)*exp((0.46*(-tempc))-11.6)             !  [DeMott, 2015]
!        xni = (5.94e-5*(-tempc)**3.33)                                 &
!                   * (nifa_cc**((-0.0264*(tempc))+0.0033))
         xni = xni*rho/RHO_NOT0 * 1000.
      endif

      iceDeMott = MAX(0., xni)

      end FUNCTION iceDeMott

!+---+-----------------------------------------------------------------+
!..Newer research since Koop et al (2001) suggests that the freezing
!.. rate should be lower than original paper, so J_rate is reduced
!.. by two orders of magnitude.

      real function iceKoop(temp, qv, qvs, naero, dt)
      implicit none

      REAL, INTENT(IN):: temp, qv, qvs, naero, DT
      REAL:: mu_diff, a_w_i, delta_aw, log_J_rate, J_rate, prob_h, satw
      REAL:: xni

      xni = 0.0
      satw = qv/qvs
      mu_diff    = 210368.0 + (131.438*temp) - (3.32373E6/temp)         &
     &           - (41729.1*alog(temp))
      a_w_i      = exp(mu_diff/(R_uni*temp))
      delta_aw   = satw - a_w_i
      log_J_rate = -906.7 + (8502.0*delta_aw)                           &
     &           - (26924.0*delta_aw*delta_aw)                          &
     &           + (29180.0*delta_aw*delta_aw*delta_aw)
      log_J_rate = MIN(20.0, log_J_rate)
      J_rate     = 0.01*(10.**log_J_rate)                                ! cm-3 s-1
      prob_h     = MIN(1.-exp(-J_rate*ar_volume*DT), 1.)
      if (prob_h .gt. 0.) then
         xni     = MIN(prob_h*naero, 1000.E3)
      endif

      iceKoop = MAX(0.0, xni)

      end FUNCTION iceKoop

!+---+-----------------------------------------------------------------+
!.. Helper routine for Phillips et al (2008) ice nucleation.  Trude

      REAL FUNCTION delta_p (yy, y1, y2, aa, bb)
      IMPLICIT NONE

      REAL, INTENT(IN):: yy, y1, y2, aa, bb
      REAL:: dab, A, B, a0, a1, a2, a3

      A   = 6.*(aa-bb)/((y2-y1)*(y2-y1)*(y2-y1))
      B   = aa+(A*y1*y1*y1/6.)-(A*y1*y1*y2*0.5)
      a0  = B
      a1  = A*y1*y2
      a2  = -A*(y1+y2)*0.5
      a3  = A/3.

      if (yy.le.y1) then 
         dab = aa
      else if (yy.ge.y2) then
         dab = bb
      else
         dab = a0+(a1*yy)+(a2*yy*yy)+(a3*yy*yy*yy)
      endif

      if (dab.lt.aa) then 
         dab = aa
      endif
      if (dab.gt.bb) then 
         dab = bb
      endif
      delta_p = dab

      END FUNCTION delta_p 

!+---+-----------------------------------------------------------------+
!ctrlL

!+---+-----------------------------------------------------------------+
!..Compute _radiation_ effective radii of cloud water, ice, and snow.
!.. These are entirely consistent with microphysics assumptions, not
!.. constant or otherwise ad hoc as is internal to most radiation
!.. schemes.  Since only the smallest snowflakes should impact
!.. radiation, compute from first portion of complicated Field number
!.. distribution, not the second part, which is the larger sizes.
!+---+-----------------------------------------------------------------+

      subroutine calc_effectRad (t1d, p1d, qv1d, qc1d, nc1d, qi1d, ni1d, qs1d,   &
     &                re_qc1d, re_qi1d, re_qs1d, kts, kte)

      IMPLICIT NONE

!..Sub arguments
      INTEGER, INTENT(IN):: kts, kte
      REAL, DIMENSION(kts:kte), INTENT(IN)::                            &
     &                    t1d, p1d, qv1d, qc1d, nc1d, qi1d, ni1d, qs1d
      REAL, DIMENSION(kts:kte), INTENT(INOUT):: re_qc1d, re_qi1d, re_qs1d
!..Local variables
      INTEGER:: k
      REAL, DIMENSION(kts:kte):: rho, rc, nc, ri, ni, rs
      REAL:: smo2, smob, smoc
      REAL:: tc0, loga_, a_, b_
      DOUBLE PRECISION:: lamc, lami
      LOGICAL:: has_qc, has_qi, has_qs
      INTEGER:: inu_c
      real, dimension(15), parameter:: g_ratio = (/24,60,120,210,336,   &
     &                504,720,990,1320,1716,2184,2730,3360,4080,4896/)

      has_qc = .false.
      has_qi = .false.
      has_qs = .false.

      do k = kts, kte
         rho(k) = 0.622*p1d(k)/(R*t1d(k)*(qv1d(k)+0.622))
         rc(k) = MAX(R1, qc1d(k)*rho(k))
         nc(k) = MAX(R2, nc1d(k)*rho(k))
         if (.NOT. is_aerosol_aware) nc(k) = Nt_c
         if (rc(k).gt.R1 .and. nc(k).gt.R2) has_qc = .true.
         ri(k) = MAX(R1, qi1d(k)*rho(k))
         ni(k) = MAX(R2, ni1d(k)*rho(k))
         if (ri(k).gt.R1 .and. ni(k).gt.R2) has_qi = .true.
         rs(k) = MAX(R1, qs1d(k)*rho(k))
         if (rs(k).gt.R1) has_qs = .true.
      enddo

      if (has_qc) then
      do k = kts, kte
         if (rc(k).le.R1 .or. nc(k).le.R2) CYCLE
         if (nc(k).lt.100) then
            inu_c = 15
         elseif (nc(k).gt.1.E10) then
            inu_c = 2
         else
            inu_c = MIN(15, NINT(1000.E6/nc(k)) + 2)
         endif
         lamc = (nc(k)*am_r*g_ratio(inu_c)/rc(k))**obmr
         re_qc1d(k) = MAX(2.51E-6, MIN(SNGL(0.5D0 * DBLE(3.+inu_c)/lamc), 50.E-6))
      enddo
      endif

      if (has_qi) then
      do k = kts, kte
         if (ri(k).le.R1 .or. ni(k).le.R2) CYCLE
         lami = (am_i*cig(2)*oig1*ni(k)/ri(k))**obmi
         re_qi1d(k) = MAX(10.01E-6, MIN(SNGL(0.5D0 * DBLE(3.+mu_i)/lami), 125.E-6))
      enddo
      endif

      if (has_qs) then
      do k = kts, kte
         if (rs(k).le.R1) CYCLE
         tc0 = MIN(-0.1, t1d(k)-273.15)
         smob = rs(k)*oams

!..All other moments based on reference, 2nd moment.  If bm_s.ne.2,
!.. then we must compute actual 2nd moment and use as reference.
         if (bm_s.gt.(2.0-1.e-3) .and. bm_s.lt.(2.0+1.e-3)) then
            smo2 = smob
         else
            loga_ = sa(1) + sa(2)*tc0 + sa(3)*bm_s &
     &         + sa(4)*tc0*bm_s + sa(5)*tc0*tc0 &
     &         + sa(6)*bm_s*bm_s + sa(7)*tc0*tc0*bm_s &
     &         + sa(8)*tc0*bm_s*bm_s + sa(9)*tc0*tc0*tc0 &
     &         + sa(10)*bm_s*bm_s*bm_s
            a_ = 10.0**loga_
            b_ = sb(1) + sb(2)*tc0 + sb(3)*bm_s &
     &         + sb(4)*tc0*bm_s + sb(5)*tc0*tc0 &
     &         + sb(6)*bm_s*bm_s + sb(7)*tc0*tc0*bm_s &
     &         + sb(8)*tc0*bm_s*bm_s + sb(9)*tc0*tc0*tc0 &
     &         + sb(10)*bm_s*bm_s*bm_s
            smo2 = (smob/a_)**(1./b_)
         endif
!..Calculate bm_s+1 (th) moment.  Useful for diameter calcs.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(1) &
     &         + sa(4)*tc0*cse(1) + sa(5)*tc0*tc0 &
     &         + sa(6)*cse(1)*cse(1) + sa(7)*tc0*tc0*cse(1) &
     &         + sa(8)*tc0*cse(1)*cse(1) + sa(9)*tc0*tc0*tc0 &
     &         + sa(10)*cse(1)*cse(1)*cse(1)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(1) + sb(4)*tc0*cse(1) &
     &        + sb(5)*tc0*tc0 + sb(6)*cse(1)*cse(1) &
     &        + sb(7)*tc0*tc0*cse(1) + sb(8)*tc0*cse(1)*cse(1) &
     &        + sb(9)*tc0*tc0*tc0 + sb(10)*cse(1)*cse(1)*cse(1)
         smoc = a_ * smo2**b_
         re_qs1d(k) = MAX(10.E-6, MIN(0.5*(smoc/smob), 999.E-6))
      enddo
      endif

      end subroutine calc_effectRad

!+---+-----------------------------------------------------------------+
!..Compute radar reflectivity assuming 10 cm wavelength radar and using
!.. Rayleigh approximation.  Only complication is melted snow/graupel
!.. which we treat as water-coated ice spheres and use Uli Blahak's
!.. library of routines.  The meltwater fraction is simply the amount
!.. of frozen species remaining from what initially existed at the
!.. melting level interface.
!+---+-----------------------------------------------------------------+

      subroutine calc_refl10cm (qv1d, qc1d, qr1d, nr1d, qs1d, qg1d,     &
                          t1d, p1d, dBZ, kts, kte, ii, jj)

      IMPLICIT NONE

!..Sub arguments
      INTEGER, INTENT(IN):: kts, kte, ii, jj
      REAL, DIMENSION(kts:kte), INTENT(IN)::                            &
                          qv1d, qc1d, qr1d, nr1d, qs1d, qg1d, t1d, p1d
      REAL, DIMENSION(kts:kte), INTENT(INOUT):: dBZ
!     REAL, DIMENSION(kts:kte), INTENT(INOUT):: vt_dBZ

!..Local variables
      REAL, DIMENSION(kts:kte):: temp, pres, qv, rho, rhof
      REAL, DIMENSION(kts:kte):: rc, rr, nr, rs, rg

      DOUBLE PRECISION, DIMENSION(kts:kte):: ilamr, ilamg, N0_r, N0_g
      REAL, DIMENSION(kts:kte):: mvd_r
      REAL, DIMENSION(kts:kte):: smob, smo2, smoc, smoz
      REAL:: oM3, M0, Mrat, slam1, slam2, xDs
      REAL:: ils1, ils2, t1_vts, t2_vts, t3_vts, t4_vts
      REAL:: vtr_dbz_wt, vts_dbz_wt, vtg_dbz_wt

      REAL, DIMENSION(kts:kte):: ze_rain, ze_snow, ze_graupel

      DOUBLE PRECISION:: N0_exp, N0_min, lam_exp, lamr, lamg
      REAL:: a_, b_, loga_, tc0
      DOUBLE PRECISION:: fmelt_s, fmelt_g

      INTEGER:: i, k, k_0, kbot, n
      LOGICAL:: melti
      LOGICAL, DIMENSION(kts:kte):: L_qr, L_qs, L_qg

      DOUBLE PRECISION:: cback, x, eta, f_d
      REAL:: xslw1, ygra1, zans1

!+---+

      do k = kts, kte
         dBZ(k) = -35.0
      enddo

!+---+-----------------------------------------------------------------+
!..Put column of data into local arrays.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         temp(k) = t1d(k)
         qv(k) = MAX(1.E-10, qv1d(k))
         pres(k) = p1d(k)
         rho(k) = 0.622*pres(k)/(R*temp(k)*(qv(k)+0.622))
         rhof(k) = SQRT(RHO_NOT/rho(k))
         rc(k) = MAX(R1, qc1d(k)*rho(k))
         if (qr1d(k) .gt. R1) then
            rr(k) = qr1d(k)*rho(k)
            nr(k) = MAX(R2, nr1d(k)*rho(k))
            lamr = (am_r*crg(3)*org2*nr(k)/rr(k))**obmr
            ilamr(k) = 1./lamr
            N0_r(k) = nr(k)*org2*lamr**cre(2)
            mvd_r(k) = (3.0 + mu_r + 0.672) * ilamr(k)
            L_qr(k) = .true.
         else
            rr(k) = R1
            nr(k) = R1
            mvd_r(k) = 50.E-6
            L_qr(k) = .false.
         endif
         if (qs1d(k) .gt. R2) then
            rs(k) = qs1d(k)*rho(k)
            L_qs(k) = .true.
         else
            rs(k) = R1
            L_qs(k) = .false.
         endif
         if (qg1d(k) .gt. R2) then
            rg(k) = qg1d(k)*rho(k)
            L_qg(k) = .true.
         else
            rg(k) = R1
            L_qg(k) = .false.
         endif
      enddo

!+---+-----------------------------------------------------------------+
!..Calculate y-intercept, slope, and useful moments for snow.
!+---+-----------------------------------------------------------------+
      do k = kts, kte
         tc0 = MIN(-0.1, temp(k)-273.15)
         smob(k) = rs(k)*oams

!..All other moments based on reference, 2nd moment.  If bm_s.ne.2,
!.. then we must compute actual 2nd moment and use as reference.
         if (bm_s.gt.(2.0-1.e-3) .and. bm_s.lt.(2.0+1.e-3)) then
            smo2(k) = smob(k)
         else
            loga_ = sa(1) + sa(2)*tc0 + sa(3)*bm_s &
     &         + sa(4)*tc0*bm_s + sa(5)*tc0*tc0 &
     &         + sa(6)*bm_s*bm_s + sa(7)*tc0*tc0*bm_s &
     &         + sa(8)*tc0*bm_s*bm_s + sa(9)*tc0*tc0*tc0 &
     &         + sa(10)*bm_s*bm_s*bm_s
            a_ = 10.0**loga_
            b_ = sb(1) + sb(2)*tc0 + sb(3)*bm_s &
     &         + sb(4)*tc0*bm_s + sb(5)*tc0*tc0 &
     &         + sb(6)*bm_s*bm_s + sb(7)*tc0*tc0*bm_s &
     &         + sb(8)*tc0*bm_s*bm_s + sb(9)*tc0*tc0*tc0 &
     &         + sb(10)*bm_s*bm_s*bm_s
            smo2(k) = (smob(k)/a_)**(1./b_)
         endif

!..Calculate bm_s+1 (th) moment.  Useful for diameter calcs.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(1) &
     &         + sa(4)*tc0*cse(1) + sa(5)*tc0*tc0 &
     &         + sa(6)*cse(1)*cse(1) + sa(7)*tc0*tc0*cse(1) &
     &         + sa(8)*tc0*cse(1)*cse(1) + sa(9)*tc0*tc0*tc0 &
     &         + sa(10)*cse(1)*cse(1)*cse(1)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(1) + sb(4)*tc0*cse(1) &
     &        + sb(5)*tc0*tc0 + sb(6)*cse(1)*cse(1) &
     &        + sb(7)*tc0*tc0*cse(1) + sb(8)*tc0*cse(1)*cse(1) &
     &        + sb(9)*tc0*tc0*tc0 + sb(10)*cse(1)*cse(1)*cse(1)
         smoc(k) = a_ * smo2(k)**b_

!..Calculate bm_s*2 (th) moment.  Useful for reflectivity.
         loga_ = sa(1) + sa(2)*tc0 + sa(3)*cse(3) &
     &         + sa(4)*tc0*cse(3) + sa(5)*tc0*tc0 &
     &         + sa(6)*cse(3)*cse(3) + sa(7)*tc0*tc0*cse(3) &
     &         + sa(8)*tc0*cse(3)*cse(3) + sa(9)*tc0*tc0*tc0 &
     &         + sa(10)*cse(3)*cse(3)*cse(3)
         a_ = 10.0**loga_
         b_ = sb(1)+ sb(2)*tc0 + sb(3)*cse(3) + sb(4)*tc0*cse(3) &
     &        + sb(5)*tc0*tc0 + sb(6)*cse(3)*cse(3) &
     &        + sb(7)*tc0*tc0*cse(3) + sb(8)*tc0*cse(3)*cse(3) &
     &        + sb(9)*tc0*tc0*tc0 + sb(10)*cse(3)*cse(3)*cse(3)
         smoz(k) = a_ * smo2(k)**b_
      enddo

!+---+-----------------------------------------------------------------+
!..Calculate y-intercept, slope values for graupel.
!+---+-----------------------------------------------------------------+

      N0_min = gonv_max
      do k = kte, kts, -1
         if (temp(k).lt.270.65 .and. L_qr(k) .and. mvd_r(k).gt.100.E-6) then
            xslw1 = 4.01 + alog10(mvd_r(k))
         else
            xslw1 = 0.01
         endif
         ygra1 = 4.31 + alog10(max(5.E-5, rg(k)))
         zans1 = 3.1 + (100./(300.*xslw1*ygra1/(10./xslw1+1.+0.25*ygra1)+30.+10.*ygra1))
         N0_exp = 10.**(zans1)
         N0_exp = MAX(DBLE(gonv_min), MIN(N0_exp, DBLE(gonv_max)))
         N0_min = MIN(N0_exp, N0_min)
         N0_exp = N0_min
         lam_exp = (N0_exp*am_g*cgg(1)/rg(k))**oge1
         lamg = lam_exp * (cgg(3)*ogg2*ogg1)**obmg
         ilamg(k) = 1./lamg
         N0_g(k) = N0_exp/(cgg(2)*lam_exp) * lamg**cge(2)
      enddo

!+---+-----------------------------------------------------------------+
!..Locate K-level of start of melting (k_0 is level above).
!+---+-----------------------------------------------------------------+
      melti = .false.
      k_0 = kts
      do k = kte-1, kts, -1
         if ( (temp(k).gt.273.15) .and. L_qr(k)                         &
     &                            .and. (L_qs(k+1).or.L_qg(k+1)) ) then
            k_0 = MAX(k+1, k_0)
            melti=.true.
            goto 195
         endif
      enddo
 195  continue

!+---+-----------------------------------------------------------------+
!..Assume Rayleigh approximation at 10 cm wavelength. Rain (all temps)
!.. and non-water-coated snow and graupel when below freezing are
!.. simple. Integrations of m(D)*m(D)*N(D)*dD.
!+---+-----------------------------------------------------------------+

      do k = kts, kte
         ze_rain(k) = 1.e-22
         ze_snow(k) = 1.e-22
         ze_graupel(k) = 1.e-22
         if (L_qr(k)) ze_rain(k) = N0_r(k)*crg(4)*ilamr(k)**cre(4)
         if (L_qs(k)) ze_snow(k) = (0.176/0.93) * (6.0/PI)*(6.0/PI)     &
     &                           * (am_s/900.0)*(am_s/900.0)*smoz(k)
         if (L_qg(k)) ze_graupel(k) = (0.176/0.93) * (6.0/PI)*(6.0/PI)  &
     &                              * (am_g/900.0)*(am_g/900.0)         &
     &                              * N0_g(k)*cgg(4)*ilamg(k)**cge(4)
      enddo

!+---+-----------------------------------------------------------------+
!..Special case of melting ice (snow/graupel) particles.  Assume the
!.. ice is surrounded by the liquid water.  Fraction of meltwater is
!.. extremely simple based on amount found above the melting level.
!.. Uses code from Uli Blahak (rayleigh_soak_wetgraupel and supporting
!.. routines).
!+---+-----------------------------------------------------------------+

      if (.not. iiwarm .and. melti .and. k_0.ge.2) then
       do k = k_0-1, kts, -1

!..Reflectivity contributed by melting snow
          if (L_qs(k) .and. L_qs(k_0) ) then
           fmelt_s = MAX(0.05d0, MIN(1.0d0-rs(k)/rs(k_0), 0.99d0))
           eta = 0.d0
           oM3 = 1./smoc(k)
           M0 = (smob(k)*oM3)
           Mrat = smob(k)*M0*M0*M0
           slam1 = M0 * Lam0
           slam2 = M0 * Lam1
           do n = 1, nrbins
              x = am_s * xxDs(n)**bm_s
              call rayleigh_soak_wetgraupel (x, DBLE(ocms), DBLE(obms), &
     &              fmelt_s, melt_outside_s, m_w_0, m_i_0, lamda_radar, &
     &              CBACK, mixingrulestring_s, matrixstring_s,          &
     &              inclusionstring_s, hoststring_s,                    &
     &              hostmatrixstring_s, hostinclusionstring_s)
              f_d = Mrat*(Kap0*DEXP(-slam1*xxDs(n))                     &
     &              + Kap1*(M0*xxDs(n))**mu_s * DEXP(-slam2*xxDs(n)))
              eta = eta + f_d * CBACK * simpson(n) * xdts(n)
           enddo
           ze_snow(k) = SNGL(lamda4 / (pi5 * K_w) * eta)
          endif

!..Reflectivity contributed by melting graupel

          if (L_qg(k) .and. L_qg(k_0) ) then
           fmelt_g = MAX(0.05d0, MIN(1.0d0-rg(k)/rg(k_0), 0.99d0))
           eta = 0.d0
           lamg = 1./ilamg(k)
           do n = 1, nrbins
              x = am_g * xxDg(n)**bm_g
              call rayleigh_soak_wetgraupel (x, DBLE(ocmg), DBLE(obmg), &
     &              fmelt_g, melt_outside_g, m_w_0, m_i_0, lamda_radar, &
     &              CBACK, mixingrulestring_g, matrixstring_g,          &
     &              inclusionstring_g, hoststring_g,                    &
     &              hostmatrixstring_g, hostinclusionstring_g)
              f_d = N0_g(k)*xxDg(n)**mu_g * DEXP(-lamg*xxDg(n))
              eta = eta + f_d * CBACK * simpson(n) * xdtg(n)
           enddo
           ze_graupel(k) = SNGL(lamda4 / (pi5 * K_w) * eta)
          endif

       enddo
      endif

      do k = kte, kts, -1
         dBZ(k) = 10.*log10((ze_rain(k)+ze_snow(k)+ze_graupel(k))*1.d18)
      enddo


!..Reflectivity-weighted terminal velocity (snow, rain, graupel, mix).
!     do k = kte, kts, -1
!        vt_dBZ(k) = 1.E-3
!        if (rs(k).gt.R2) then
!         Mrat = smob(k) / smoc(k)
!         ils1 = 1./(Mrat*Lam0 + fv_s)
!         ils2 = 1./(Mrat*Lam1 + fv_s)
!         t1_vts = Kap0*csg(5)*ils1**cse(5)
!         t2_vts = Kap1*Mrat**mu_s*csg(11)*ils2**cse(11)
!         ils1 = 1./(Mrat*Lam0)
!         ils2 = 1./(Mrat*Lam1)
!         t3_vts = Kap0*csg(6)*ils1**cse(6)
!         t4_vts = Kap1*Mrat**mu_s*csg(12)*ils2**cse(12)
!         vts_dbz_wt = rhof(k)*av_s * (t1_vts+t2_vts)/(t3_vts+t4_vts)
!         if (temp(k).ge.273.15 .and. temp(k).lt.275.15) then
!            vts_dbz_wt = vts_dbz_wt*1.5
!         elseif (temp(k).ge.275.15) then
!            vts_dbz_wt = vts_dbz_wt*2.0
!         endif
!        else
!         vts_dbz_wt = 1.E-3
!        endif

!        if (rr(k).gt.R1) then
!         lamr = 1./ilamr(k)
!         vtr_dbz_wt = rhof(k)*av_r*crg(13)*(lamr+fv_r)**(-cre(13))      &
!    &               / (crg(4)*lamr**(-cre(4)))
!        else
!         vtr_dbz_wt = 1.E-3
!        endif

!        if (rg(k).gt.R2) then
!         lamg = 1./ilamg(k)
!         vtg_dbz_wt = rhof(k)*av_g*cgg(5)*lamg**(-cge(5))               &
!    &               / (cgg(4)*lamg**(-cge(4)))
!        else
!         vtg_dbz_wt = 1.E-3
!        endif

!        vt_dBZ(k) = (vts_dbz_wt*ze_snow(k) + vtr_dbz_wt*ze_rain(k)      &
!    &                + vtg_dbz_wt*ze_graupel(k))                        &
!    &                / (ze_rain(k)+ze_snow(k)+ze_graupel(k))
!     enddo

      end subroutine calc_refl10cm
!
!+---+-----------------------------------------------------------------+

!+---+-----------------------------------------------------------------+
END MODULE module_mp_thompson
!+---+-----------------------------------------------------------------+
