| [1585] | 1 | ! path: $Source: /storm/rc1/cvsroot/rc/rrtmg_lw/src/rrtmg_lw_cldprop.f90,v $ |
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| 2 | ! author: $Author: miacono $ |
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| 3 | ! revision: $Revision: 1.9 $ |
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| 4 | ! created: $Date: 2011/04/08 20:25:00 $ |
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| 5 | ! |
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| 6 | module rrtmg_lw_cldprop |
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| 7 | |
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| 8 | ! -------------------------------------------------------------------------- |
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| 9 | ! | | |
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| 10 | ! | Copyright 2002-2009, Atmospheric & Environmental Research, Inc. (AER). | |
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| 11 | ! | This software may be used, copied, or redistributed as long as it is | |
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| 12 | ! | not sold and this copyright notice is reproduced on each copy made. | |
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| 13 | ! | This model is provided as is without any express or implied warranties. | |
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| 14 | ! | (http://www.rtweb.aer.com/) | |
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| 15 | ! | | |
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| 16 | ! -------------------------------------------------------------------------- |
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| 17 | |
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| 18 | ! --------- Modules ---------- |
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| 19 | |
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| 20 | use parkind, only : im => kind_im, rb => kind_rb |
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| 21 | use parrrtm, only : nbndlw |
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| 22 | use rrlw_cld, only: abscld1, absliq0, absliq1, & |
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| 23 | absice0, absice1, absice2, absice3 |
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| 24 | use rrlw_vsn, only: hvrcld, hnamcld |
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| 25 | |
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| 26 | implicit none |
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| 27 | |
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| 28 | contains |
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| 29 | |
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| 30 | ! ------------------------------------------------------------------------------ |
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| 31 | subroutine cldprop(nlayers, inflag, iceflag, liqflag, cldfrac, tauc, & |
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| 32 | ciwp, clwp, rei, rel, ncbands, taucloud) |
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| 33 | ! ------------------------------------------------------------------------------ |
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| 34 | |
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| 35 | ! Purpose: Compute the cloud optical depth(s) for each cloudy layer. |
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| 36 | |
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| 37 | ! ------- Input ------- |
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| 38 | |
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| 39 | integer(kind=im), intent(in) :: nlayers ! total number of layers |
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| 40 | integer(kind=im), intent(in) :: inflag ! see definitions |
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| 41 | integer(kind=im), intent(in) :: iceflag ! see definitions |
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| 42 | integer(kind=im), intent(in) :: liqflag ! see definitions |
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| 43 | |
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| 44 | real(kind=rb), intent(in) :: cldfrac(:) ! cloud fraction |
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| 45 | ! Dimensions: (nlayers) |
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| 46 | real(kind=rb), intent(in) :: ciwp(:) ! cloud ice water path |
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| 47 | ! Dimensions: (nlayers) |
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| 48 | real(kind=rb), intent(in) :: clwp(:) ! cloud liquid water path |
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| 49 | ! Dimensions: (nlayers) |
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| 50 | real(kind=rb), intent(in) :: rei(:) ! cloud ice particle effective size (microns) |
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| 51 | ! Dimensions: (nlayers) |
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| 52 | ! specific definition of rei depends on setting of iceflag: |
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| 53 | ! iceflag = 0: ice effective radius, r_ec, (Ebert and Curry, 1992), |
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| 54 | ! r_ec must be >= 10.0 microns |
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| 55 | ! iceflag = 1: ice effective radius, r_ec, (Ebert and Curry, 1992), |
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| 56 | ! r_ec range is limited to 13.0 to 130.0 microns |
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| 57 | ! iceflag = 2: ice effective radius, r_k, (Key, Streamer Ref. Manual, 1996) |
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| 58 | ! r_k range is limited to 5.0 to 131.0 microns |
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| 59 | ! iceflag = 3: generalized effective size, dge, (Fu, 1996), |
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| 60 | ! dge range is limited to 5.0 to 140.0 microns |
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| 61 | ! [dge = 1.0315 * r_ec] |
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| 62 | real(kind=rb), intent(in) :: rel(:) ! cloud liquid particle effective radius (microns) |
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| 63 | ! Dimensions: (nlayers) |
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| 64 | real(kind=rb), intent(in) :: tauc(:,:) ! cloud optical depth |
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| 65 | ! Dimensions: (nbndlw,nlayers) |
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| 66 | |
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| 67 | ! ------- Output ------- |
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| 68 | |
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| 69 | integer(kind=im), intent(out) :: ncbands ! number of cloud spectral bands |
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| 70 | real(kind=rb), intent(out) :: taucloud(:,:) ! cloud optical depth |
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| 71 | ! Dimensions: (nlayers,nbndlw) |
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| 72 | |
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| 73 | ! ------- Local ------- |
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| 74 | |
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| 75 | integer(kind=im) :: lay ! Layer index |
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| 76 | integer(kind=im) :: ib ! spectral band index |
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| 77 | integer(kind=im) :: index |
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| 78 | integer(kind=im) :: iceind |
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| 79 | integer(kind=im) :: liqind |
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| 80 | integer(kind=im) :: icb(nbndlw,0:2) |
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| 81 | |
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| 82 | real(kind=rb) :: abscoice(nbndlw) ! ice absorption coefficients |
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| 83 | real(kind=rb) :: abscoliq(nbndlw) ! liquid absorption coefficients |
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| 84 | real(kind=rb) :: cwp ! cloud water path |
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| 85 | real(kind=rb) :: radliq ! cloud liquid droplet radius (microns) |
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| 86 | real(kind=rb) :: radice ! cloud ice effective size (microns) |
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| 87 | real(kind=rb) :: factor ! |
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| 88 | real(kind=rb) :: fint ! |
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| 89 | real(kind=rb) :: tauctot(nlayers) ! band integrated cloud optical depth |
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| 90 | real(kind=rb), parameter :: eps = 1.e-6_rb ! epsilon |
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| 91 | real(kind=rb), parameter :: cldmin = 1.e-20_rb ! minimum value for cloud quantities |
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| 92 | |
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| 93 | ! ------- Definitions ------- |
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| 94 | |
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| 95 | ! Explanation of the method for each value of INFLAG. Values of |
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| 96 | ! 0 or 1 for INFLAG do not distingish being liquid and ice clouds. |
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| 97 | ! INFLAG = 2 does distinguish between liquid and ice clouds, and |
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| 98 | ! requires further user input to specify the method to be used to |
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| 99 | ! compute the aborption due to each. |
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| 100 | ! INFLAG = 0: For each cloudy layer, the cloud fraction and (gray) |
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| 101 | ! optical depth are input. |
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| 102 | ! INFLAG = 1: For each cloudy layer, the cloud fraction and cloud |
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| 103 | ! water path (g/m2) are input. The (gray) cloud optical |
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| 104 | ! depth is computed as in CCM2. |
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| 105 | ! INFLAG = 2: For each cloudy layer, the cloud fraction, cloud |
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| 106 | ! water path (g/m2), and cloud ice fraction are input. |
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| 107 | ! ICEFLAG = 0: The ice effective radius (microns) is input and the |
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| 108 | ! optical depths due to ice clouds are computed as in CCM3. |
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| 109 | ! ICEFLAG = 1: The ice effective radius (microns) is input and the |
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| 110 | ! optical depths due to ice clouds are computed as in |
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| 111 | ! Ebert and Curry, JGR, 97, 3831-3836 (1992). The |
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| 112 | ! spectral regions in this work have been matched with |
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| 113 | ! the spectral bands in RRTM to as great an extent |
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| 114 | ! as possible: |
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| 115 | ! E&C 1 IB = 5 RRTM bands 9-16 |
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| 116 | ! E&C 2 IB = 4 RRTM bands 6-8 |
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| 117 | ! E&C 3 IB = 3 RRTM bands 3-5 |
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| 118 | ! E&C 4 IB = 2 RRTM band 2 |
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| 119 | ! E&C 5 IB = 1 RRTM band 1 |
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| 120 | ! ICEFLAG = 2: The ice effective radius (microns) is input and the |
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| 121 | ! optical properties due to ice clouds are computed from |
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| 122 | ! the optical properties stored in the RT code, |
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| 123 | ! STREAMER v3.0 (Reference: Key. J., Streamer |
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| 124 | ! User's Guide, Cooperative Institute for |
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| 125 | ! Meteorological Satellite Studies, 2001, 96 pp.). |
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| 126 | ! Valid range of values for re are between 5.0 and |
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| 127 | ! 131.0 micron. |
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| 128 | ! ICEFLAG = 3: The ice generalized effective size (dge) is input |
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| 129 | ! and the optical properties, are calculated as in |
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| 130 | ! Q. Fu, J. Climate, (1998). Q. Fu provided high resolution |
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| 131 | ! tables which were appropriately averaged for the |
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| 132 | ! bands in RRTM_LW. Linear interpolation is used to |
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| 133 | ! get the coefficients from the stored tables. |
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| 134 | ! Valid range of values for dge are between 5.0 and |
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| 135 | ! 140.0 micron. |
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| 136 | ! LIQFLAG = 0: The optical depths due to water clouds are computed as |
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| 137 | ! in CCM3. |
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| 138 | ! LIQFLAG = 1: The water droplet effective radius (microns) is input |
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| 139 | ! and the optical depths due to water clouds are computed |
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| 140 | ! as in Hu and Stamnes, J., Clim., 6, 728-742, (1993). |
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| 141 | ! The values for absorption coefficients appropriate for |
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| 142 | ! the spectral bands in RRTM have been obtained for a |
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| 143 | ! range of effective radii by an averaging procedure |
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| 144 | ! based on the work of J. Pinto (private communication). |
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| 145 | ! Linear interpolation is used to get the absorption |
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| 146 | ! coefficients for the input effective radius. |
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| 147 | |
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| 148 | data icb /1,1,1,1,1,1,1,1,1, 1, 1, 1, 1, 1, 1, 1, & |
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| 149 | 1,2,3,3,3,4,4,4,5, 5, 5, 5, 5, 5, 5, 5, & |
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| 150 | 1,2,3,4,5,6,7,8,9,10,11,12,13,14,15,16/ |
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| 151 | |
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| 152 | hvrcld = '$Revision: 1.9 $' |
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| 153 | |
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| 154 | ncbands = 1 |
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| 155 | tauctot(:) = 0._rb |
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| 156 | |
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| 157 | do lay = 1, nlayers |
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| 158 | do ib = 1, nbndlw |
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| 159 | taucloud(lay,ib) = 0.0_rb |
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| 160 | tauctot(lay) = tauctot(lay) + tauc(ib,lay) |
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| 161 | enddo |
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| 162 | enddo |
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| 163 | |
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| 164 | ! Main layer loop |
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| 165 | do lay = 1, nlayers |
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| 166 | cwp = ciwp(lay) + clwp(lay) |
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| 167 | if (cldfrac(lay) .ge. cldmin .and. & |
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| 168 | (cwp .ge. cldmin .or. tauctot(lay) .ge. cldmin)) then |
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| 169 | |
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| 170 | ! Ice clouds and water clouds combined. |
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| 171 | if (inflag .eq. 0) then |
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| 172 | ncbands = 16 |
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| 173 | do ib = 1, ncbands |
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| 174 | taucloud(lay,ib) = tauc(ib,lay) |
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| 175 | end do |
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| 176 | |
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| 177 | elseif (inflag .eq. 1) then |
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| 178 | ncbands = 16 |
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| 179 | do ib = 1, ncbands |
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| 180 | taucloud(lay,ib) = abscld1 * cwp |
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| 181 | end do |
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| 182 | |
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| 183 | ! Separate treatement of ice clouds and water clouds. |
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| 184 | elseif (inflag .eq. 2) then |
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| 185 | radice = rei(lay) |
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| 186 | |
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| 187 | ! Calculation of absorption coefficients due to ice clouds. |
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| 188 | if (ciwp(lay) .eq. 0.0_rb) then |
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| 189 | abscoice(1) = 0.0_rb |
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| 190 | iceind = 0 |
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| 191 | |
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| 192 | elseif (iceflag .eq. 0) then |
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| 193 | if (radice .lt. 10.0_rb) stop 'ICE RADIUS TOO SMALL' |
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| 194 | abscoice(1) = absice0(1) + absice0(2)/radice |
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| 195 | iceind = 0 |
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| 196 | |
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| 197 | elseif (iceflag .eq. 1) then |
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| 198 | if (radice .lt. 13.0_rb .or. radice .gt. 130._rb) stop & |
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| 199 | 'ICE RADIUS OUT OF BOUNDS' |
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| 200 | ncbands = 5 |
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| 201 | do ib = 1, ncbands |
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| 202 | abscoice(ib) = absice1(1,ib) + absice1(2,ib)/radice |
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| 203 | enddo |
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| 204 | iceind = 1 |
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| 205 | |
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| 206 | ! For iceflag=2 option, ice particle effective radius is limited to 5.0 to 131.0 microns |
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| 207 | |
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| 208 | elseif (iceflag .eq. 2) then |
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| 209 | if (radice .lt. 5.0_rb .or. radice .gt. 131.0_rb) stop 'ICE RADIUS OUT OF BOUNDS' |
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| 210 | ncbands = 16 |
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| 211 | factor = (radice - 2._rb)/3._rb |
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| 212 | index = int(factor) |
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| 213 | if (index .eq. 43) index = 42 |
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| 214 | fint = factor - real(index) |
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| 215 | do ib = 1, ncbands |
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| 216 | abscoice(ib) = & |
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| 217 | absice2(index,ib) + fint * & |
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| 218 | (absice2(index+1,ib) - (absice2(index,ib))) |
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| 219 | enddo |
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| 220 | iceind = 2 |
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| 221 | |
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| 222 | ! For iceflag=3 option, ice particle generalized effective size is limited to 5.0 to 140.0 microns |
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| 223 | |
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| 224 | elseif (iceflag .eq. 3) then |
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| 225 | if (radice .lt. 5.0_rb .or. radice .gt. 140.0_rb) stop 'ICE GENERALIZED EFFECTIVE SIZE OUT OF BOUNDS' |
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| 226 | ncbands = 16 |
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| 227 | factor = (radice - 2._rb)/3._rb |
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| 228 | index = int(factor) |
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| 229 | if (index .eq. 46) index = 45 |
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| 230 | fint = factor - real(index) |
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| 231 | do ib = 1, ncbands |
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| 232 | abscoice(ib) = & |
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| 233 | absice3(index,ib) + fint * & |
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| 234 | (absice3(index+1,ib) - (absice3(index,ib))) |
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| 235 | enddo |
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| 236 | iceind = 2 |
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| 237 | |
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| 238 | endif |
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| 239 | |
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| 240 | ! Calculation of absorption coefficients due to water clouds. |
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| 241 | if (clwp(lay) .eq. 0.0_rb) then |
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| 242 | abscoliq(1) = 0.0_rb |
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| 243 | liqind = 0 |
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| 244 | if (iceind .eq. 1) iceind = 2 |
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| 245 | |
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| 246 | elseif (liqflag .eq. 0) then |
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| 247 | abscoliq(1) = absliq0 |
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| 248 | liqind = 0 |
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| 249 | if (iceind .eq. 1) iceind = 2 |
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| 250 | |
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| 251 | elseif (liqflag .eq. 1) then |
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| 252 | radliq = rel(lay) |
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| 253 | if (radliq .lt. 2.5_rb .or. radliq .gt. 60._rb) stop & |
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| 254 | 'LIQUID EFFECTIVE RADIUS OUT OF BOUNDS' |
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| 255 | index = int(radliq - 1.5_rb) |
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| 256 | if (index .eq. 0) index = 1 |
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| 257 | if (index .eq. 58) index = 57 |
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| 258 | fint = radliq - 1.5_rb - real(index) |
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| 259 | ncbands = 16 |
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| 260 | do ib = 1, ncbands |
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| 261 | abscoliq(ib) = & |
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| 262 | absliq1(index,ib) + fint * & |
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| 263 | (absliq1(index+1,ib) - (absliq1(index,ib))) |
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| 264 | enddo |
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| 265 | liqind = 2 |
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| 266 | endif |
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| 267 | |
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| 268 | do ib = 1, ncbands |
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| 269 | taucloud(lay,ib) = ciwp(lay) * abscoice(icb(ib,iceind)) + & |
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| 270 | clwp(lay) * abscoliq(icb(ib,liqind)) |
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| 271 | enddo |
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| 272 | endif |
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| 273 | endif |
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| 274 | enddo |
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| 275 | |
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| 276 | end subroutine cldprop |
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| 277 | |
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| 278 | end module rrtmg_lw_cldprop |
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