1 | MODULE YOERAD |
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2 | |
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3 | USE PARKIND1, ONLY : JPIM, JPRB |
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4 | USE YOE_SPECTRAL_PLANCK, ONLY : TSPECTRALPLANCK |
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5 | |
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6 | IMPLICIT NONE |
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7 | |
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8 | SAVE |
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9 | |
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10 | ! ------------------------------------------------------------------ |
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11 | !* ** *YOERAD* - CONTROL OPTIONS FOR RADIATION CONFIGURATION |
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12 | ! ------------------------------------------------------------------ |
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13 | |
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14 | ! Here we have hard-coded the options that configure the radiation |
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15 | ! scheme; in the IFS they are set in suecrad.F90 with the option to |
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16 | ! override them using the NAERAD namelist |
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17 | TYPE :: TERAD |
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18 | INTEGER(KIND=JPIM) :: NSW = 6 |
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19 | INTEGER(KIND=JPIM) :: NLWEMISS = 2 |
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20 | INTEGER(KIND=JPIM) :: NICEOPT = 3 |
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21 | INTEGER(KIND=JPIM) :: NLIQOPT = 4 |
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22 | INTEGER(KIND=JPIM) :: NRADIP = 3 |
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23 | INTEGER(KIND=JPIM) :: NRADLP = 2 |
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24 | INTEGER(KIND=JPIM) :: NLWOUT = 1 |
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25 | INTEGER(KIND=JPIM) :: NDECOLAT = 2 |
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26 | INTEGER(KIND=JPIM) :: NMINICE = 1 |
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27 | INTEGER(KIND=JPIM) :: NAERMACC = 1 |
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28 | INTEGER(KIND=JPIM) :: NMCVAR = 12 |
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29 | INTEGER(KIND=JPIM) :: NLWSCATTERING = 1 |
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30 | INTEGER(KIND=JPIM) :: NSWSOLVER = 3 ! Tripleclouds |
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31 | INTEGER(KIND=JPIM) :: NLWSOLVER = 3 ! Tripleclouds |
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32 | INTEGER(KIND=JPIM) :: NSOLARSPECTRUM = 0 |
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33 | INTEGER(KIND=JPIM) :: NDUMPBADINPUTS = 0 |
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34 | INTEGER(KIND=JPIM) :: NDUMPINPUTS = 0 |
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35 | INTEGER(KIND=JPIM) :: NCLOUDOVERLAP = 3 |
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36 | REAL(KIND=JPRB) :: RCLOUD_FRAC_STD = 1.0_JPRB |
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37 | REAL(KIND=JPRB) :: RCLOUD_SEPARATION_SCALE_TOA = 14000.0_JPRB |
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38 | REAL(KIND=JPRB) :: RCLOUD_SEPARATION_SCALE_SURF = 2500.0_JPRB |
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39 | LOGICAL :: LFU_LW_ICE_OPTICS_BUG = .FALSE. |
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40 | LOGICAL :: LDIAGFORCING = .FALSE. |
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41 | LOGICAL :: LAPPROXLWUPDATE = .TRUE. |
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42 | LOGICAL :: LAPPROXSWUPDATE = .FALSE. |
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43 | LOGICAL :: LCCNL = .TRUE. |
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44 | LOGICAL :: LCCNO = .TRUE. |
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45 | REAL(KIND=JPRB) :: RCCNLND = 900.0_JPRB |
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46 | REAL(KIND=JPRB) :: RCCNSEA = 50.0_JPRB |
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47 | REAL(KIND=JPRB) :: RRE2DE = 0.64952_JPRB |
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48 | REAL(KIND=JPRB) :: RMINICE = 60.0_JPRB |
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49 | |
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50 | ! Look-up table for Planck function in emissivity intervals |
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51 | TYPE(TSPECTRALPLANCK) :: YSPECTPLANCK |
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52 | |
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53 | END TYPE TERAD |
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54 | !============================================================================ |
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55 | |
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56 | TYPE(TERAD), POINTER :: YRERAD => NULL() |
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57 | |
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58 | |
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59 | ! * E.C.M.W.F. PHYSICS PACKAGE * |
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60 | |
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61 | ! J.-J. MORCRETTE E.C.M.W.F. 89/07/14 |
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62 | ! Modifications |
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63 | ! R J Hogan 20 May 2014: Added LApproxLwUpdate |
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64 | ! R J Hogan 19 June 2014: Added LApproxSwUpdate |
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65 | ! R J Hogan 19 Nov 2014: Added LCentredTimeSZA |
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66 | ! R J Hogan 15 Apr 2015: Added LMannersSwUpdate |
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67 | ! R J Hogan 24 Apr 2015: Added LAverageSZA |
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68 | ! R J Hogan 18 Sept 2015: Added LUsePre2017Rad (was LUsePre2015Rad) |
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69 | ! R J Hogan 1 Mar 2016: Added NLwSolver, NSwSolver, NLwScattering |
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70 | ! A Bozzo Feb 2017: Added logical to enable 3D aerosol climatology |
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71 | ! R J Hogan 9 Mar 2018: Added NDUMPBADINPUTS |
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72 | ! R J Hogan 22 Jan 2019: Added NLWEMISS, NCLOUDOVERLAP, NDUMPINPUTS |
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73 | ! R J Hogan 4 Feb 2019: Added NLWOUT |
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74 | ! R J Hogan 5 Feb 2019: Added YSPECTPLANCK |
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75 | ! R J Hogan 11 Mar 2019: Added CGHG*FILE, CSOLARIRRADIANCEFILE |
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76 | |
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77 | ! NAME TYPE PURPOSE |
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78 | ! ---- : ---- : --------------------------------------------------- |
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79 | ! LERAD1H: LOGICAL : .T. TO ALLOW MORE FREQUENT RADIATION CALCULATIONS |
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80 | ! : DURING FIRST N HOURS OF FORECAST |
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81 | ! NLNGR1H: INTEGER : NUMBER FORECAST HOURS DURING WHICH MORE FREQUENT |
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82 | ! RADIATION CALCULATIONS ARE REQUIRED |
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83 | ! LEPO3RA: LOGICAL : .T. IF PROGNOSTIC OZONE (EC) IS PASSED TO RADIATION |
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84 | ! NAER : INTEGER : CONFIGURATION INDEX FOR AEROSOLS |
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85 | ! NMODE : INTEGER : CONFIGURATION FOR RADIATION CODE: FLUX VS. RADIANCE |
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86 | ! NOZOCL : INTEGER : CHOICE OF OZONE CLIMATOLOGY (0 old, 1 new) |
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87 | ! NRADFR : INTEGER : FREQUENCY OF FULL RADIATION COMPUTATIONS |
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88 | ! IF(NRADFR.GT.0): RAD EVERY 'NRADFR' TIME-STEPS |
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89 | ! IF(NRADFR.LT.0): RAD EVERY '-NRADFR' HOURS |
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90 | ! NRADPFR: INTEGER : PRINT FREQUENCY FOR RAD.STATISTICS (in RAD.T.STEPS) |
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91 | ! NRADPLA: INTEGER : PRINT RAD.STATISTICS EVERY 'NRADPLA' ROWS |
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92 | ! NRADINT: INTEGER : RADIATION INTERPOLATION METHOD |
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93 | ! : 1 = SPECTRAL TRANSFORM INTERPOLATION |
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94 | ! : 2 = 4 POINT HORIZONTAL INTERPOLATION |
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95 | ! : 3 = 12 POINT HORIZONTAL INTERPOLATION |
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96 | ! NRADRES: INTEGER : RADIATION GRID SPECTRAL RESOLUTION |
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97 | ! NRADNFR: INTEGER : NORMAL FREQUENCY OF RADIATION STEPS |
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98 | ! NRADSFR: INTEGER : START-UP FREQUENCY OF RADIATION STEPS |
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99 | ! NRADE1H: INTEGER : START-UP FREQUENCY OF RADIATION STEPS FOR EPS |
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100 | ! NRADE3H: INTEGER : SUBSEQUENT FREQUENCY OF RADIATION STEPS FOR EPS |
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101 | ! NRADELG: INTEGER : LENGTH IN HOURS DURING WHICH THE FREQUENCY OF RADIATION IS INCREASED FOR EPS |
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102 | ! NOVLP : INTEGER : CLOUD OVERLAP CONFIGURATION IN PRE-MCRAD/ECRAD SCHEME |
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103 | ! : 1 = Max-rand (Geleyn & Hollingsworth) |
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104 | ! : 2 = Maximum |
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105 | ! : 3 = Random |
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106 | ! NRPROMA: INTEGER : VECTOR LENGTH FOR RADIATION CALCULATIONS |
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107 | ! NSW : INTEGER : NUMBER OF SHORTWAVE SPECTRAL INTERVALS |
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108 | ! NSWNL : INTEGER : NUMBER OF SHORTWAVE SPECTRAL INTERVALS IN NL MODEL |
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109 | ! NSWTL : INTEGER : NUMBER OF SHORTWAVE SPECTRAL INTERVALS IN TL MODEL |
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110 | ! NTSW : INTEGER : MAXIMUM POSSIBLE NUMBER OF SW SPECTRAL INTERVALS |
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111 | ! NUV : INTEGER : NUMBER OF UV SPECTRAL INTERVALS FOR THE UV PROCESSOR |
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112 | ! LOPTRPROMA:LOGICAL: .T. NRPROMA will be optimised |
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113 | ! : .F. NRPROMA will not be optimised (forced |
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114 | ! : by negative NRPROMA in namelist) |
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115 | |
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116 | ! NRADIP : INTEGER : INDEX FOR DIAGNOSIS OF ICE CLOUD EFFECTIVE RADIUS |
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117 | ! 0 = fixed at 40 microns |
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118 | ! 1 = Liou & Ou (1994) capped between 40-130 microns |
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119 | ! 2 = Liou & Ou but capped between 30 and 60 microns |
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120 | ! 3 = Sun & Rikus (1999) revised by Sun (2001) |
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121 | ! NRADLP : INTEGER : INDEX FOR DIAGNOSIS OF LIQ. CLOUD EFFECTIVE RADIUS |
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122 | ! 0 = ERA-15 function of pressure |
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123 | ! 1 = 10 microns over land, 13 microns over sea |
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124 | ! 2 = Martin_et_al (1994) in terms of land-sea number conc |
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125 | ! 3 = Linked to prognostic aerosols |
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126 | ! NICEOPT: INTEGER : INDEX FOR ICE CLOUD OPTICAL PROPERTIES |
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127 | ! 0 = SW Ebert-Curry, LW Smith & Shi (1992) |
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128 | ! 1 = SW Ebert-Curry, LW Ebert-Curry (1992) |
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129 | ! 2 = SW & LW Fu-Liou (1993) |
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130 | ! 3 = SW Fu (1996) LW Fu et al. (1998) + Chou et al. (1999) LW scatt approx |
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131 | ! the following only available in newer modular radiation scheme: |
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132 | ! 4 = SW/LW Baran data fitted versus ice mixing ratio |
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133 | ! NLIQOPT: INTEGER : INDEX FOR LIQUID WATER CLOUD OPTICAL PROPERTIES |
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134 | ! 0 = SW Fouquart (1991) LW Smith-Shi (1992) YF/SmSh |
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135 | ! 1 = SW Slingo (1989) LW Savijarvi (1997) |
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136 | ! 2 = SW Slingo (1989) LW Lindner-Li (2000) |
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137 | ! the following only available in RADLSW, not RADLSWR: |
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138 | ! 3 = SW Nielsen LW Smith-Shi |
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139 | ! the following only available in newer modular radiation scheme: |
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140 | ! 4 = SW/LW SOCRATES scheme |
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141 | ! |
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142 | ! LONEWSW: LOGICAL : .T. IF NEW SW CODE IS ACTIVE |
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143 | ! LECSRAD: LOGICAL : .T. IF CLEAR-SKY RADIATION IS ARCHIVED AS PEXTR2 |
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144 | ! NCSRADF: INTEGER : 1 IF ACCUMULATED, 2 IF INSTANTANEOUS |
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145 | ! LRRTM : LOGICAL : .T. IF RRTM140MR IS USED FOR LW RADIATION TRANSFER |
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146 | |
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147 | ! LHVOLCA: LOGICAL : .T. IF USING HISTORICAL VOLCANIC AEROSOLS |
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148 | ! LNEWAER: LOGICAL : .T. IF AEROSOL MONTHLY DISTRIBUTIONS ARE USED |
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149 | ! LNOTROAER:LOGICAL: .T. IF NO TROPOSPHERIC AEROSOLS |
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150 | ! CRTABLEDIR: CHAR : IF NRADINT > 0 SPECIFIES DIRECTORY PATH FOR RADIATION |
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151 | ! : GRID RTABLE NAMELIST |
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152 | ! CRTABLEFIL: CHAR : IF NRADINT > 0 SPECIFIES FILE NAME OF RADIATION |
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153 | ! : GRID RTABLE NAMELIST |
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154 | ! LRAYL : LOGICAL : .T. NEW RAYLEIGH FOR SW-6 VERSION |
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155 | |
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156 | ! RAOVLP : REAL : COEFFICIENTS FOR ALPHA1 FACTOR IN HOGAN & |
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157 | ! RBOVLP : REAL : ILLINGWORTH's PARAMETRIZATION |
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158 | |
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159 | ! LCCNL : LOGICAL : .T. IF CCN CONCENTRATION OVER LAND IS DIAGNOSED |
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160 | ! LCCNO : LOGICAL : .T. IF CCN CONCENTRATION OVER OCEAN IS DIAGNOSED |
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161 | ! RCCNLND: REAL : NUMBER CONCENTRATION (CM-3) OF CCNs OVER LAND |
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162 | ! RCCNSEA: REAL : NUMBER CONCENTRATION (CM-3) OF CCNs OVER SEA |
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163 | |
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164 | ! LDIFFC : LOGICAL : .T. IF SAVIJARVI'S DIFFUSIVITY CORRECTION IS ON |
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165 | |
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166 | ! NINHOM : INTEGER : 0 IF NO INHOMOGENEITY SCALING EFFECT |
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167 | ! 1 IF SIMPLE 0.7 SCALING |
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168 | ! 2 IF BARKER, 3 IF CAIRNS ET AL. |
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169 | ! RLWINHF: REAL : INHOMOG. SCALING FACTOR FOR CLOUD LW OPTICAL THICKNESS |
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170 | ! RSWINHF: REAL : INHOMOG. SCALING FACTOR FOR CLOUD SW OPTICAL THICKNESS |
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171 | |
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172 | ! NPERTAER : INTERGER : PERCENTAGE OF PERTURBATION FOR AEROSOL |
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173 | ! NPERTOZONE : INTEGER : PERCENTAGE OF PERTURBATION FOR OZONE |
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174 | ! NHINCSOL : INTEGER : 0: Total Solar Irradiance (TSI) fixed at 1366.0 W m-2 |
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175 | ! 1: Deprecated - use default |
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176 | ! 2: Deprecated - use default |
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177 | ! 3: Deprecated (was CMIP5) - use default |
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178 | ! 4: TSI from CMIP6 NetCDF (default), or override with CSOLARIRRADIANCEFILE |
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179 | ! NSWWVCONTINUUM : INTEGER : 0 MT_CKD2.5 (SRTM default WV continuum) |
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180 | ! 1 CAVIAR continuum (Shine et al. 2016) |
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181 | ! LECO2VAR: LOGICAL: .T. IF ERA-40/AMIP2 VARIABILITY OF GHG IS ON (ignored) |
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182 | ! LHGHG : LOGICAL : .T. IF VARIABILITY OF GREENHOUSE GASES (INCLUDING CO2) IS ON |
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183 | ! N.B.: LHGHG supersedes LECO2VAR and allows using better specification of trace gases |
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184 | ! NSCEN : INTEGER : 21st CENTURY SCENARIO FOR GHG (1=A1B, 2=A2, 3=B1) |
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185 | ! RRe2De : REAL : CONVERSION FACTOR BETWWEN EFFECTIVE RADIUS AND PARTICLE SIZE |
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186 | ! RMINICE: REAL : MINIMUM SIZE FOR ICE PARTICLES (um) |
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187 | ! FOR ICE |
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188 | ! NMINICE: INTEGER : 1-6 MINIMUM ICE PARTICLE SIZE DEPENDS ON LATITUDE, 0=INDEPENDENT OF LATITUDE |
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189 | ! NDECOLAT:INTEGER : DECORRELATION LENGTH FOR CF AND CW |
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190 | ! 0: SPECIFIED INDEPENDENT OF LATITUDE, 1: SHONK-HOGAN, 2: IMPROVED |
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191 | ! NMCICA : INTEGER : 0: NO McICA |
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192 | ! 1: McICA w maximum-random in cloud generator |
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193 | ! 2: McICA w generalized overlap in cloud generator |
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194 | ! LESO4HIS: LOGICAL:.T.: Use historical/projected SO4 data per decade and month |
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195 | ! NGHGRAD: INTEGER : configuration of 3D GHG climatologies accounted for in radiation |
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196 | ! 0: global values |
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197 | ! 1: CO2 2: CH4 3: N2O 4: NO2 5:CFC11 6:CFC12 |
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198 | ! 12: CO2+CH4 13: CO2+CH4+N2O |
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199 | ! 16: CO2+CH4+N2O+CFC11+CFC12 |
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200 | ! LETRACGMS: LOGICAL : F=Cariolle climatol. T=GEMS-derived clim for CO2, CH4, O3 |
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201 | ! LAERCLIM : LOGICAL : .T. for output of the climatological aerosol optical depth at 550 nm |
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202 | ! LAERVISI : LOGICAL : .T. for output of the visibility (from diagnsotic or prognostic aerosols) |
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203 | ! NVOLCVERT: INTEGER : Vertical distribution of volcanic aerosol |
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204 | ! 0: original profile, diagnosed from T |
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205 | ! 1: original profile, but upper boundary at 10hPa |
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206 | ! 2: lower boundary diagnosed from ozone, upper boundary at 10hPa |
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207 | ! LVOLCSPEC: LOGICAL : T for specified volcanic aerosol |
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208 | ! LVOLCDAMP: LOGICAL : T for damping of specified volcanic aerosol from initial value |
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209 | ! RVOLCSPEC: REAL : Specified volcanic aerosol (total optical depth) in NH/Tropics/SH |
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210 | ! RNs : derived from Avogadro |
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211 | ! RSIGAIR: invariant terms in expression of Rayleigh scattering cross-section |
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212 | ! NREDGSW : INTEGER : 0 full resolution for RRTM_SW (224) |
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213 | ! 1 ECMWF High resolution model configuration (_SW: 112) |
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214 | ! 2 ECMWF EPS configuration (_SW: 56) |
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215 | ! NREDGLW : INTEGER : 0 full resolution for RRTM_LW (256) |
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216 | ! 1 ECMWF High resolution model configuration (_LW: 140) |
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217 | ! 2 ECMWF EPS configuration (_LW: 70) |
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218 | ! LDIAGFORCING : LOGICAL : T Write input ozone, ghg and aerosol forcing to 3D fields |
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219 | ! To be used for diagnostics only; do not use in production runs |
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220 | ! NAERMACC : INTEGER : MACC-derived aerosol climatology on a NMCLAT x NMCLON grid |
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221 | ! RAESHxx : REAL : parameters related to scale height of MACC-derived aerosol climatology |
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222 | ! CVDAExx : REAL : scale heights of MACC-derived aerosol climatology |
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223 | ! LAERADJDU: LOGICAL : T adjust MACC-derived DU climatology |
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224 | ! LAERADCLI: LOGICAL : T if radiation uses the MACC-derived aerosol climatology |
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225 | ! LApproxLwUpdate : LOGICAL : Update the longwave upwelling flux every |
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226 | ! timestep/gridpoint using the stored rate |
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227 | ! of change of the fluxes with respect to |
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228 | ! the surface upwelling longwave flux |
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229 | ! LApproxSwUpdate : LOGICAL : Update the shortwave upwelling flux |
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230 | ! every gridpoint to account for the local |
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231 | ! value of surface albedo |
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232 | ! LMannersSwUpdate: LOGICAL : Update the shortwave flux every timestep |
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233 | ! using Manners et al. (2009) correction |
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234 | ! for solar zenith angle change |
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235 | ! LCentredTimeSZA : LOGICAL : Compute solar zenith angle in radiation |
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236 | ! scheme half way between calls to |
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237 | ! radiation scheme (rather than previous |
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238 | ! behaviour, which is half way between |
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239 | ! calls plus half a model timestep) |
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240 | ! LAverageSZA : LOGICAL : Compute an averaged solar zenith angle |
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241 | ! across the time interval required |
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242 | ! (either a model timestep or a radiation |
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243 | ! timestep). Should be used with |
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244 | ! LCentredTimeSZA=TRUE. |
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245 | ! LUsePre2017Rad : LOGICAL : Use the pre-2017 radiation scheme, rather |
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246 | ! than the modular scheme contained in the |
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247 | ! separate "radiation" library. Note that |
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248 | ! the radiation library may make use of the |
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249 | ! pre-2017 RRTM-G gas optics. |
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250 | ! RCloud_Frac_Std : REAL : Cloud water content horizontal fractional |
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251 | ! standard deviation in a gridbox |
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252 | ! LInterpInCloudMean : LOGICAL : When interpolating model fields to |
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253 | ! radiation grid, interpolate in-cloud |
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254 | ! mean water contents? Better |
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255 | ! conservation achieved by interpolating |
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256 | ! gridbox-means. |
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257 | ! CGHGCLIMFILE : STRING : Location of greenhouse gas climatology file, |
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258 | ! or empty if the default is to be used. If it |
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259 | ! starts with "." or "/" then a relative path |
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260 | ! is assumed, otherwise the default directory. |
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261 | ! CGHGTIMESERIESFILE:STRING : Location of greenhouse gas timeseries |
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262 | ! file, or empty if it is to be worked out |
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263 | ! from the NSCEN, YOECMIP%NGHGCMIP and |
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264 | ! YOECMIP%NRCP variables. If it starts |
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265 | ! with "." or "/" then a relative path is |
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266 | ! assumed, otherwise the default |
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267 | ! directory. |
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268 | ! CSOLARIRRADIANCEFILE:STRING:Location of Total Solar Irradiance file, |
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269 | ! or empty if the default is to be |
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270 | ! used. If it starts with "." or "/" then |
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271 | ! a relative path is assumed, otherwise |
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272 | ! the default directory. |
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273 | ! NLWEMISS : INTEGER : Number of emissivity spectral intervals, set |
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274 | ! according to the value of NEMISSSCHEME; traditionally |
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275 | ! this has always been 2: outside the IR window and within |
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276 | ! NLWOUT : INTEGER : Number of spectral intervals to pass LW downwelling flux |
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277 | ! to RADHEATN; traditionally this was 1, but this led |
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278 | ! to errors with LAPPROXLWUPDATE=TRUE, which updated |
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279 | ! fluxes using a single broadband emissivity. Now we can |
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280 | ! do approximate updates using full spectral emissivity. |
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281 | ! ------------------------------------------------------------------ |
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282 | ! THE FOLLOWING ARE ONLY USED FOR THE ECRAD SCHEME (LUsePre2017Rad = .FALSE.) |
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283 | ! NLwScattering : INTEGER : 0: No longwave scattering |
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284 | ! 1: Longwave scattering by clouds only |
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285 | ! 2: Longwave scattering by clouds and aerosols |
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286 | ! NSwSolver : INTEGER : |
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287 | ! NLwSolver : INTEGER : 0: McICA |
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288 | ! 1: SPARTACUS 1D |
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289 | ! 2: SPARTACUS 3D |
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290 | ! 3: TripleClouds |
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291 | ! LFU_LW_ICE_OPTICS_BUG : LOGICAL : Continue to use bug in Fu LW ice |
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292 | ! optics whereby single scattering albedo is |
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293 | ! one minus what it should be |
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294 | ! NSOLARSPECTRUM : INTEGER : 0: Kurucz |
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295 | ! 1: Coddington et al. (BAMS 2016) |
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296 | ! NDUMPBADINPUTS : INTEGER : 0: Warn only if fluxes out of physical bounds |
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297 | ! n: Write netcdf file of bad inputs up to n times per task |
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298 | ! -n: Abort if fluxes ever out of physical bounds |
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299 | ! NDUMPINPUTS : INTEGER : 0: Do nothing |
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300 | ! n: Write netcdf file of all inputs up to n times per task |
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301 | ! NCLOUDOVERLAP : INTEGER : Cloud overlap scheme |
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302 | ! 1: Maximum-random |
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303 | ! 2: Exponential-exponential (the actual behaviour of McRad) |
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304 | ! 3: Exponential-random (only option for Tripleclouds and SPARTACUS) |
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305 | ! RCLOUD_SEPARATION_SCALE_TOA, RCLOUD_SEPARATION_SCALE_SURF : REAL |
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306 | ! Cloud horizontal length scale, in metres, used to |
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307 | ! compute rate of horizontal exchange of radiation |
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308 | ! between clouds and clear skies in SPARTACUS solver |
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309 | ! ------------------------------------------------------------------ |
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310 | ! KMODTS : INTEGER : (A Bozzo) switch for different radiative transfer schemes for UV |
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311 | ! = 0 Fouquart&Bonnel adapted by Morcrette and Arola |
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312 | ! = 1 eddington (joseph et al., 1976) |
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313 | ! = 2 pifm (zdunkowski et al., 1980) |
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314 | ! = 3 discrete ordinates (liou, 1973) |
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315 | ! ------------------------------------------------------------------ |
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316 | ! TRBKG : REAL tropospheric background OD@550nm for aerosol climatology. |
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317 | ! default for Tegen climatology was 0.03 |
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318 | ! STBKG : REAL stratospheric background OD@550nm for aerosol climatology. |
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319 | ! ------------------------------------------------------------------ |
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320 | ! LDUSEASON : LOGICAL enables a monthly-varying scale height for the |
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321 | ! dust aerosol climatology |
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322 | ! LAER3D : LOGICAL : to enable aerosol climatology in 3D |
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323 | |
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324 | |
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325 | END MODULE YOERAD |
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