1 | c $Header$ |
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2 | SUBROUTINE CONVECT3 |
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3 | * (DTIME,EPMAX,ok_adj, |
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4 | * T1, R1, RS, U, V, TRA, P, PH, |
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5 | * ND, NDP1, NL, NTRA, DELT, IFLAG, |
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6 | * FT, FR, FU, FV, FTRA, PRECIP, |
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7 | * icb,inb, upwd,dnwd,dnwd0,SIG, W0,Mike,Mke, |
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8 | * Ma,MENTS,QENTS,TPS,TLS,SIGIJ,CAPE,TVP,PBASE,BUOYBASE, |
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9 | cccc * DTVPDT1,DTVPDQ1,DPLCLDT,DPLCLDR) |
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10 | * DTVPDT1,DTVPDQ1,DPLCLDT,DPLCLDR, ! sbl |
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11 | * FT2,FR2,FU2,FV2,WD,QCOND,QCONDC) ! sbl |
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12 | C |
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13 | C *** THE PARAMETER NA SHOULD IN GENERAL EQUAL ND *** |
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14 | C |
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15 | c################################################################# |
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16 | cFleur Introduction des traceurs dans convect3 le 6 juin 200 |
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17 | c################################################################# |
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18 | #include "dimensions.h" |
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19 | #include "dimphy.h" |
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20 | PARAMETER (NA=60) |
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21 | |
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22 | integer NTRAC |
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23 | PARAMETER (NTRAC=nqmx-2) |
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24 | REAL DELTAC ! cld |
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25 | PARAMETER (DELTAC=0.01) ! cld |
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26 | |
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27 | INTEGER NENT(NA) |
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28 | REAL T1(ND),R1(ND),RS(ND),U(ND),V(ND),TRA(ND,NTRA) |
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29 | REAL P(ND),PH(NDP1) |
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30 | REAL FT(ND),FR(ND),FU(ND),FV(ND),FTRA(ND,NTRA) |
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31 | REAL SIG(ND),W0(ND) |
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32 | REAL UENT(NA,NA),VENT(NA,NA),TRAENT(NA,NA,NTRAC),TRATM(NA) |
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33 | REAL UP(NA),VP(NA),TRAP(NA,NTRAC) |
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34 | REAL M(NA),MP(NA),MENT(NA,NA),QENT(NA,NA),ELIJ(NA,NA) |
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35 | REAL SIJ(NA,NA),TVP(NA),TV(NA),WATER(NA) |
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36 | REAL RP(NA),EP(NA),TH(NA),WT(NA),EVAP(NA),CLW(NA) |
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37 | REAL SIGP(NA),B(NA),TP(NA),CPN(NA) |
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38 | REAL LV(NA),LVCP(NA),H(NA),HP(NA),GZ(NA) |
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39 | REAL T(NA),RR(NA) |
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40 | C |
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41 | REAL FT2(ND),FR2(ND),FU2(ND),FV2(ND) ! added sbl |
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42 | REAL U1(ND),V1(ND) ! added sbl |
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43 | C |
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44 | REAL BUOY(NA) ! Lifted parcel buoyancy |
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45 | REAL DTVPDT1(ND),DTVPDQ1(ND) ! Derivatives of parcel virtual |
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46 | C temperature wrt T1 and Q1 |
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47 | REAL CLW_NEW(NA),QI(NA) |
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48 | C |
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49 | REAL WD, BETAD ! for gust factor (sb) |
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50 | REAL QCONDC(ND) ! interface cld param (sb) |
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51 | REAL QCOND(ND),NQCOND(NA),WA(NA),MAA(NA),SIGA(NA),AXC(NA) ! cld |
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52 | C |
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53 | LOGICAL ICE_CONV,ok_adj |
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54 | PARAMETER (ICE_CONV=.TRUE.) |
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55 | |
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56 | cccccccccccccccccccccccccccccccccccccccccccccc |
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57 | c declaration des variables a sortir |
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58 | ccccccccccccccccccccccccccccccccccccccccccccc |
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59 | real Mke(nd) |
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60 | real Mike(nd) |
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61 | real Ma(nd) |
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62 | real TPS(ND) !temperature dans les ascendances non diluees |
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63 | real TLS(ND) !temperature potentielle |
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64 | real MENTS(nd,nd) |
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65 | real QENTS(nd,nd) |
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66 | REAL SIGIJ(KLEV,KLEV) |
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67 | REAL PBASE ! pressure at the cloud base level |
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68 | REAL BUOYBASE ! buoyancy at the cloud base level |
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69 | cccccccccccccccccccccccccccccccccccccccccccccc |
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70 | |
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71 | |
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72 | |
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73 | c |
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74 | real dnwd0(nd) ! precipitation driven unsaturated downdraft flux |
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75 | real dnwd(nd), dn1 ! in-cloud saturated downdraft mass flux |
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76 | real upwd(nd), up1 ! in-cloud saturated updraft mass flux |
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77 | C |
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78 | C *** ASSIGN VALUES OF THERMODYNAMIC CONSTANTS *** |
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79 | C *** THESE SHOULD BE CONSISTENT WITH *** |
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80 | C *** THOSE USED IN CALLING PROGRAM *** |
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81 | C *** NOTE: THESE ARE ALSO SPECIFIED IN SUBROUTINE TLIFT *** |
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82 | C |
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83 | c sb CPD=1005.7 |
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84 | c sb CPV=1870.0 |
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85 | c sb CL=4190.0 |
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86 | c sb CPVMCL=CL-CPV |
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87 | c sb RV=461.5 |
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88 | c sb RD=287.04 |
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89 | c sb EPS=RD/RV |
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90 | c sb ALV0=2.501E6 |
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91 | ccccccccccccccccccccccc |
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92 | c constantes coherentes avec le modele du Centre Europeen |
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93 | c sb RD = 1000.0 * 1.380658E-23 * 6.0221367E+23 / 28.9644 |
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94 | c sb RV = 1000.0 * 1.380658E-23 * 6.0221367E+23 / 18.0153 |
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95 | c sb CPD = 3.5 * RD |
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96 | c sb CPV = 4.0 * RV |
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97 | c sb CL = 4218.0 |
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98 | c sb CPVMCL=CL-CPV |
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99 | c sb EPS=RD/RV |
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100 | c sb ALV0=2.5008E+06 |
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101 | cccccccccccccccccccccc |
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102 | c on utilise les constantes thermo du Centre Europeen: (SB) |
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103 | c |
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104 | #include "YOMCST.h" |
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105 | c |
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106 | CPD = RCPD |
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107 | CPV = RCPV |
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108 | CL = RCW |
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109 | CPVMCL = CL-CPV |
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110 | EPS = RD/RV |
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111 | ALV0 = RLVTT |
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112 | c |
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113 | NK = 1 ! origin level of the lifted parcel |
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114 | c |
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115 | cccccccccccccccccccccc |
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116 | C |
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117 | C *** INITIALIZE OUTPUT ARRAYS AND PARAMETERS *** |
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118 | C |
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119 | DO 5 I=1,ND |
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120 | FT(I)=0.0 |
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121 | FR(I)=0.0 |
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122 | FU(I)=0.0 |
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123 | FV(I)=0.0 |
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124 | |
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125 | FT2(I)=0.0 |
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126 | FR2(I)=0.0 |
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127 | FU2(I)=0.0 |
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128 | FV2(I)=0.0 |
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129 | |
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130 | DO 4 J=1,NTRA |
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131 | FTRA(I,J)=0.0 |
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132 | 4 CONTINUE |
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133 | |
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134 | QCONDC(I)=0.0 ! cld |
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135 | QCOND(I)=0.0 ! cld |
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136 | NQCOND(I)=0.0 ! cld |
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137 | |
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138 | T(I)=T1(I) |
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139 | RR(I)=R1(I) |
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140 | U1(I)=U(I) ! added sbl |
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141 | V1(I)=V(I) ! added sbl |
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142 | 5 CONTINUE |
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143 | DO 7 I=1,NL |
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144 | RDCP=(RD*(1.-RR(I))+RR(I)*RV)/ (CPD*(1.-RR(I))+RR(I)*CPV) |
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145 | TH(I)=T(I)*(1000.0/P(I))**RDCP |
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146 | 7 CONTINUE |
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147 | C |
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148 | ************************************************************* |
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149 | ** CALCUL DES TEMPERATURES POTENTIELLES A SORTIR |
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150 | ************************************************************* |
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151 | do i=1,ND |
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152 | RDCP=(RD*(1.-RR(I))+RR(I)*RV)/ (CPD*(1.-RR(I))+RR(I)*CPV) |
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153 | |
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154 | TLS(i)=T(I)*(1000.0/P(I))**RDCP |
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155 | enddo |
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156 | |
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157 | |
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158 | |
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159 | |
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160 | ************************************************************ |
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161 | |
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162 | |
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163 | PRECIP=0.0 |
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164 | WD=0.0 ! sb |
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165 | IFLAG=1 |
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166 | C |
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167 | C *** SPECIFY PARAMETERS *** |
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168 | C *** PBCRIT IS THE CRITICAL CLOUD DEPTH (MB) BENEATH WHICH THE *** |
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169 | C *** PRECIPITATION EFFICIENCY IS ASSUMED TO BE ZERO *** |
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170 | C *** PTCRIT IS THE CLOUD DEPTH (MB) ABOVE WHICH THE PRECIP. *** |
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171 | C *** EFFICIENCY IS ASSUMED TO BE UNITY *** |
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172 | C *** SIGD IS THE FRACTIONAL AREA COVERED BY UNSATURATED DNDRAFT *** |
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173 | C *** SPFAC IS THE FRACTION OF PRECIPITATION FALLING OUTSIDE *** |
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174 | C *** OF CLOUD *** |
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175 | C *** ALPHA AND BETA ARE PARAMETERS THAT CONTROL THE RATE OF *** |
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176 | C *** APPROACH TO QUASI-EQUILIBRIUM *** |
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177 | C *** (THEIR STANDARD VALUES ARE 1.0 AND 0.96, RESPECTIVELY) *** |
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178 | C *** (BETA MUST BE LESS THAN OR EQUAL TO 1) *** |
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179 | C *** DTCRIT IS THE CRITICAL BUOYANCY (K) USED TO ADJUST THE *** |
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180 | C *** APPROACH TO QUASI-EQUILIBRIUM *** |
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181 | C *** IT MUST BE LESS THAN 0 *** |
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182 | C |
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183 | PBCRIT=150.0 |
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184 | PTCRIT=500.0 |
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185 | SIGD=0.01 |
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186 | SPFAC=0.15 |
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187 | c sb: |
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188 | c EPMAX=0.993 ! precip efficiency less than unity |
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189 | c EPMAX=1. ! precip efficiency less than unity |
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190 | C |
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191 | Cjyg |
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192 | CCC BETA=0.96 |
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193 | C Beta is now expressed as a function of the characteristic time |
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194 | C of the convective process. |
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195 | CCC Old value : TAU = 15000. !(for dtime = 600.s) |
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196 | CCC Other value (inducing little change) :TAU = 8000. |
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197 | TAU = 8000. |
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198 | BETA = 1.-DTIME/TAU |
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199 | Cjyg |
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200 | CCC ALPHA=1.0 |
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201 | ALPHA=1.5E-3*DTIME/TAU |
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202 | C Increase alpha in order to compensate W decrease |
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203 | ALPHA = ALPHA*1.5 |
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204 | C |
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205 | Cjyg (voir CONVECT 3) |
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206 | CCC DTCRIT=-0.2 |
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207 | DTCRIT=-2. |
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208 | Cgf&jyg |
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209 | CCC DT pour l'overshoot. |
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210 | DTOVSH = -0.2 |
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211 | |
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212 | C |
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213 | C *** INCREMENT THE COUNTER *** |
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214 | C |
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215 | SIG(ND)=SIG(ND)+1.0 |
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216 | SIG(ND)=AMIN1(SIG(ND),12.1) |
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217 | C |
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218 | C *** IF NOPT IS AN INTEGER OTHER THAN 0, CONVECT *** |
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219 | C *** RETURNS ARRAYS T AND R THAT MAY HAVE BEEN *** |
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220 | C *** ALTERED BY DRY ADIABATIC ADJUSTMENT; OTHERWISE *** |
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221 | C *** THE RETURNED ARRAYS ARE UNALTERED. *** |
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222 | C |
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223 | NOPT=0 |
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224 | c! NOPT=1 ! sbl |
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225 | C |
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226 | C *** PERFORM DRY ADIABATIC ADJUSTMENT *** |
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227 | C |
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228 | C *** DO NOT BYPASS THIS EVEN IF THE CALLING PROGRAM HAS A *** |
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229 | C *** BOUNDARY LAYER SCHEME !!! *** |
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230 | C |
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231 | IF (ok_adj) THEN ! added sbl |
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232 | |
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233 | DO 30 I=NL-1,1,-1 |
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234 | JN=0 |
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235 | DO 10 J=I+1,NL |
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236 | 10 IF(TH(J).LT.TH(I))JN=J |
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237 | IF(JN.EQ.0)GOTO 30 |
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238 | AHM=0.0 |
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239 | RM=0.0 |
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240 | UM=0.0 |
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241 | VM=0.0 |
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242 | DO K=1,NTRA |
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243 | TRATM(K)=0.0 |
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244 | END DO |
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245 | DO 15 J=I,JN |
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246 | AHM=AHM+(CPD*(1.-RR(J))+RR(J)*CPV)*T(J)*(PH(J)-PH(J+1)) |
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247 | RM=RM+RR(J)*(PH(J)-PH(J+1)) |
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248 | UM=UM+U(J)*(PH(J)-PH(J+1)) |
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249 | VM=VM+V(J)*(PH(J)-PH(J+1)) |
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250 | DO K=1,NTRA |
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251 | TRATM(K)=TRATM(K)+TRA(J,K)*(PH(J)-PH(J+1)) |
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252 | END DO |
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253 | 15 CONTINUE |
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254 | DPHINV=1./(PH(I)-PH(JN+1)) |
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255 | RM=RM*DPHINV |
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256 | UM=UM*DPHINV |
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257 | VM=VM*DPHINV |
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258 | DO K=1,NTRA |
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259 | TRATM(K)=TRATM(K)*DPHINV |
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260 | END DO |
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261 | A2=0.0 |
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262 | DO 20 J=I,JN |
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263 | RR(J)=RM |
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264 | U(J)=UM |
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265 | V(J)=VM |
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266 | DO K=1,NTRA |
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267 | TRA(J,K)=TRATM(K) |
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268 | END DO |
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269 | RDCP=(RD*(1.-RR(J))+RR(J)*RV)/ (CPD*(1.-RR(J))+RR(J)*CPV) |
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270 | X=(0.001*P(J))**RDCP |
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271 | T(J)=X |
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272 | A2=A2+(CPD*(1.-RR(J))+RR(J)*CPV)*X*(PH(J)-PH(J+1)) |
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273 | 20 CONTINUE |
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274 | DO 25 J=I,JN |
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275 | TH(J)=AHM/A2 |
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276 | T(J)=T(J)*TH(J) |
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277 | 25 CONTINUE |
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278 | 30 CONTINUE |
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279 | |
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280 | ENDIF ! added sbl |
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281 | C |
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282 | C *** RESET INPUT ARRAYS IF ok_adj 0 *** |
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283 | C |
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284 | IF (ok_adj)THEN |
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285 | DO 35 I=1,ND |
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286 | |
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287 | FT2(I)=(T(I)-T1(I))/DELT ! sbl |
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288 | FR2(I)=(RR(I)-R1(I))/DELT ! sbl |
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289 | FU2(I)=(U(I)-U1(I))/DELT ! sbl |
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290 | FV2(I)=(V(I)-V1(I))/DELT ! sbl |
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291 | |
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292 | c! T1(I)=T(I) ! commente sbl |
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293 | c! R1(I)=RR(I) ! commente sbl |
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294 | 35 CONTINUE |
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295 | END IF |
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296 | C |
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297 | C *** CALCULATE ARRAYS OF GEOPOTENTIAL, HEAT CAPACITY AND STATIC ENERGY |
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298 | C |
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299 | GZ(1)=0.0 |
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300 | CPN(1)=CPD*(1.-RR(1))+RR(1)*CPV |
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301 | H(1)=T(1)*CPN(1) |
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302 | DO 40 I=2,NL |
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303 | TVX=T(I)*(1.+RR(I)/EPS-RR(I)) |
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304 | TVY=T(I-1)*(1.+RR(I-1)/EPS-RR(I-1)) |
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305 | GZ(I)=GZ(I-1)+0.5*RD*(TVX+TVY)*(P(I-1)-P(I))/PH(I) |
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306 | CPN(I)=CPD*(1.-RR(I))+CPV*RR(I) |
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307 | H(I)=T(I)*CPN(I)+GZ(I) |
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308 | 40 CONTINUE |
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309 | C |
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310 | C *** CALCULATE LIFTED CONDENSATION LEVEL OF AIR AT LOWEST MODEL LEVEL *** |
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311 | C *** (WITHIN 0.2% OF FORMULA OF BOLTON, MON. WEA. REV.,1980) *** |
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312 | C |
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313 | IF (T(1).LT.250.0.OR.RR(1).LE.0.0)THEN |
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314 | IFLAG=0 |
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315 | c sb3d print*,'je suis passe par 366' |
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316 | RETURN |
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317 | END IF |
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318 | |
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319 | cjyg1 Utilisation de la subroutine CLIFT |
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320 | CC RH=RR(1)/RS(1) |
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321 | CC CHI=T(1)/(1669.0-122.0*RH-T(1)) |
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322 | CC PLCL=P(1)*(RH**CHI) |
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323 | CALL CLIFT(P(1),T(1),RR(1),RS(1),PLCL,DPLCLDT,DPLCLDR) |
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324 | cjyg2 |
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325 | c sb3d PRINT *,' em_plcl,p1,t1,r1,rs1,rh ' |
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326 | c sb3d $ ,PLCL,P(1),T(1),RR(1),RS(1),RH |
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327 | c |
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328 | IF (PLCL.LT.200.0.OR.PLCL.GE.2000.0)THEN |
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329 | IFLAG=2 |
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330 | RETURN |
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331 | END IF |
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332 | Cjyg1 |
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333 | C Essais de modification de ICB |
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334 | C |
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335 | C *** CALCULATE FIRST LEVEL ABOVE LCL (=ICB) *** |
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336 | C |
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337 | CC ICB=NL-1 |
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338 | CC DO 50 I=2,NL-1 |
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339 | CC IF(P(I).LT.PLCL)THEN |
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340 | CC ICB=MIN(ICB,I) ! ICB sup ou egal a 2 |
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341 | CC END IF |
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342 | CC 50 CONTINUE |
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343 | CC IF(ICB.EQ.(NL-1))THEN |
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344 | CC IFLAG=3 |
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345 | CC RETURN |
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346 | CC END IF |
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347 | C |
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348 | C *** CALCULATE LAYER CONTAINING LCL (=ICB) *** |
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349 | C |
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350 | ICB=NL-1 |
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351 | c sb DO 50 I=2,NL-1 |
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352 | DO 50 I=3,NL-1 ! modif sb pour que ICB soit sup/egal a 2 |
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353 | C la modification consiste a comparer PLCL a PH et non a P: |
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354 | C ICB est defini par : PH(ICB)<PLCL<PH(ICB-!) |
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355 | IF(PH(I).LT.PLCL)THEN |
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356 | ICB=MIN(ICB,I) |
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357 | END IF |
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358 | 50 CONTINUE |
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359 | IF(ICB.EQ.(NL-1))THEN |
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360 | IFLAG=3 |
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361 | RETURN |
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362 | END IF |
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363 | ICB = ICB-1 ! ICB sup ou egal a 2 |
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364 | Cjyg2 |
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365 | C |
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366 | C |
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367 | |
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368 | C *** SUBROUTINE TLIFT CALCULATES PART OF THE LIFTED PARCEL VIRTUAL *** |
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369 | C *** TEMPERATURE, THE ACTUAL TEMPERATURE AND THE ADIABATIC *** |
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370 | C *** LIQUID WATER CONTENT *** |
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371 | C |
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372 | |
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373 | cjyg1 |
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374 | c make sure that "Cloud base" seen by TLIFT is actually the |
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375 | c fisrt level where adiabatic ascent is saturated |
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376 | IF (PLCL .GT. P(ICB)) THEN |
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377 | c sb CALL TLIFT(P,T,RR,RS,GZ,PLCL,ICB,TVP,TP,CLW,ND,NL) |
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378 | CALL TLIFT(P,T,RR,RS,GZ,PLCL,ICB,NK,TVP,TP,CLW,ND,NL |
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379 | : ,DTVPDT1,DTVPDQ1) |
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380 | ELSE |
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381 | c sb CALL TLIFT(P,T,RR,RS,GZ,PLCL,ICB+1,TVP,TP,CLW,ND,NL) |
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382 | CALL TLIFT(P,T,RR,RS,GZ,PLCL,ICB+1,NK,TVP,TP,CLW,ND,NL |
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383 | : ,DTVPDT1,DTVPDQ1) |
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384 | ENDIF |
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385 | cjyg2 |
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386 | |
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387 | ****************************************************************************** |
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388 | **** SORTIE DE LA TEMPERATURE DE L ASCENDANCE NON DILUE |
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389 | ****************************************************************************** |
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390 | do i=1,ND |
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391 | TPS(i)=TP(i) |
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392 | enddo |
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393 | |
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394 | |
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395 | ****************************************************************************** |
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396 | |
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397 | C |
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398 | C *** SET THE PRECIPITATION EFFICIENCIES AND THE FRACTION OF *** |
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399 | C *** PRECIPITATION FALLING OUTSIDE OF CLOUD *** |
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400 | C *** THESE MAY BE FUNCTIONS OF TP(I), P(I) AND CLW(I) *** |
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401 | C |
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402 | DO 55 I=1,NL |
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403 | PDEN=PTCRIT-PBCRIT |
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404 | c |
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405 | cjyg |
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406 | ccc EP(I)=(P(ICB)-P(I)-PBCRIT)/PDEN |
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407 | c sb EP(I)=(PLCL-P(I)-PBCRIT)/PDEN |
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408 | EP(I)=(PLCL-P(I)-PBCRIT)/PDEN * EPMAX ! sb |
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409 | c |
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410 | EP(I)=AMAX1(EP(I),0.0) |
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411 | c sb EP(I)=AMIN1(EP(I),1.0) |
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412 | EP(I)=AMIN1(EP(I),EPMAX) ! sb |
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413 | SIGP(I)=SPFAC |
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414 | C |
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415 | C *** CALCULATE VIRTUAL TEMPERATURE AND LIFTED PARCEL *** |
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416 | C *** VIRTUAL TEMPERATURE *** |
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417 | C |
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418 | TV(I)=T(I)*(1.+RR(I)/EPS-RR(I)) |
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419 | Ccd1 |
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420 | C . Keep all liquid water in lifted parcel (-> adiabatic CAPE) |
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421 | C |
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422 | ccc TVP(I)=TVP(I)-TP(I)*(RR(1)-EP(I)*CLW(I)) |
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423 | c!!! sb TVP(I)=TVP(I)-TP(I)*RR(1) ! calcule dans tlift |
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424 | Ccd2 |
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425 | C |
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426 | C *** Calculate first estimate of buoyancy |
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427 | C |
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428 | BUOY(I) = TVP(I) - TV(I) |
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429 | 55 CONTINUE |
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430 | C |
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431 | C *** Set Cloud Base Buoyancy at (Plcl+DPbase) level buoyancy |
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432 | C |
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433 | DPBASE = -40. !That is 400m above LCL |
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434 | PBASE = PLCL + DPBASE |
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435 | TVPBASE = TVP(ICB )*(PBASE -P(ICB+1))/(P(ICB)-P(ICB+1)) |
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436 | $ +TVP(ICB+1)*(P(ICB)-PBASE )/(P(ICB)-P(ICB+1)) |
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437 | TVBASE = TV(ICB )*(PBASE -P(ICB+1))/(P(ICB)-P(ICB+1)) |
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438 | $ +TV(ICB+1)*(P(ICB)-PBASE )/(P(ICB)-P(ICB+1)) |
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439 | C |
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440 | c test sb: |
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441 | c@ write(*,*) '++++++++++++++++++++++++++++++++++++++++' |
---|
442 | c@ write(*,*) 'plcl,dpbas,tvpbas,tvbas,tvp(icb),tvp(icb1) |
---|
443 | c@ : ,tv(icb),tv(icb1)' |
---|
444 | c@ write(*,*) plcl,dpbase,tvpbase,tvbase,tvp(icb) |
---|
445 | c@ L ,tvp(icb+1),tv(icb),tv(icb+1) |
---|
446 | c@ write(*,*) '++++++++++++++++++++++++++++++++++++++++' |
---|
447 | c fin test sb |
---|
448 | BUOYBASE = TVPBASE - TVBASE |
---|
449 | C |
---|
450 | CC Set buoyancy = BUOYBASE for all levels below BASE. |
---|
451 | CC For safety, set : BUOY(ICB) = BUOYBASE |
---|
452 | DO I = ICB,NL |
---|
453 | IF (P(I) .GE. PBASE) THEN |
---|
454 | BUOY(I) = BUOYBASE |
---|
455 | ENDIF |
---|
456 | ENDDO |
---|
457 | BUOY(ICB) = BUOYBASE |
---|
458 | C |
---|
459 | c sb3d print *,'buoybase,tvp_tv,tvpbase,tvbase,pbase,plcl' |
---|
460 | c sb3d $, buoybase,tvp(icb)-tv(icb),tvpbase,tvbase,pbase,plcl |
---|
461 | c sb3d print *,'TVP ',(tvp(i),i=1,nl) |
---|
462 | c sb3d print *,'TV ',(tv(i),i=1,nl) |
---|
463 | c sb3d print *, 'P ',(p(i),i=1,nl) |
---|
464 | c sb3d print *,'ICB ',icb |
---|
465 | c test sb: |
---|
466 | c@ write(*,*) '@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@' |
---|
467 | c@ write(*,*) 'icb,icbs,inb,buoybase:' |
---|
468 | c@ write(*,*) icb,icb+1,inb,buoybase |
---|
469 | c@ write(*,*) 'k,tvp,tv,tp,buoy,ep: ' |
---|
470 | c@ do k=1,nl |
---|
471 | c@ write(*,*) k,tvp(k),tv(k),tp(k),buoy(k),ep(k) |
---|
472 | c@ enddo |
---|
473 | c@ write(*,*) '@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@@' |
---|
474 | c fin test sb |
---|
475 | |
---|
476 | |
---|
477 | C |
---|
478 | C *** MAKE SURE THAT COLUMN IS DRY ADIABATIC BETWEEN THE SURFACE *** |
---|
479 | C *** AND CLOUD BASE, AND THAT LIFTED AIR IS POSITIVELY BUOYANT *** |
---|
480 | C *** AT CLOUD BASE *** |
---|
481 | C *** IF NOT, RETURN TO CALLING PROGRAM AFTER RESETTING *** |
---|
482 | C *** SIG(I) AND W0(I) *** |
---|
483 | C |
---|
484 | Cjyg |
---|
485 | CCC TDIF=TVP(ICB)-TV(ICB) |
---|
486 | TDIF = BUOY(ICB) |
---|
487 | ATH1=TH(1) |
---|
488 | Cjyg |
---|
489 | CCC ATH=TH(ICB-1)-1.0 |
---|
490 | ATH=TH(ICB-1)-5.0 |
---|
491 | c ATH=0. ! ajout sb |
---|
492 | c IF (ICB.GT.1) ATH=TH(ICB-1)-5.0 ! modif sb |
---|
493 | IF(TDIF.LT.DTCRIT.OR.ATH.GT.ATH1)THEN |
---|
494 | DO 60 I=1,NL |
---|
495 | SIG(I)=BETA*SIG(I)-2.*ALPHA*TDIF*TDIF |
---|
496 | SIG(I)=AMAX1(SIG(I),0.0) |
---|
497 | W0(I)=BETA*W0(I) |
---|
498 | 60 CONTINUE |
---|
499 | IFLAG=0 |
---|
500 | RETURN |
---|
501 | END IF |
---|
502 | C |
---|
503 | |
---|
504 | |
---|
505 | C *** IF THIS POINT IS REACHED, MOIST CONVECTIVE ADJUSTMENT IS NECESSARY *** |
---|
506 | C *** NOW INITIALIZE VARIOUS ARRAYS USED IN THE COMPUTATIONS *** |
---|
507 | C |
---|
508 | DO 70 I=1,NL |
---|
509 | HP(I)=H(I) |
---|
510 | WT(I)=0.001 |
---|
511 | RP(I)=RR(I) |
---|
512 | UP(I)=U(I) |
---|
513 | VP(I)=V(I) |
---|
514 | DO 71 J=1,NTRA |
---|
515 | TRAP(I,J)=TRA(I,J) |
---|
516 | 71 CONTINUE |
---|
517 | NENT(I)=0 |
---|
518 | WATER(I)=0.0 |
---|
519 | EVAP(I)=0.0 |
---|
520 | B(I)=0.0 |
---|
521 | MP(I)=0.0 |
---|
522 | M(I)=0.0 |
---|
523 | LV(I)=ALV0-CPVMCL*(T(I)-273.15) |
---|
524 | LVCP(I)=LV(I)/CPN(I) |
---|
525 | DO 70 J=1,NL |
---|
526 | QENT(I,J)=RR(J) |
---|
527 | ELIJ(I,J)=0.0 |
---|
528 | MENT(I,J)=0.0 |
---|
529 | SIJ(I,J)=0.0 |
---|
530 | UENT(I,J)=U(J) |
---|
531 | VENT(I,J)=V(J) |
---|
532 | DO 70 K=1,NTRA |
---|
533 | TRAENT(I,J,K)=TRA(J,K) |
---|
534 | 70 CONTINUE |
---|
535 | |
---|
536 | DELTI=1.0/DELT |
---|
537 | C |
---|
538 | C *** FIND THE FIRST MODEL LEVEL (INB) ABOVE THE PARCEL'S *** |
---|
539 | C *** LEVEL OF NEUTRAL BUOYANCY *** |
---|
540 | C |
---|
541 | INB=NL-1 |
---|
542 | DO 80 I=ICB,NL-1 |
---|
543 | Cjyg |
---|
544 | CCC IF((TVP(I)-TV(I)).LT.DTCRIT)THEN |
---|
545 | IF(BUOY(I).LT.DTOVSH)THEN |
---|
546 | INB=MIN(INB,I) |
---|
547 | END IF |
---|
548 | 80 CONTINUE |
---|
549 | |
---|
550 | |
---|
551 | |
---|
552 | |
---|
553 | C |
---|
554 | C *** RESET SIG(I) AND W0(I) FOR I>INB AND I<ICB *** |
---|
555 | C |
---|
556 | IF(INB.LT.(NL-1))THEN |
---|
557 | DO 85 I=INB+1,NL-1 |
---|
558 | Cjyg |
---|
559 | CCC SIG(I)=BETA*SIG(I)-2.0E-4*ALPHA*(TV(INB)-TVP(INB))* |
---|
560 | CCC 1 ABS(TV(INB)-TVP(INB)) |
---|
561 | SIG(I)=BETA*SIG(I)+2.*ALPHA*BUOY(INB)* |
---|
562 | 1 ABS(BUOY(INB)) |
---|
563 | SIG(I)=AMAX1(SIG(I),0.0) |
---|
564 | W0(I)=BETA*W0(I) |
---|
565 | 85 CONTINUE |
---|
566 | END IF |
---|
567 | DO 87 I=1,ICB |
---|
568 | Cjyg |
---|
569 | CCC SIG(I)=BETA*SIG(I)-2.0E-4*ALPHA*(TV(ICB)-TVP(ICB))* |
---|
570 | CCC 1 (TV(ICB)-TVP(ICB)) |
---|
571 | SIG(I)=BETA*SIG(I)-2.*ALPHA*BUOY(ICB)*BUOY(ICB) |
---|
572 | SIG(I)=AMAX1(SIG(I),0.0) |
---|
573 | W0(I)=BETA*W0(I) |
---|
574 | 87 CONTINUE |
---|
575 | C |
---|
576 | C *** RESET FRACTIONAL AREAS OF UPDRAFTS AND W0 AT INITIAL TIME *** |
---|
577 | C *** AND AFTER 10 TIME STEPS OF NO CONVECTION *** |
---|
578 | C |
---|
579 | |
---|
580 | IF(SIG(ND).LT.1.5.OR.SIG(ND).GT.12.0)THEN |
---|
581 | DO 90 I=1,NL-1 |
---|
582 | SIG(I)=0.0 |
---|
583 | W0(I)=0.0 |
---|
584 | 90 CONTINUE |
---|
585 | END IF |
---|
586 | C |
---|
587 | C *** CALCULATE LIQUID WATER STATIC ENERGY OF LIFTED PARCEL *** |
---|
588 | C |
---|
589 | DO 95 I=ICB,INB |
---|
590 | HP(I)=H(1)+(LV(I)+(CPD-CPV)*T(I))*EP(I)*CLW(I) |
---|
591 | 95 CONTINUE |
---|
592 | C |
---|
593 | C *** CALCULATE CONVECTIVE AVAILABLE POTENTIAL ENERGY (CAPE), *** |
---|
594 | C *** VERTICAL VELOCITY (W), FRACTIONAL AREA COVERED BY *** |
---|
595 | C *** UNDILUTE UPDRAFT (SIG), AND UPDRAFT MASS FLUX (M) *** |
---|
596 | C |
---|
597 | CAPE=0.0 |
---|
598 | C |
---|
599 | DO 98 I=ICB+1,INB |
---|
600 | Cjyg1 |
---|
601 | CCC CAPE=CAPE+RD*(TVP(I-1)-TV(I-1))*(PH(I-1)-PH(I))/P(I-1) |
---|
602 | CCC DCAPE=RD*BUOY(I-1)*(PH(I-1)-PH(I))/P(I-1) |
---|
603 | CCC DLNP=(PH(I-1)-PH(I))/P(I-1) |
---|
604 | C The interval on which CAPE is computed starts at PBASE : |
---|
605 | DELTAP = MIN(PBASE,PH(I-1))-MIN(PBASE,PH(I)) |
---|
606 | CAPE=CAPE+RD*BUOY(I-1)*DELTAP/P(I-1) |
---|
607 | DCAPE=RD*BUOY(I-1)*DELTAP/P(I-1) |
---|
608 | DLNP=DELTAP/P(I-1) |
---|
609 | Cjyg2 |
---|
610 | c sb3d print *,'buoy,dlnp,dcape,cape',buoy(i-1),dlnp,dcape,cape |
---|
611 | c test sb: |
---|
612 | c@ write(*,*) '############################################' |
---|
613 | c@ write(*,*) 'cape,rrd,buoy,deltap,p,pbase,ph:' |
---|
614 | c@ : ,cape,rd,buoy(i-1),deltap,p(i-1),pbase,ph(i) |
---|
615 | c@ write(*,*) '############################################' |
---|
616 | |
---|
617 | c fin test sb |
---|
618 | CAPE=AMAX1(0.0,CAPE) |
---|
619 | C |
---|
620 | SIGOLD=SIG(I) |
---|
621 | DTMIN=100.0 |
---|
622 | DO 97 J=ICB,I-1 |
---|
623 | Cjyg |
---|
624 | CCC DTMIN=AMIN1(DTMIN,(TVP(J)-TV(J))) |
---|
625 | DTMIN=AMIN1(DTMIN,BUOY(J)) |
---|
626 | 97 CONTINUE |
---|
627 | c sb3d print *, 'DTMIN, BETA, ALPHA, SIG = ',DTMIN,BETA,ALPHA,SIG(I) |
---|
628 | SIG(I)=BETA*SIG(I)+ALPHA*DTMIN*ABS(DTMIN) |
---|
629 | SIG(I)=AMAX1(SIG(I),0.0) |
---|
630 | SIG(I)=AMIN1(SIG(I),0.01) |
---|
631 | FAC=AMIN1(((DTCRIT-DTMIN)/DTCRIT),1.0) |
---|
632 | Cjyg |
---|
633 | CC Essais de reduction de la vitesse |
---|
634 | CC FAC = FAC*.5 |
---|
635 | C |
---|
636 | W=(1.-BETA)*FAC*SQRT(CAPE)+BETA*W0(I) |
---|
637 | AMU=0.5*(SIG(I)+SIGOLD)*W |
---|
638 | M(I)=AMU*0.007*P(I)*(PH(I)-PH(I+1))/TV(I) |
---|
639 | |
---|
640 | c --------- test sb: |
---|
641 | c write(*,*) '############################################' |
---|
642 | c write(*,*) 'k,amu,buoy(k-1),deltap,w,beta,fac,cape,w0(k)' |
---|
643 | c write(*,*) i,amu,buoy(i-1),deltap |
---|
644 | c : ,w,beta,fac,cape,w0(i) |
---|
645 | c write(*,*) '############################################' |
---|
646 | c --------- |
---|
647 | |
---|
648 | W0(I)=W |
---|
649 | 98 CONTINUE |
---|
650 | W0(ICB)=0.5*W0(ICB+1) |
---|
651 | M(ICB)=0.5*M(ICB+1)*(PH(ICB)-PH(ICB+1))/(PH(ICB+1)-PH(ICB+2)) |
---|
652 | SIG(ICB)=SIG(ICB+1) |
---|
653 | SIG(ICB-1)=SIG(ICB) |
---|
654 | cjyg1 |
---|
655 | c sb3d print *, 'Cloud base, c. top, CAPE',ICB,INB,cape |
---|
656 | c sb3d print *, 'SIG ',(sig(i),i=1,inb) |
---|
657 | c sb3d print *, 'W ',(w0(i),i=1,inb) |
---|
658 | c sb3d print *, 'M ',(m(i), i=1,inb) |
---|
659 | c sb3d print *, 'Dt1 ',(tvp(i)-tv(i),i=1,inb) |
---|
660 | c sb3d print *, 'Dt_vrai ',(buoy(i),i=1,inb) |
---|
661 | Cjyg2 |
---|
662 | C |
---|
663 | C *** CALCULATE ENTRAINED AIR MASS FLUX (MENT), TOTAL WATER MIXING *** |
---|
664 | C *** RATIO (QENT), TOTAL CONDENSED WATER (ELIJ), AND MIXING *** |
---|
665 | C *** FRACTION (SIJ) *** |
---|
666 | C |
---|
667 | |
---|
668 | |
---|
669 | DO 170 I=ICB,INB |
---|
670 | RTI=RR(1)-EP(I)*CLW(I) |
---|
671 | DO 160 J=ICB-1,INB |
---|
672 | BF2=1.+LV(J)*LV(J)*RS(J)/(RV*T(J)*T(J)*CPD) |
---|
673 | ANUM=H(J)-HP(I)+(CPV-CPD)*T(J)*(RTI-RR(J)) |
---|
674 | DENOM=H(I)-HP(I)+(CPD-CPV)*(RR(I)-RTI)*T(J) |
---|
675 | DEI=DENOM |
---|
676 | IF(ABS(DEI).LT.0.01)DEI=0.01 |
---|
677 | SIJ(I,J)=ANUM/DEI |
---|
678 | SIJ(I,I)=1.0 |
---|
679 | ALTEM=SIJ(I,J)*RR(I)+(1.-SIJ(I,J))*RTI-RS(J) |
---|
680 | ALTEM=ALTEM/BF2 |
---|
681 | CWAT=CLW(J)*(1.-EP(J)) |
---|
682 | STEMP=SIJ(I,J) |
---|
683 | IF((STEMP.LT.0.0.OR.STEMP.GT.1.0.OR. |
---|
684 | 1 ALTEM.GT.CWAT).AND.J.GT.I)THEN |
---|
685 | ANUM=ANUM-LV(J)*(RTI-RS(J)-CWAT*BF2) |
---|
686 | DENOM=DENOM+LV(J)*(RR(I)-RTI) |
---|
687 | IF(ABS(DENOM).LT.0.01)DENOM=0.01 |
---|
688 | SIJ(I,J)=ANUM/DENOM |
---|
689 | ALTEM=SIJ(I,J)*RR(I)+(1.-SIJ(I,J))*RTI-RS(J) |
---|
690 | ALTEM=ALTEM-(BF2-1.)*CWAT |
---|
691 | END IF |
---|
692 | |
---|
693 | |
---|
694 | IF(SIJ(I,J).GT.0.0.AND.SIJ(I,J).LT.0.95)THEN |
---|
695 | QENT(I,J)=SIJ(I,J)*RR(I)+(1.-SIJ(I,J))*RTI |
---|
696 | UENT(I,J)=SIJ(I,J)*U(I)+(1.-SIJ(I,J))*U(NK) |
---|
697 | VENT(I,J)=SIJ(I,J)*V(I)+(1.-SIJ(I,J))*V(NK) |
---|
698 | DO K=1,NTRA |
---|
699 | TRAENT(I,J,K)=SIJ(I,J)*TRA(I,K)+(1.-SIJ(I,J))* |
---|
700 | 1 TRA(NK,K) |
---|
701 | END DO |
---|
702 | ELIJ(I,J)=ALTEM |
---|
703 | ELIJ(I,J)=AMAX1(0.0,ELIJ(I,J)) |
---|
704 | MENT(I,J)=M(I)/(1.-SIJ(I,J)) |
---|
705 | NENT(I)=NENT(I)+1 |
---|
706 | END IF |
---|
707 | SIJ(I,J)=AMAX1(0.0,SIJ(I,J)) |
---|
708 | SIJ(I,J)=AMIN1(1.0,SIJ(I,J)) |
---|
709 | 160 CONTINUE |
---|
710 | C |
---|
711 | C *** IF NO AIR CAN ENTRAIN AT LEVEL I ASSUME THAT UPDRAFT DETRAINS *** |
---|
712 | C *** AT THAT LEVEL AND CALCULATE DETRAINED AIR FLUX AND PROPERTIES *** |
---|
713 | C |
---|
714 | IF(NENT(I).EQ.0)THEN |
---|
715 | MENT(I,I)=M(I) |
---|
716 | QENT(I,I)=RR(NK)-EP(I)*CLW(I) |
---|
717 | UENT(I,I)=U(NK) |
---|
718 | VENT(I,I)=V(NK) |
---|
719 | DO J=1,NTRA |
---|
720 | TRAENT(I,I,J)=TRA(NK,J) |
---|
721 | END DO |
---|
722 | ELIJ(I,I)=CLW(I) |
---|
723 | SIJ(I,I)=1.0 |
---|
724 | END IF |
---|
725 | C |
---|
726 | DO J = ICB-1,INB |
---|
727 | SIGIJ(I,J) = SIJ(I,J) |
---|
728 | ENDDO |
---|
729 | C |
---|
730 | 170 CONTINUE |
---|
731 | C |
---|
732 | C *** NORMALIZE ENTRAINED AIR MASS FLUXES TO REPRESENT EQUAL *** |
---|
733 | C *** PROBABILITIES OF MIXING *** |
---|
734 | C |
---|
735 | |
---|
736 | DO 200 I=ICB,INB |
---|
737 | IF(NENT(I).NE.0)THEN |
---|
738 | QP=RR(1)-EP(I)*CLW(I) |
---|
739 | ANUM=H(I)-HP(I)-LV(I)*(QP-RS(I))+(CPV-CPD)*T(I)* |
---|
740 | 1 (QP-RR(I)) |
---|
741 | DENOM=H(I)-HP(I)+LV(I)*(RR(I)-QP)+ |
---|
742 | 1 (CPD-CPV)*T(I)*(RR(I)-QP) |
---|
743 | IF(ABS(DENOM).LT.0.01)DENOM=0.01 |
---|
744 | SCRIT=ANUM/DENOM |
---|
745 | ALT=QP-RS(I)+SCRIT*(RR(I)-QP) |
---|
746 | IF(SCRIT.LE.0.0.OR.ALT.LE.0.0)SCRIT=1.0 |
---|
747 | SMAX=0.0 |
---|
748 | ASIJ=0.0 |
---|
749 | DO 175 J=INB,ICB-1,-1 |
---|
750 | IF(SIJ(I,J).GT.1.0E-16.AND.SIJ(I,J).LT.0.95)THEN |
---|
751 | WGH=1.0 |
---|
752 | IF(J.GT.I)THEN |
---|
753 | SJMAX=AMAX1(SIJ(I,J+1),SMAX) |
---|
754 | SJMAX=AMIN1(SJMAX,SCRIT) |
---|
755 | SMAX=AMAX1(SIJ(I,J),SMAX) |
---|
756 | SJMIN=AMAX1(SIJ(I,J-1),SMAX) |
---|
757 | SJMIN=AMIN1(SJMIN,SCRIT) |
---|
758 | IF(SIJ(I,J).LT.(SMAX-1.0E-16))WGH=0.0 |
---|
759 | SMID=AMIN1(SIJ(I,J),SCRIT) |
---|
760 | ELSE |
---|
761 | SJMAX=AMAX1(SIJ(I,J+1),SCRIT) |
---|
762 | SMID=AMAX1(SIJ(I,J),SCRIT) |
---|
763 | SJMIN=0.0 |
---|
764 | IF(J.GT.1)SJMIN=SIJ(I,J-1) |
---|
765 | SJMIN=AMAX1(SJMIN,SCRIT) |
---|
766 | END IF |
---|
767 | DELP=ABS(SJMAX-SMID) |
---|
768 | DELM=ABS(SJMIN-SMID) |
---|
769 | ASIJ=ASIJ+WGH*(DELP+DELM) |
---|
770 | MENT(I,J)=MENT(I,J)*(DELP+DELM)*WGH |
---|
771 | END IF |
---|
772 | 175 CONTINUE |
---|
773 | ASIJ=AMAX1(1.0E-16,ASIJ) |
---|
774 | ASIJ=1.0/ASIJ |
---|
775 | DO 180 J=ICB-1,INB |
---|
776 | MENT(I,J)=MENT(I,J)*ASIJ |
---|
777 | 180 CONTINUE |
---|
778 | ASUM=0.0 |
---|
779 | BSUM=0.0 |
---|
780 | DO 190 J=ICB-1,INB |
---|
781 | ASUM=ASUM+MENT(I,J) |
---|
782 | MENT(I,J)=MENT(I,J)*SIG(J) |
---|
783 | BSUM=BSUM+MENT(I,J) |
---|
784 | 190 CONTINUE |
---|
785 | BSUM=AMAX1(BSUM,1.0E-16) |
---|
786 | BSUM=1.0/BSUM |
---|
787 | DO 195 J=ICB-1,INB |
---|
788 | MENT(I,J)=MENT(I,J)*ASUM*BSUM |
---|
789 | 195 CONTINUE |
---|
790 | CSUM=0.0 |
---|
791 | DO 197 J=ICB-1,INB |
---|
792 | CSUM=CSUM+MENT(I,J) |
---|
793 | 197 CONTINUE |
---|
794 | |
---|
795 | IF(CSUM.LT.M(I))THEN |
---|
796 | NENT(I)=0 |
---|
797 | MENT(I,I)=M(I) |
---|
798 | QENT(I,I)=RR(1)-EP(I)*CLW(I) |
---|
799 | UENT(I,I)=U(NK) |
---|
800 | VENT(I,I)=V(NK) |
---|
801 | DO J=1,NTRA |
---|
802 | TRAENT(I,I,J)=TRA(NK,J) |
---|
803 | END DO |
---|
804 | ELIJ(I,I)=CLW(I) |
---|
805 | SIJ(I,I)=1.0 |
---|
806 | END IF |
---|
807 | END IF |
---|
808 | 200 CONTINUE |
---|
809 | |
---|
810 | |
---|
811 | |
---|
812 | *************************************************************** |
---|
813 | ** CALCUL DES MENTS(I,J) ET DES QENTS(I,J) |
---|
814 | ************************************************************** |
---|
815 | |
---|
816 | DO im=1,nd |
---|
817 | do jm=1,nd |
---|
818 | |
---|
819 | QENTS(im,jm)=QENT(im,jm) |
---|
820 | MENTS(im,jm)=MENT(im,jm) |
---|
821 | enddo |
---|
822 | enddo |
---|
823 | |
---|
824 | *********************************************************** |
---|
825 | c--- test sb: |
---|
826 | c@ write(*,*) '^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^' |
---|
827 | c@ write(*,*) 'inb,m(inb),ment(inb,inb),sigij(inb,inb):' |
---|
828 | c@ write(*,*) inb,m(inb),ment(inb,inb),sigij(inb,inb) |
---|
829 | c@ write(*,*) '^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^^' |
---|
830 | c--- |
---|
831 | |
---|
832 | |
---|
833 | |
---|
834 | |
---|
835 | C |
---|
836 | C *** CHECK WHETHER EP(INB)=0, IF SO, SKIP PRECIPITATING *** |
---|
837 | C *** DOWNDRAFT CALCULATION *** |
---|
838 | C |
---|
839 | IF(EP(INB).LT.0.0001)GOTO 405 |
---|
840 | C |
---|
841 | C *** INTEGRATE LIQUID WATER EQUATION TO FIND CONDENSED WATER *** |
---|
842 | C *** AND CONDENSED WATER FLUX *** |
---|
843 | C |
---|
844 | WFLUX=0.0 |
---|
845 | TINV=1./3. |
---|
846 | C |
---|
847 | C *** BEGIN DOWNDRAFT LOOP *** |
---|
848 | C |
---|
849 | DO 400 I=INB,1,-1 |
---|
850 | C |
---|
851 | C *** CALCULATE DETRAINED PRECIPITATION *** |
---|
852 | C |
---|
853 | |
---|
854 | |
---|
855 | WDTRAIN=10.0*EP(I)*M(I)*CLW(I) |
---|
856 | IF(I.GT.1)THEN |
---|
857 | DO 320 J=1,I-1 |
---|
858 | AWAT=ELIJ(J,I)-(1.-EP(I))*CLW(I) |
---|
859 | AWAT=AMAX1(AWAT,0.0) |
---|
860 | 320 WDTRAIN=WDTRAIN+10.0*AWAT*MENT(J,I) |
---|
861 | END IF |
---|
862 | C |
---|
863 | C *** FIND RAIN WATER AND EVAPORATION USING PROVISIONAL *** |
---|
864 | C *** ESTIMATES OF RP(I)AND RP(I-1) *** |
---|
865 | C |
---|
866 | |
---|
867 | |
---|
868 | WT(I)=45.0 |
---|
869 | IF(I.LT.INB)THEN |
---|
870 | RP(I)=RP(I+1)+(CPD*(T(I+1)-T(I))+GZ(I+1)-GZ(I))/LV(I) |
---|
871 | RP(I)=0.5*(RP(I)+RR(I)) |
---|
872 | END IF |
---|
873 | RP(I)=AMAX1(RP(I),0.0) |
---|
874 | RP(I)=AMIN1(RP(I),RS(I)) |
---|
875 | RP(INB)=RR(INB) |
---|
876 | IF(I.EQ.1)THEN |
---|
877 | AFAC=P(1)*(RS(1)-RP(1))/(1.0E4+2000.0*P(1)*RS(1)) |
---|
878 | ELSE |
---|
879 | RP(I-1)=RP(I)+(CPD*(T(I)-T(I-1))+GZ(I)-GZ(I-1))/LV(I) |
---|
880 | RP(I-1)=0.5*(RP(I-1)+RR(I-1)) |
---|
881 | RP(I-1)=AMIN1(RP(I-1),RS(I-1)) |
---|
882 | RP(I-1)=AMAX1(RP(I-1),0.0) |
---|
883 | AFAC1=P(I)*(RS(I)-RP(I))/(1.0E4+2000.0*P(I)*RS(I)) |
---|
884 | AFAC2=P(I-1)*(RS(I-1)-RP(I-1))/(1.0E4+ |
---|
885 | 1 2000.0*P(I-1)*RS(I-1)) |
---|
886 | AFAC=0.5*(AFAC1+AFAC2) |
---|
887 | END IF |
---|
888 | IF(I.EQ.INB)AFAC=0.0 |
---|
889 | AFAC=AMAX1(AFAC,0.0) |
---|
890 | BFAC=1./(SIGD*WT(I)) |
---|
891 | C |
---|
892 | Cjyg1 |
---|
893 | CCC SIGT=1.0 |
---|
894 | CCC IF(I.GE.ICB)SIGT=SIGP(I) |
---|
895 | C Prise en compte de la variation progressive de SIGT dans |
---|
896 | C les couches ICB et ICB-1: |
---|
897 | C Pour PLCL<PH(I+1), PR1=0 & PR2=1 |
---|
898 | C Pour PLCL>PH(I), PR1=1 & PR2=0 |
---|
899 | C Pour PH(I+1)<PLCL<PH(I), PR1 est la proportion a cheval |
---|
900 | C sur le nuage, et PR2 est la proportion sous la base du |
---|
901 | C nuage. |
---|
902 | PR1 =(PLCL-PH(I+1))/(PH(I)-PH(I+1)) |
---|
903 | PR1 = MAX(0.,MIN(1.,PR1)) |
---|
904 | PR2 = (PH(I)-PLCL)/(PH(I)-PH(I+1)) |
---|
905 | PR2 = MAX(0.,MIN(1.,PR2)) |
---|
906 | SIGT = SIGP(I)*PR1 + PR2 |
---|
907 | c sb3d print *,'i,sigt,pr1,pr2', i,sigt,pr1,pr2 |
---|
908 | Cjyg2 |
---|
909 | C |
---|
910 | B6=BFAC*50.*SIGD*(PH(I)-PH(I+1))*SIGT*AFAC |
---|
911 | C6=WATER(I+1)+BFAC*WDTRAIN-50.*SIGD*BFAC* |
---|
912 | 1 (PH(I)-PH(I+1))*EVAP(I+1) |
---|
913 | IF(C6.GT.0.0)THEN |
---|
914 | REVAP=0.5*(-B6+SQRT(B6*B6+4.*C6)) |
---|
915 | EVAP(I)=SIGT*AFAC*REVAP |
---|
916 | WATER(I)=REVAP*REVAP |
---|
917 | ELSE |
---|
918 | EVAP(I)=-EVAP(I+1)+0.02*(WDTRAIN+SIGD*WT(I)* |
---|
919 | 1 WATER(I+1))/(SIGD*(PH(I)-PH(I+1))) |
---|
920 | END IF |
---|
921 | |
---|
922 | |
---|
923 | C |
---|
924 | C *** CALCULATE PRECIPITATING DOWNDRAFT MASS FLUX UNDER *** |
---|
925 | C *** HYDROSTATIC APPROXIMATION *** |
---|
926 | C |
---|
927 | IF(I.EQ.1)GOTO 360 |
---|
928 | TEVAP=AMAX1(0.0,EVAP(I)) |
---|
929 | DELTH=AMAX1(0.001,(TH(I)-TH(I-1))) |
---|
930 | MP(I)=10.*LVCP(I)*SIGD*TEVAP*(P(I-1)-P(I))/DELTH |
---|
931 | C |
---|
932 | C *** IF HYDROSTATIC ASSUMPTION FAILS, *** |
---|
933 | C *** SOLVE CUBIC DIFFERENCE EQUATION FOR DOWNDRAFT THETA *** |
---|
934 | C *** AND MASS FLUX FROM TWO SIMULTANEOUS DIFFERENTIAL EQNS *** |
---|
935 | C |
---|
936 | AMFAC=SIGD*SIGD*70.0*PH(I)*(P(I-1)-P(I))* |
---|
937 | 1 (TH(I)-TH(I-1))/(TV(I)*TH(I)) |
---|
938 | AMP2=ABS(MP(I+1)*MP(I+1)-MP(I)*MP(I)) |
---|
939 | IF(AMP2.GT.(0.1*AMFAC))THEN |
---|
940 | XF=100.0*SIGD*SIGD*SIGD*(PH(I)-PH(I+1)) |
---|
941 | TF=B(I)-5.0*(TH(I)-TH(I-1))*T(I)/(LVCP(I)*SIGD*TH(I)) |
---|
942 | AF=XF*TF+MP(I+1)*MP(I+1)*TINV |
---|
943 | BF=2.*(TINV*MP(I+1))**3+TINV*MP(I+1)*XF*TF+50.* |
---|
944 | 1 (P(I-1)-P(I))*XF*TEVAP |
---|
945 | FAC2=1.0 |
---|
946 | IF(BF.LT.0.0)FAC2=-1.0 |
---|
947 | BF=ABS(BF) |
---|
948 | UR=0.25*BF*BF-AF*AF*AF*TINV*TINV*TINV |
---|
949 | IF(UR.GE.0.0)THEN |
---|
950 | SRU=SQRT(UR) |
---|
951 | FAC=1.0 |
---|
952 | IF((0.5*BF-SRU).LT.0.0)FAC=-1.0 |
---|
953 | MP(I)=MP(I+1)*TINV+(0.5*BF+SRU)**TINV+ |
---|
954 | 1 FAC*(ABS(0.5*BF-SRU))**TINV |
---|
955 | ELSE |
---|
956 | D=ATAN(2.*SQRT(-UR)/(BF+1.0E-28)) |
---|
957 | IF(FAC2.LT.0.0)D=3.14159-D |
---|
958 | MP(I)=MP(I+1)*TINV+2.*SQRT(AF*TINV)*COS(D*TINV) |
---|
959 | END IF |
---|
960 | MP(I)=AMAX1(0.0,MP(I)) |
---|
961 | B(I-1)=B(I)+100.0*(P(I-1)-P(I))*TEVAP/(MP(I)+SIGD*0.1)- |
---|
962 | 1 10.0*(TH(I)-TH(I-1))*T(I)/(LVCP(I)*SIGD*TH(I)) |
---|
963 | B(I-1)=AMAX1(B(I-1),0.0) |
---|
964 | END IF |
---|
965 | |
---|
966 | |
---|
967 | C |
---|
968 | C *** LIMIT MAGNITUDE OF MP(I) TO MEET CFL CONDITION *** |
---|
969 | C |
---|
970 | AMPMAX=2.0*(PH(I)-PH(I+1))*DELTI |
---|
971 | AMP2=2.0*(PH(I-1)-PH(I))*DELTI |
---|
972 | AMPMAX=AMIN1(AMPMAX,AMP2) |
---|
973 | MP(I)=AMIN1(MP(I),AMPMAX) |
---|
974 | C |
---|
975 | C *** FORCE MP TO DECREASE LINEARLY TO ZERO *** |
---|
976 | C *** BETWEEN CLOUD BASE AND THE SURFACE *** |
---|
977 | C |
---|
978 | IF(P(I).GT.P(ICB))THEN |
---|
979 | MP(I)=MP(ICB)*(P(1)-P(I))/(P(1)-P(ICB)) |
---|
980 | END IF |
---|
981 | 360 CONTINUE |
---|
982 | C |
---|
983 | C *** FIND MIXING RATIO OF PRECIPITATING DOWNDRAFT *** |
---|
984 | C |
---|
985 | IF(I.EQ.INB)GOTO 400 |
---|
986 | RP(I)=RR(I) |
---|
987 | IF(MP(I).GT.MP(I+1))THEN |
---|
988 | RP(I)=RP(I+1)*MP(I+1)+RR(I)*(MP(I)-MP(I+1))+ |
---|
989 | 1 5.*SIGD*(PH(I)-PH(I+1))*(EVAP(I+1)+EVAP(I)) |
---|
990 | RP(I)=RP(I)/MP(I) |
---|
991 | UP(I)=UP(I+1)*MP(I+1)+U(I)*(MP(I)-MP(I+1)) |
---|
992 | UP(I)=UP(I)/MP(I) |
---|
993 | VP(I)=VP(I+1)*MP(I+1)+V(I)*(MP(I)-MP(I+1)) |
---|
994 | VP(I)=VP(I)/MP(I) |
---|
995 | DO J=1,NTRA |
---|
996 | TRAP(I,J)=TRAP(I+1,J)*MP(I+1)+ |
---|
997 | s TRAP(I,J)*(MP(I)-MP(I+1)) |
---|
998 | TRAP(I,J)=TRAP(I,J)/MP(I) |
---|
999 | END DO |
---|
1000 | ELSE |
---|
1001 | IF(MP(I+1).GT.1.0E-16)THEN |
---|
1002 | RP(I)=RP(I+1)+5.0*SIGD*(PH(I)-PH(I+1))*(EVAP(I+1)+ |
---|
1003 | 1 EVAP(I))/MP(I+1) |
---|
1004 | UP(I)=UP(I+1) |
---|
1005 | VP(I)=VP(I+1) |
---|
1006 | DO J=1,NTRA |
---|
1007 | TRAP(I,J)=TRAP(I+1,J) |
---|
1008 | END DO |
---|
1009 | END IF |
---|
1010 | END IF |
---|
1011 | RP(I)=AMIN1(RP(I),RS(I)) |
---|
1012 | RP(I)=AMAX1(RP(I),0.0) |
---|
1013 | 400 CONTINUE |
---|
1014 | C |
---|
1015 | C *** CALCULATE SURFACE PRECIPITATION IN MM/DAY *** |
---|
1016 | C |
---|
1017 | PRECIP=WT(1)*SIGD*WATER(1)*8640.0 |
---|
1018 | |
---|
1019 | c sb *** Calculate downdraft velocity scale and surface temperature and *** |
---|
1020 | c sb *** water vapor fluctuations *** |
---|
1021 | c sb (inspire de convect 4.3) |
---|
1022 | |
---|
1023 | c BETAD=10.0 |
---|
1024 | BETAD=5.0 |
---|
1025 | WD=BETAD*ABS(MP(ICB))*0.01*RD*T(ICB)/(SIGD*P(ICB)) |
---|
1026 | |
---|
1027 | 405 CONTINUE |
---|
1028 | C |
---|
1029 | C *** CALCULATE TENDENCIES OF LOWEST LEVEL POTENTIAL TEMPERATURE *** |
---|
1030 | C *** AND MIXING RATIO *** |
---|
1031 | C |
---|
1032 | DPINV=1.0/(PH(1)-PH(2)) |
---|
1033 | AM=0.0 |
---|
1034 | DO 410 K=2,INB |
---|
1035 | 410 AM=AM+M(K) |
---|
1036 | IF((0.1*DPINV*AM).GE.DELTI)IFLAG=4 |
---|
1037 | FT(1)=0.1*DPINV*AM*(T(2)-T(1)+(GZ(2)-GZ(1))/CPN(1)) |
---|
1038 | FT(1)=FT(1)-0.5*LVCP(1)*SIGD*(EVAP(1)+EVAP(2)) |
---|
1039 | FT(1)=FT(1)-0.09*SIGD*MP(2)*T(1)*B(1)*DPINV |
---|
1040 | FT(1)=FT(1)+0.01*SIGD*WT(1)*(CL-CPD)*WATER(2)*(T(2)- |
---|
1041 | 1 T(1))*DPINV/CPN(1) |
---|
1042 | FR(1)=0.1*MP(2)*(RP(2)-RR(1))* |
---|
1043 | 1 DPINV+SIGD*0.5*(EVAP(1)+EVAP(2)) |
---|
1044 | FR(1)=FR(1)+0.1*AM*(RR(2)-RR(1))*DPINV |
---|
1045 | FU(1)=FU(1)+0.1*DPINV*(MP(2)*(UP(2)-U(1))+AM*(U(2)-U(1))) |
---|
1046 | FV(1)=FV(1)+0.1*DPINV*(MP(2)*(VP(2)-V(1))+AM*(V(2)-V(1))) |
---|
1047 | DO J=1,NTRA |
---|
1048 | FTRA(1,J)=FTRA(1,J)+0.1*DPINV*(MP(2)*(TRAP(2,J)-TRA(1,J))+ |
---|
1049 | 1 AM*(TRA(2,J)-TRA(1,J))) |
---|
1050 | END DO |
---|
1051 | AMDE=0.0 |
---|
1052 | DO 415 J=2,INB |
---|
1053 | FR(1)=FR(1)+0.1*DPINV*MENT(J,1)*(QENT(J,1)-RR(1)) |
---|
1054 | FU(1)=FU(1)+0.1*DPINV*MENT(J,1)*(UENT(J,1)-U(1)) |
---|
1055 | FV(1)=FV(1)+0.1*DPINV*MENT(J,1)*(VENT(J,1)-V(1)) |
---|
1056 | DO K=1,NTRA |
---|
1057 | FTRA(1,K)=FTRA(1,K)+0.1*DPINV*MENT(J,1)*(TRAENT(J,1,K)- |
---|
1058 | 1 TRA(1,K)) |
---|
1059 | END DO |
---|
1060 | 415 CONTINUE |
---|
1061 | C |
---|
1062 | C *** CALCULATE TENDENCIES OF POTENTIAL TEMPERATURE AND MIXING RATIO *** |
---|
1063 | C *** AT LEVELS ABOVE THE LOWEST LEVEL *** |
---|
1064 | C |
---|
1065 | C *** FIRST FIND THE NET SATURATED UPDRAFT AND DOWNDRAFT MASS FLUXES *** |
---|
1066 | C *** THROUGH EACH LEVEL *** |
---|
1067 | C |
---|
1068 | |
---|
1069 | |
---|
1070 | DO 500 I=2,INB |
---|
1071 | DPINV=1.0/(PH(I)-PH(I+1)) |
---|
1072 | CPINV=1.0/CPN(I) |
---|
1073 | AMP1=0.0 |
---|
1074 | DO 440 K=I+1,INB+1 |
---|
1075 | 440 AMP1=AMP1+M(K) |
---|
1076 | DO 450 K=1,I |
---|
1077 | DO 450 J=I+1,INB+1 |
---|
1078 | AMP1=AMP1+MENT(K,J) |
---|
1079 | 450 CONTINUE |
---|
1080 | IF((0.1*DPINV*AMP1).GE.DELTI)IFLAG=4 |
---|
1081 | AD=0.0 |
---|
1082 | DO 470 K=1,I-1 |
---|
1083 | DO 470 J=I,INB |
---|
1084 | 470 AD=AD+MENT(J,K) |
---|
1085 | FT(I)=0.1*DPINV*(AMP1*(T(I+1)-T(I)+(GZ(I+1)-GZ(I))* |
---|
1086 | 1 CPINV)-AD*(T(I)-T(I-1)+(GZ(I)-GZ(I-1))*CPINV)) |
---|
1087 | 2 -0.5*SIGD*LVCP(I)*(EVAP(I)+EVAP(I+1)) |
---|
1088 | RAT=CPN(I-1)*CPINV |
---|
1089 | FT(I)=FT(I)-0.09*SIGD*(MP(I+1)*T(I)* |
---|
1090 | 1 B(I)-MP(I)*T(I-1)*RAT*B(I-1))*DPINV |
---|
1091 | FT(I)=FT(I)+0.1*DPINV*MENT(I,I)*(HP(I)-H(I)+ |
---|
1092 | 1 T(I)*(CPV-CPD)*(RR(I)-QENT(I,I)))*CPINV |
---|
1093 | FT(I)=FT(I)+0.01*SIGD*WT(I)*(CL-CPD)*WATER(I+1)* |
---|
1094 | 1 (T(I+1)-T(I))*DPINV*CPINV |
---|
1095 | FR(I)=0.1*DPINV*(AMP1*(RR(I+1)-RR(I))- |
---|
1096 | 1 AD*(RR(I)-RR(I-1))) |
---|
1097 | FU(I)=FU(I)+0.1*DPINV*(AMP1*(U(I+1)-U(I))- |
---|
1098 | 1 AD*(U(I)-U(I-1))) |
---|
1099 | FV(I)=FV(I)+0.1*DPINV*(AMP1*(V(I+1)-V(I))- |
---|
1100 | 1 AD*(V(I)-V(I-1))) |
---|
1101 | DO K=1,NTRA |
---|
1102 | FTRA(I,K)=FTRA(I,K)+0.1*DPINV*(AMP1*(TRA(I+1,K)- |
---|
1103 | 1 TRA(I,K))-AD*(TRA(I,K)-TRA(I-1,K))) |
---|
1104 | END DO |
---|
1105 | DO 480 K=1,I-1 |
---|
1106 | AWAT=ELIJ(K,I)-(1.-EP(I))*CLW(I) |
---|
1107 | AWAT=AMAX1(AWAT,0.0) |
---|
1108 | FR(I)=FR(I)+0.1*DPINV*MENT(K,I)*(QENT(K,I)-AWAT |
---|
1109 | 1 -RR(I)) |
---|
1110 | FU(I)=FU(I)+0.1*DPINV*MENT(K,I)*(UENT(K,I)-U(I)) |
---|
1111 | FV(I)=FV(I)+0.1*DPINV*MENT(K,I)*(VENT(K,I)-V(I)) |
---|
1112 | C (saturated updrafts resulting from mixing) ! cld |
---|
1113 | QCOND(I)=QCOND(I)+(ELIJ(K,I)-AWAT) ! cld |
---|
1114 | NQCOND(I)=NQCOND(I)+1. ! cld |
---|
1115 | DO J=1,NTRA |
---|
1116 | FTRA(I,J)=FTRA(I,J)+0.1*DPINV*MENT(K,I)*(TRAENT(K,I,J)- |
---|
1117 | 1 TRA(I,J)) |
---|
1118 | END DO |
---|
1119 | 480 CONTINUE |
---|
1120 | DO 490 K=I,INB |
---|
1121 | FR(I)=FR(I)+0.1*DPINV*MENT(K,I)*(QENT(K,I)-RR(I)) |
---|
1122 | FU(I)=FU(I)+0.1*DPINV*MENT(K,I)*(UENT(K,I)-U(I)) |
---|
1123 | FV(I)=FV(I)+0.1*DPINV*MENT(K,I)*(VENT(K,I)-V(I)) |
---|
1124 | DO J=1,NTRA |
---|
1125 | FTRA(I,J)=FTRA(I,J)+0.1*DPINV*MENT(K,I)*(TRAENT(K,I,J)- |
---|
1126 | 1 TRA(I,J)) |
---|
1127 | END DO |
---|
1128 | 490 CONTINUE |
---|
1129 | FR(I)=FR(I)+0.5*SIGD*(EVAP(I)+EVAP(I+1))+0.1*(MP(I+1)* |
---|
1130 | 1 (RP(I+1)-RR(I))-MP(I)*(RP(I)-RR(I-1)))*DPINV |
---|
1131 | FU(I)=FU(I)+0.1*(MP(I+1)*(UP(I+1)-U(I))-MP(I)* |
---|
1132 | 1 (UP(I)-U(I-1)))*DPINV |
---|
1133 | FV(I)=FV(I)+0.1*(MP(I+1)*(VP(I+1)-V(I))-MP(I)* |
---|
1134 | 1 (VP(I)-V(I-1)))*DPINV |
---|
1135 | DO J=1,NTRA |
---|
1136 | FTRA(I,J)=FTRA(I,J)+0.1*DPINV*(MP(I+1)*(TRAP(I+1,J)-TRA(I,J))- |
---|
1137 | 1 MP(I)*(TRAP(I,J)-TRAP(I-1,J))) |
---|
1138 | END DO |
---|
1139 | C (saturated downdrafts resulting from mixing) ! cld |
---|
1140 | DO K=I+1,INB ! cld |
---|
1141 | QCOND(I)=QCOND(I)+ELIJ(K,I) ! cld |
---|
1142 | NQCOND(I)=NQCOND(I)+1. ! cld |
---|
1143 | ENDDO ! cld |
---|
1144 | C (particular case: no detraining level is found) ! cld |
---|
1145 | IF (NENT(I).EQ.0) THEN ! cld |
---|
1146 | QCOND(I)=QCOND(I)+(1-EP(I))*CLW(I) ! cld |
---|
1147 | NQCOND(I)=NQCOND(I)+1. ! cld |
---|
1148 | ENDIF ! cld |
---|
1149 | IF (NQCOND(I).NE.0.) THEN ! cld |
---|
1150 | QCOND(I)=QCOND(I)/NQCOND(I) ! cld |
---|
1151 | ENDIF ! cld |
---|
1152 | 500 CONTINUE |
---|
1153 | |
---|
1154 | |
---|
1155 | |
---|
1156 | C |
---|
1157 | C *** MOVE THE DETRAINMENT AT LEVEL INB DOWN TO LEVEL INB-1 *** |
---|
1158 | C *** IN SUCH A WAY AS TO PRESERVE THE VERTICALLY *** |
---|
1159 | C *** INTEGRATED ENTHALPY AND WATER TENDENCIES *** |
---|
1160 | C |
---|
1161 | c test sb: |
---|
1162 | c@ write(*,*) '--------------------------------------------' |
---|
1163 | c@ write(*,*) 'inb,ft,hp,h,t,rr,qent,ment,water,waterp,wt,mp,b' |
---|
1164 | c@ write(*,*) inb,ft(inb),hp(inb),h(inb) |
---|
1165 | c@ : ,t(inb),rr(inb),qent(inb,inb) |
---|
1166 | c@ : ,ment(inb,inb),water(inb) |
---|
1167 | c@ : ,water(inb+1),wt(inb),mp(inb),b(inb) |
---|
1168 | c@ write(*,*) '--------------------------------------------' |
---|
1169 | c fin test sb: |
---|
1170 | |
---|
1171 | AX=0.1*MENT(INB,INB)*(HP(INB)-H(INB)+T(INB)* |
---|
1172 | 1 (CPV-CPD)*(RR(INB)-QENT(INB,INB)))/(CPN(INB)* |
---|
1173 | 2 (PH(INB)-PH(INB+1))) |
---|
1174 | FT(INB)=FT(INB)-AX |
---|
1175 | FT(INB-1)=FT(INB-1)+AX*CPN(INB)*(PH(INB)-PH(INB+1))/ |
---|
1176 | 1 (CPN(INB-1)*(PH(INB-1)-PH(INB))) |
---|
1177 | BX=0.1*MENT(INB,INB)*(QENT(INB,INB)-RR(INB))/ |
---|
1178 | 1 (PH(INB)-PH(INB+1)) |
---|
1179 | FR(INB)=FR(INB)-BX |
---|
1180 | FR(INB-1)=FR(INB-1)+BX*(PH(INB)-PH(INB+1))/ |
---|
1181 | 1 (PH(INB-1)-PH(INB)) |
---|
1182 | CX=0.1*MENT(INB,INB)*(UENT(INB,INB)-U(INB))/ |
---|
1183 | 1 (PH(INB)-PH(INB+1)) |
---|
1184 | FU(INB)=FU(INB)-CX |
---|
1185 | FU(INB-1)=FU(INB-1)+CX*(PH(INB)-PH(INB+1))/ |
---|
1186 | 1 (PH(INB-1)-PH(INB)) |
---|
1187 | DX=0.1*MENT(INB,INB)*(VENT(INB,INB)-V(INB))/ |
---|
1188 | 1 (PH(INB)-PH(INB+1)) |
---|
1189 | FV(INB)=FV(INB)-DX |
---|
1190 | FV(INB-1)=FV(INB-1)+DX*(PH(INB)-PH(INB+1))/ |
---|
1191 | 1 (PH(INB-1)-PH(INB)) |
---|
1192 | DO J=1,NTRA |
---|
1193 | EX=0.1*MENT(INB,INB)*(TRAENT(INB,INB,J) |
---|
1194 | 1 -TRA(INB,J))/(PH(INB)-PH(INB+1)) |
---|
1195 | FTRA(INB,J)=FTRA(INB,J)-EX |
---|
1196 | FTRA(INB-1,J)=FTRA(INB-1,J)+EX* |
---|
1197 | 1 (PH(INB)-PH(INB+1))/(PH(INB-1)-PH(INB)) |
---|
1198 | ENDDO |
---|
1199 | C |
---|
1200 | C *** HOMOGINIZE TENDENCIES BELOW CLOUD BASE *** |
---|
1201 | C |
---|
1202 | ASUM=0.0 |
---|
1203 | BSUM=0.0 |
---|
1204 | CSUM=0.0 |
---|
1205 | DSUM=0.0 |
---|
1206 | DO 650 I=1,ICB-1 |
---|
1207 | ASUM=ASUM+FT(I)*(PH(I)-PH(I+1)) |
---|
1208 | BSUM=BSUM+FR(I)*(LV(I)+(CL-CPD)*(T(I)-T(1)))* |
---|
1209 | 1 (PH(I)-PH(I+1)) |
---|
1210 | CSUM=CSUM+(LV(I)+(CL-CPD)*(T(I)-T(1)))*(PH(I)-PH(I+1)) |
---|
1211 | DSUM=DSUM+T(I)*(PH(I)-PH(I+1))/TH(I) |
---|
1212 | 650 CONTINUE |
---|
1213 | DO 700 I=1,ICB-1 |
---|
1214 | FT(I)=ASUM*T(I)/(TH(I)*DSUM) |
---|
1215 | FR(I)=BSUM/CSUM |
---|
1216 | 700 CONTINUE |
---|
1217 | C |
---|
1218 | C *** RESET COUNTER AND RETURN *** |
---|
1219 | C |
---|
1220 | SIG(ND)=2.0 |
---|
1221 | c |
---|
1222 | c |
---|
1223 | do i = 1, nd |
---|
1224 | upwd(i) = 0.0 |
---|
1225 | dnwd(i) = 0.0 |
---|
1226 | c sb dnwd0(i) = - mp(i) |
---|
1227 | enddo |
---|
1228 | c |
---|
1229 | do i = 1, nl |
---|
1230 | dnwd0(i) = - mp(i) |
---|
1231 | enddo |
---|
1232 | do i = nl+1, nd |
---|
1233 | dnwd0(i) = 0. |
---|
1234 | enddo |
---|
1235 | c |
---|
1236 | do i = icb, inb |
---|
1237 | upwd(i) = 0.0 |
---|
1238 | dnwd(i) = 0.0 |
---|
1239 | |
---|
1240 | do k =i, inb |
---|
1241 | up1=0.0 |
---|
1242 | dn1=0.0 |
---|
1243 | do n = 1, i-1 |
---|
1244 | up1 = up1 + ment(n,k) |
---|
1245 | dn1 = dn1 - ment(k,n) |
---|
1246 | enddo |
---|
1247 | upwd(i) = upwd(i)+ m(k) + up1 |
---|
1248 | dnwd(i) = dnwd(i) + dn1 |
---|
1249 | enddo |
---|
1250 | enddo |
---|
1251 | |
---|
1252 | cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
---|
1253 | c DETERMINATION DE LA VARIATION DE FLUX ASCENDANT ENTRE |
---|
1254 | C DEUX NIVEAU NON DILUE Mike |
---|
1255 | cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
---|
1256 | |
---|
1257 | |
---|
1258 | c sb do i=1,ND |
---|
1259 | c sb Mike(i)=M(i) |
---|
1260 | c sb enddo |
---|
1261 | |
---|
1262 | do i = 1, NL |
---|
1263 | Mike(i) = M(i) |
---|
1264 | enddo |
---|
1265 | do i = NL+1, ND |
---|
1266 | Mike(i) = 0. |
---|
1267 | enddo |
---|
1268 | |
---|
1269 | do i=1,nd |
---|
1270 | Ma(i)=0 |
---|
1271 | enddo |
---|
1272 | |
---|
1273 | c sb do i=1,nd |
---|
1274 | c sb do j=i,nd |
---|
1275 | c sb Ma(i)=Ma(i)+M(j) |
---|
1276 | c sb enddo |
---|
1277 | c sb enddo |
---|
1278 | |
---|
1279 | do i = 1, NL |
---|
1280 | do j = i, NL |
---|
1281 | Ma(i) = Ma(i) + M(j) |
---|
1282 | enddo |
---|
1283 | enddo |
---|
1284 | c |
---|
1285 | do i = NL+1, ND |
---|
1286 | Ma(i) = 0. |
---|
1287 | enddo |
---|
1288 | c |
---|
1289 | do i=1,ICB-1 |
---|
1290 | Ma(i)=0 |
---|
1291 | enddo |
---|
1292 | |
---|
1293 | |
---|
1294 | |
---|
1295 | ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
---|
1296 | C ICB REPRESENTE DE NIVEAU OU SE TROUVE LA |
---|
1297 | c BASE DU NUAGE , ET INB LE TOP DU NUAGE |
---|
1298 | cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
---|
1299 | |
---|
1300 | |
---|
1301 | do i=1,ND |
---|
1302 | Mke(i)=upwd(i)+dnwd(i) |
---|
1303 | enddo |
---|
1304 | |
---|
1305 | C |
---|
1306 | C *** Diagnose the in-cloud mixing ratio *** ! cld |
---|
1307 | C *** of condensed water *** ! cld |
---|
1308 | C ! cld |
---|
1309 | DO I=1,ND ! cld |
---|
1310 | MAA(I)=0.0 ! cld |
---|
1311 | WA(I)=0.0 ! cld |
---|
1312 | SIGA(I)=0.0 ! cld |
---|
1313 | ENDDO ! cld |
---|
1314 | DO I=NK,INB ! cld |
---|
1315 | DO K=I+1,INB+1 ! cld |
---|
1316 | MAA(I)=MAA(I)+M(K) ! cld |
---|
1317 | ENDDO ! cld |
---|
1318 | ENDDO ! cld |
---|
1319 | DO I=ICB,INB-1 ! cld |
---|
1320 | AXC(I)=0. ! cld |
---|
1321 | DO J=ICB,I ! cld |
---|
1322 | AXC(I)=AXC(I)+RD*(TVP(J)-TV(J))*(PH(J)-PH(J+1))/P(J) ! cld |
---|
1323 | ENDDO ! cld |
---|
1324 | IF (AXC(I).GT.0.0) THEN ! cld |
---|
1325 | WA(I)=SQRT(2.*AXC(I)) ! cld |
---|
1326 | ENDIF ! cld |
---|
1327 | ENDDO ! cld |
---|
1328 | DO I=1,NL ! cld |
---|
1329 | IF (WA(I).GT.0.0) ! cld |
---|
1330 | 1 SIGA(I)=MAA(I)/WA(I)*RD*TVP(I)/P(I)/100./DELTAC ! cld |
---|
1331 | SIGA(I) = MIN(SIGA(I),1.0) ! cld |
---|
1332 | QCONDC(I)=SIGA(I)*CLW(I)*(1.-EP(I)) ! cld |
---|
1333 | 1 + (1.-SIGA(I))*QCOND(I) ! cld |
---|
1334 | ENDDO ! cld |
---|
1335 | |
---|
1336 | |
---|
1337 | c$$$cccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
---|
1338 | c$$$ call writeg1d(1,klev,ma,'ma ','ma ') |
---|
1339 | c$$$ call writeg1d(1,klev,upwd,'upwd ','upwd ') |
---|
1340 | c$$$ call writeg1d(1,klev,dnwd,'dnwd ','dnwd ') |
---|
1341 | c$$$ call writeg1d(1,klev,dnwd0,'dnwd0 ','dnwd0 ') |
---|
1342 | c$$$ call writeg1d(1,klev,tvp,'tvp ','tvp ') |
---|
1343 | c$$$ call writeg1d(1,klev,tra(1:klev,3),'tra3 ','tra3 ') |
---|
1344 | c$$$ call writeg1d(1,klev,tra(1:klev,4),'tra4 ','tra4 ') |
---|
1345 | c$$$ call writeg1d(1,klev,tra(1:klev,5),'tra5 ','tra5 ') |
---|
1346 | c$$$ call writeg1d(1,klev,tra(1:klev,6),'tra6 ','tra6 ') |
---|
1347 | c$$$ call writeg1d(1,klev,tra(1:klev,7),'tra7 ','tra7 ') |
---|
1348 | c$$$ call writeg1d(1,klev,tra(1:klev,8),'tra8 ','tra8 ') |
---|
1349 | c$$$ call writeg1d(1,klev,tra(1:klev,9),'tra9 ','tra9 ') |
---|
1350 | c$$$ call writeg1d(1,klev,tra(1:klev,10),'tra10','tra10') |
---|
1351 | c$$$ call writeg1d(1,klev,tra(1:klev,11),'tra11','tra11') |
---|
1352 | c$$$ call writeg1d(1,klev,tra(1:klev,12),'tra12','tra12') |
---|
1353 | c$$$ call writeg1d(1,klev,tra(1:klev,13),'tra13','tra13') |
---|
1354 | c$$$ call writeg1d(1,klev,tra(1:klev,14),'tra14','tra14') |
---|
1355 | c$$$ call writeg1d(1,klev,tra(1:klev,15),'tra15','tra15') |
---|
1356 | c$$$ call writeg1d(1,klev,tra(1:klev,16),'tra16','tra16') |
---|
1357 | c$$$ call writeg1d(1,klev,tra(1:klev,17),'tra17','tra17') |
---|
1358 | c$$$ call writeg1d(1,klev,tra(1:klev,18),'tra18','tra18') |
---|
1359 | c$$$ call writeg1d(1,klev,tra(1:klev,19),'tra19','tra19') |
---|
1360 | c$$$ call writeg1d(1,klev,tra(1:klev,20),'tra20','tra20 ') |
---|
1361 | c$$$ call writeg1d(1,klev,trap(1:klev,1),'trp1','trp1') |
---|
1362 | c$$$ call writeg1d(1,klev,trap(1:klev,2),'trp2','trp2') |
---|
1363 | c$$$ call writeg1d(1,klev,trap(1:klev,3),'trp3','trp3') |
---|
1364 | c$$$ call writeg1d(1,klev,trap(1:klev,4),'trp4','trp4') |
---|
1365 | c$$$ call writeg1d(1,klev,trap(1:klev,5),'trp5','trp5') |
---|
1366 | c$$$ call writeg1d(1,klev,trap(1:klev,10),'trp10','trp10') |
---|
1367 | c$$$ call writeg1d(1,klev,trap(1:klev,12),'trp12','trp12') |
---|
1368 | c$$$ call writeg1d(1,klev,trap(1:klev,15),'trp15','trp15') |
---|
1369 | c$$$ call writeg1d(1,klev,trap(1:klev,20),'trp20','trp20') |
---|
1370 | c$$$ call writeg1d(1,klev,ftra(1:klev,1),'ftr1 ','ftr1 ') |
---|
1371 | c$$$ call writeg1d(1,klev,ftra(1:klev,2),'ftr2 ','ftr2 ') |
---|
1372 | c$$$ call writeg1d(1,klev,ftra(1:klev,3),'ftr3 ','ftr3 ') |
---|
1373 | c$$$ call writeg1d(1,klev,ftra(1:klev,4),'ftr4 ','ftr4 ') |
---|
1374 | c$$$ call writeg1d(1,klev,ftra(1:klev,5),'ftr5 ','ftr5 ') |
---|
1375 | c$$$ call writeg1d(1,klev,ftra(1:klev,6),'ftr6 ','ftr6 ') |
---|
1376 | c$$$ call writeg1d(1,klev,ftra(1:klev,7),'ftr7 ','ftr7 ') |
---|
1377 | c$$$ call writeg1d(1,klev,ftra(1:klev,8),'ftr8 ','ftr8 ') |
---|
1378 | c$$$ call writeg1d(1,klev,ftra(1:klev,9),'ftr9 ','ftr9 ') |
---|
1379 | c$$$ call writeg1d(1,klev,ftra(1:klev,10),'ftr10','ftr10') |
---|
1380 | c$$$ call writeg1d(1,klev,ftra(1:klev,11),'ftr11','ftr11') |
---|
1381 | c$$$ call writeg1d(1,klev,ftra(1:klev,12),'ftr12','ftr12') |
---|
1382 | c$$$ call writeg1d(1,klev,ftra(1:klev,13),'ftr13','ftr13') |
---|
1383 | c$$$ call writeg1d(1,klev,ftra(1:klev,14),'ftr14','ftr14') |
---|
1384 | c$$$ call writeg1d(1,klev,ftra(1:klev,15),'ftr15','ftr15') |
---|
1385 | c$$$ call writeg1d(1,klev,ftra(1:klev,16),'ftr16','ftr16') |
---|
1386 | c$$$ call writeg1d(1,klev,ftra(1:klev,17),'ftr17','ftr17') |
---|
1387 | c$$$ call writeg1d(1,klev,ftra(1:klev,18),'ftr18','ftr18') |
---|
1388 | c$$$ call writeg1d(1,klev,ftra(1:klev,19),'ftr19','ftr19') |
---|
1389 | c$$$ call writeg1d(1,klev,ftra(1:klev,20),'ftr20','ftr20 ') |
---|
1390 | c$$$ call writeg1d(1,klev,mp,'mp ','mp ') |
---|
1391 | c$$$ call writeg1d(1,klev,Mke,'Mke ','Mke ') |
---|
1392 | |
---|
1393 | |
---|
1394 | |
---|
1395 | ccccccccccccccccccccccccccccccccccccccccccccccccccccccccccccc |
---|
1396 | c |
---|
1397 | c |
---|
1398 | RETURN |
---|
1399 | END |
---|
1400 | C --------------------------------------------------------------------------- |
---|