1 | |
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2 | C SUBROUTINE DE PARAMETRISATION DES MONTAGNES D ECHELLE SOUS MAILLE |
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3 | |
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4 | SUBROUTINE drag_noro (nlon,nlev,dtime,paprs,pplay,pgeop,pn2, |
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5 | e pmea,pstd, psig, pgam, pthe,ppic,pval, |
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6 | e kgwd,kdx,ktest, |
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7 | e t, u, v, |
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8 | s pulow, pvlow, pustr, pvstr, |
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9 | s d_t, d_u, d_v) |
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10 | c |
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11 | use dimphy |
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12 | IMPLICIT none |
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13 | |
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14 | #include "dimensions.h" |
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15 | #include "paramet.h" |
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16 | |
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17 | c====================================================================== |
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18 | c Auteur(s): F.Lott (LMD/CNRS) date: 19950201 |
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19 | c Object: Mountain drag interface. Made necessary because: |
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20 | C 1. in the LMD-GCM Layers are from bottom to top, |
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21 | C contrary to most European GCM. |
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22 | c 2. the altitude above ground of each model layers |
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23 | c needs to be known (variable zgeom) |
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24 | c====================================================================== |
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25 | c Explicit Arguments: |
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26 | c ================== |
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27 | c nlon----input-I-Total number of horizontal points that get into physics |
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28 | c nlev----input-I-Number of vertical levels |
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29 | c dtime---input-R-Time-step (s) |
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30 | c paprs---input-R-Pressure in semi layers (Pa) |
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31 | c pplay---input-R-Pressure model-layers (Pa) |
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32 | c pgeop---input-R-Geopotential model layers (reference ground) |
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33 | c pn2-----input-R-Brunt-Vaisala freq.^2 at 1/2 layers |
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34 | c t-------input-R-temperature (K) |
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35 | c u-------input-R-Horizontal wind (m/s) |
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36 | c v-------input-R-Meridional wind (m/s) |
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37 | c pmea----input-R-Mean Orography (m) |
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38 | C pstd----input-R-SSO standard deviation (m) |
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39 | c psig----input-R-SSO slope |
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40 | c pgam----input-R-SSO Anisotropy |
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41 | c pthe----input-R-SSO Angle |
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42 | c ppic----input-R-SSO Peacks elevation (m) |
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43 | c pval----input-R-SSO Valleys elevation (m) |
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44 | c |
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45 | c kgwd- -input-I: Total nb of points where the orography schemes are active |
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46 | c ktest--input-I: Flags to indicate active points |
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47 | c kdx----input-I: Locate the physical location of an active point. |
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48 | |
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49 | c pulow, pvlow -output-R: Low-level wind |
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50 | c pustr, pvstr -output-R: Surface stress due to SSO drag (Pa) |
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51 | c |
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52 | c d_t-----output-R: T increment |
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53 | c d_u-----output-R: U increment |
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54 | c d_v-----output-R: V increment |
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55 | c |
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56 | c Implicit Arguments: |
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57 | c =================== |
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58 | c |
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59 | c iim--common-I: Number of longitude intervals |
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60 | c jjm--common-I: Number of latitude intervals |
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61 | c klon-common-I: Number of points seen by the physics |
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62 | c (iim+1)*(jjm+1) for instance |
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63 | c klev-common-I: Number of vertical layers |
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64 | c====================================================================== |
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65 | c Local Variables: |
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66 | c ================ |
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67 | c |
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68 | c zgeom-----R: Altitude (m) of layer above ground (from top to bottom) |
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69 | c pt, pu, pv --R: t u v from top to bottom |
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70 | c pdtdt, pdudt, pdvdt --R: t u v tendencies (from top to bottom) |
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71 | c papmf: pressure at model layer (from top to bottom) |
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72 | c papmh: pressure at model 1/2 layer (from top to bottom) |
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73 | c |
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74 | c====================================================================== |
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75 | |
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76 | #include "YOMCST.h" |
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77 | #include "YOEGWD.h" |
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78 | |
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79 | c ARGUMENTS |
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80 | c |
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81 | INTEGER nlon,nlev |
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82 | REAL dtime |
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83 | REAL paprs(nlon,nlev+1) |
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84 | REAL pplay(nlon,nlev) |
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85 | REAL pgeop(nlon,nlev),pn2(nlon,nlev) |
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86 | REAL pmea(nlon),pstd(nlon),psig(nlon),pgam(nlon),pthe(nlon) |
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87 | REAL ppic(nlon),pval(nlon) |
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88 | REAL pulow(nlon),pvlow(nlon),pustr(nlon),pvstr(nlon) |
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89 | REAL t(nlon,nlev), u(nlon,nlev), v(nlon,nlev) |
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90 | REAL d_t(nlon,nlev), d_u(nlon,nlev), d_v(nlon,nlev) |
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91 | c |
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92 | INTEGER i, k, kgwd, kdx(nlon), ktest(nlon) |
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93 | c |
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94 | c LOCAL VARIABLES: |
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95 | c |
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96 | REAL zgeom(klon,klev),zn2(klon,klev) |
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97 | REAL pdtdt(klon,klev), pdudt(klon,klev), pdvdt(klon,klev) |
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98 | REAL pt(klon,klev), pu(klon,klev), pv(klon,klev) |
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99 | REAL papmf(klon,klev),papmh(klon,klev+1) |
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100 | c |
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101 | c INITIALIZE OUTPUT VARIABLES |
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102 | c |
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103 | DO i = 1,klon |
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104 | pulow(i) = 0.0 |
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105 | pvlow(i) = 0.0 |
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106 | pustr(i) = 0.0 |
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107 | pvstr(i) = 0.0 |
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108 | ENDDO |
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109 | DO k = 1, klev |
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110 | DO i = 1, klon |
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111 | d_t(i,k) = 0.0 |
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112 | d_u(i,k) = 0.0 |
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113 | d_v(i,k) = 0.0 |
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114 | pdudt(i,k)=0.0 |
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115 | pdvdt(i,k)=0.0 |
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116 | pdtdt(i,k)=0.0 |
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117 | ENDDO |
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118 | ENDDO |
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119 | c |
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120 | c PREPARE INPUT VARIABLES FOR ORODRAG (i.e., ORDERED FROM TOP TO BOTTOM) |
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121 | C CALCULATE LAYERS HEIGHT ABOVE GROUND) |
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122 | c |
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123 | DO k = 1, klev |
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124 | DO i = 1, klon |
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125 | pt(i,k) = t(i,klev-k+1) |
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126 | pu(i,k) = u(i,klev-k+1) |
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127 | pv(i,k) = v(i,klev-k+1) |
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128 | papmf(i,k) = pplay(i,klev-k+1) |
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129 | ENDDO |
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130 | ENDDO |
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131 | DO k = 1, klev+1 |
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132 | DO i = 1, klon |
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133 | papmh(i,k) = paprs(i,klev-k+2) |
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134 | ENDDO |
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135 | ENDDO |
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136 | |
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137 | DO k = klev, 1, -1 |
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138 | DO i = 1, klon |
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139 | zgeom(i,k) = pgeop(i,klev-k+1)/RG |
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140 | zn2(i,k) = pn2(i,klev-k+1) |
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141 | ENDDO |
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142 | ENDDO |
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143 | |
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144 | c CALL SSO DRAG ROUTINES |
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145 | c |
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146 | CALL orodrag(klon,klev,kgwd,kdx,ktest, |
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147 | . dtime, |
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148 | . papmh, papmf, zgeom, zn2, |
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149 | . pt, pu, pv, |
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150 | . pmea, pstd, psig, pgam, pthe, ppic,pval, |
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151 | . pulow,pvlow, |
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152 | . pdudt,pdvdt,pdtdt) |
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153 | C |
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154 | C COMPUTE INCREMENTS AND STRESS FROM TENDENCIES |
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155 | |
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156 | DO k = 1, klev |
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157 | DO i = 1, klon |
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158 | d_u(i,klev+1-k) = dtime*pdudt(i,k) |
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159 | d_v(i,klev+1-k) = dtime*pdvdt(i,k) |
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160 | d_t(i,klev+1-k) = dtime*pdtdt(i,k) |
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161 | pustr(i) = pustr(i) |
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162 | . +pdudt(i,k)*(papmh(i,k+1)-papmh(i,k))/rg |
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163 | pvstr(i) = pvstr(i) |
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164 | . +pdvdt(i,k)*(papmh(i,k+1)-papmh(i,k))/rg |
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165 | ENDDO |
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166 | ENDDO |
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167 | c |
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168 | RETURN |
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169 | END |
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170 | |
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