1 | !IDEAL:MODEL_LAYER:INITIALIZATION |
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2 | |
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3 | ! This MODULE holds the routines which are used to perform various initializations |
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4 | ! for the individual domains. |
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5 | |
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6 | !----------------------------------------------------------------------- |
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7 | |
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8 | MODULE module_initialize_ideal |
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9 | |
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10 | USE module_domain ! frame/module_domain.F |
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11 | USE module_io_domain ! share |
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12 | USE module_state_description ! frame |
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13 | USE module_model_constants ! share |
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14 | USE module_bc ! share |
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15 | USE module_timing ! frame |
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16 | USE module_configure ! frame |
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17 | USE module_init_utilities ! dyn_em |
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18 | #ifdef DM_PARALLEL |
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19 | USE module_dm |
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20 | #endif |
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21 | |
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22 | |
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23 | CONTAINS |
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24 | |
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25 | |
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26 | !------------------------------------------------------------------- |
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27 | ! this is a wrapper for the solver-specific init_domain routines. |
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28 | ! Also dereferences the grid variables and passes them down as arguments. |
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29 | ! This is crucial, since the lower level routines may do message passing |
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30 | ! and this will get fouled up on machines that insist on passing down |
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31 | ! copies of assumed-shape arrays (by passing down as arguments, the |
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32 | ! data are treated as assumed-size -- ie. f77 -- arrays and the copying |
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33 | ! business is avoided). Fie on the F90 designers. Fie and a pox. |
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34 | |
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35 | SUBROUTINE init_domain ( grid ) |
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36 | |
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37 | IMPLICIT NONE |
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38 | |
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39 | ! Input data. |
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40 | TYPE (domain), POINTER :: grid |
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41 | ! Local data. |
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42 | INTEGER :: idum1, idum2 |
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43 | |
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44 | CALL set_scalar_indices_from_config ( head_grid%id , idum1, idum2 ) |
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45 | |
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46 | CALL init_domain_rk( grid & |
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47 | ! |
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48 | #include <actual_new_args.inc> |
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49 | ! |
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50 | ) |
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51 | |
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52 | END SUBROUTINE init_domain |
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53 | |
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54 | !------------------------------------------------------------------- |
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55 | |
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56 | SUBROUTINE init_domain_rk ( grid & |
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57 | ! |
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58 | # include <dummy_new_args.inc> |
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59 | ! |
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60 | ) |
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61 | IMPLICIT NONE |
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62 | |
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63 | ! Input data. |
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64 | TYPE (domain), POINTER :: grid |
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65 | |
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66 | # include <dummy_decl.inc> |
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67 | |
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68 | TYPE (grid_config_rec_type) :: config_flags |
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69 | |
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70 | ! Local data |
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71 | INTEGER :: & |
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72 | ids, ide, jds, jde, kds, kde, & |
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73 | ims, ime, jms, jme, kms, kme, & |
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74 | its, ite, jts, jte, kts, kte, & |
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75 | i, j, k |
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76 | |
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77 | INTEGER :: nxx, nyy, ig, jg, im, error |
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78 | |
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79 | REAL :: dlam, dphi, vlat, tperturb |
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80 | REAL :: p_surf, p_level, pd_surf, qvf1, qvf2, qvf |
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81 | REAL :: thtmp, ptmp, temp(3), cof1, cof2 |
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82 | |
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83 | INTEGER :: icm,jcm |
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84 | |
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85 | SELECT CASE ( model_data_order ) |
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86 | CASE ( DATA_ORDER_ZXY ) |
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87 | kds = grid%sd31 ; kde = grid%ed31 ; |
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88 | ids = grid%sd32 ; ide = grid%ed32 ; |
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89 | jds = grid%sd33 ; jde = grid%ed33 ; |
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90 | |
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91 | kms = grid%sm31 ; kme = grid%em31 ; |
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92 | ims = grid%sm32 ; ime = grid%em32 ; |
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93 | jms = grid%sm33 ; jme = grid%em33 ; |
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94 | |
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95 | kts = grid%sp31 ; kte = grid%ep31 ; ! note that tile is entire patch |
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96 | its = grid%sp32 ; ite = grid%ep32 ; ! note that tile is entire patch |
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97 | jts = grid%sp33 ; jte = grid%ep33 ; ! note that tile is entire patch |
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98 | CASE ( DATA_ORDER_XYZ ) |
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99 | ids = grid%sd31 ; ide = grid%ed31 ; |
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100 | jds = grid%sd32 ; jde = grid%ed32 ; |
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101 | kds = grid%sd33 ; kde = grid%ed33 ; |
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102 | |
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103 | ims = grid%sm31 ; ime = grid%em31 ; |
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104 | jms = grid%sm32 ; jme = grid%em32 ; |
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105 | kms = grid%sm33 ; kme = grid%em33 ; |
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106 | |
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107 | its = grid%sp31 ; ite = grid%ep31 ; ! note that tile is entire patch |
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108 | jts = grid%sp32 ; jte = grid%ep32 ; ! note that tile is entire patch |
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109 | kts = grid%sp33 ; kte = grid%ep33 ; ! note that tile is entire patch |
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110 | CASE ( DATA_ORDER_XZY ) |
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111 | ids = grid%sd31 ; ide = grid%ed31 ; |
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112 | kds = grid%sd32 ; kde = grid%ed32 ; |
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113 | jds = grid%sd33 ; jde = grid%ed33 ; |
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114 | |
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115 | ims = grid%sm31 ; ime = grid%em31 ; |
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116 | kms = grid%sm32 ; kme = grid%em32 ; |
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117 | jms = grid%sm33 ; jme = grid%em33 ; |
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118 | |
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119 | its = grid%sp31 ; ite = grid%ep31 ; ! note that tile is entire patch |
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120 | kts = grid%sp32 ; kte = grid%ep32 ; ! note that tile is entire patch |
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121 | jts = grid%sp33 ; jte = grid%ep33 ; ! note that tile is entire patch |
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122 | |
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123 | END SELECT |
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124 | |
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125 | CALL model_to_grid_config_rec ( grid%id , model_config_rec , config_flags ) |
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126 | |
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127 | ! here we check to see if the boundary conditions are set properly |
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128 | |
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129 | CALL boundary_condition_check( config_flags, bdyzone, error, grid%id ) |
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130 | |
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131 | grid%itimestep=0 |
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132 | grid%step_number = 0 |
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133 | |
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134 | |
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135 | #ifdef DM_PARALLEL |
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136 | CALL wrf_dm_bcast_bytes( icm , IWORDSIZE ) |
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137 | CALL wrf_dm_bcast_bytes( jcm , IWORDSIZE ) |
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138 | #endif |
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139 | |
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140 | ! Initialize 2D surface arrays |
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141 | |
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142 | nxx = ide-ids ! Don't include u-stagger |
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143 | nyy = jde-jds ! Don't include v-stagger |
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144 | dphi = 180./REAL(nyy) |
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145 | dlam = 360./REAL(nxx) |
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146 | |
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147 | DO j = jts, jte |
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148 | DO i = its, ite |
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149 | ! ig is the I index in the global (domain) span of the array. |
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150 | ! jg is the J index in the global (domain) span of the array. |
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151 | ig = i - ids + 1 ! ids is not necessarily 1 |
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152 | jg = j - jds + 1 ! jds is not necessarily 1 |
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153 | |
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154 | grid%xlat(i,j) = (REAL(jg)-0.5)*dphi-90. |
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155 | grid%xlong(i,j) = (REAL(ig)-0.5)*dlam-180. |
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156 | vlat = grid%xlat(i,j) - 0.5*dphi |
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157 | |
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158 | grid%clat(i,j) = grid%xlat(i,j) |
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159 | grid%clong(i,j) = grid%xlong(i,j) |
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160 | |
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161 | grid%msftx(i,j) = 1./COS(grid%xlat(i,j)*degrad) |
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162 | grid%msfty(i,j) = 1. |
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163 | grid%msfux(i,j) = 1./COS(grid%xlat(i,j)*degrad) |
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164 | grid%msfuy(i,j) = 1. |
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165 | grid%e(i,j) = 2*EOMEG*COS(grid%xlat(i,j)*degrad) |
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166 | grid%f(i,j) = 2*EOMEG*SIN(grid%xlat(i,j)*degrad) |
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167 | |
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168 | ! The following two are the cosine and sine of the rotation |
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169 | ! of projection. Simple cylindrical is *simple* ... no rotation! |
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170 | grid%sina(i,j) = 0. |
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171 | grid%cosa(i,j) = 1. |
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172 | |
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173 | END DO |
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174 | END DO |
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175 | |
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176 | ! DO j = max(jds+1,jts), min(jde-1,jte) |
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177 | DO j = jts, jte |
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178 | DO i = its, ite |
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179 | vlat = grid%xlat(i,j) - 0.5*dphi |
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180 | grid%msfvx(i,j) = 1./COS(vlat*degrad) |
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181 | grid%msfvy(i,j) = 1. |
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182 | grid%msfvx_inv(i,j) = 1./grid%msfvx(i,j) |
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183 | END DO |
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184 | END DO |
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185 | |
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186 | IF(jts == jds) THEN |
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187 | DO i = its, ite |
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188 | grid%msfvx(i,jts) = 00. |
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189 | grid%msfvx_inv(i,jts) = 0. |
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190 | END DO |
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191 | END IF |
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192 | |
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193 | IF(jte == jde) THEN |
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194 | DO i = its, ite |
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195 | grid%msfvx(i,jte) = 00. |
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196 | grid%msfvx_inv(i,jte) = 0. |
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197 | END DO |
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198 | END IF |
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199 | |
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200 | DO j=jts,jte |
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201 | vlat = grid%xlat(its,j) - 0.5*dphi |
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202 | write(6,*) j,vlat,grid%msfvx(its,j),grid%msfvx_inv(its,j) |
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203 | ENDDO |
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204 | |
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205 | DO j=jts,jte |
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206 | DO i=its,ite |
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207 | grid%ht(i,j) = 0. |
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208 | |
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209 | grid%albedo(i,j) = 0. |
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210 | grid%thc(i,j) = 1000. |
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211 | grid%znt(i,j) = 0.01 |
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212 | grid%emiss(i,j) = 1. |
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213 | grid%ivgtyp(i,j) = 1 |
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214 | grid%lu_index(i,j) = REAL(ivgtyp(i,j)) |
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215 | grid%xland(i,j) = 1. |
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216 | grid%mavail(i,j) = 0. |
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217 | END DO |
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218 | END DO |
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219 | |
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220 | grid%dx = dlam*degrad/reradius |
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221 | grid%dy = dphi*degrad/reradius |
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222 | grid%rdx = 1./grid%dx |
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223 | grid%rdy = 1./grid%dy |
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224 | |
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225 | !WRITE(*,*) '' |
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226 | !WRITE(*,'(A,1PG14.6,A,1PG14.6)') ' For the namelist: dx =',grid%dx,', dy =',grid%dy |
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227 | |
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228 | CALL nl_set_mminlu(1,' ') |
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229 | grid%iswater = 0 |
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230 | grid%cen_lat = 0. |
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231 | grid%cen_lon = 0. |
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232 | grid%truelat1 = 0. |
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233 | grid%truelat2 = 0. |
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234 | grid%moad_cen_lat = 0. |
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235 | grid%stand_lon = 0. |
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236 | grid%pole_lon = 0. |
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237 | grid%pole_lat = 90. |
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238 | ! Apparently, map projection 0 is "none" which actually turns out to be |
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239 | ! a regular grid of latitudes and longitudes, the simple cylindrical projection |
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240 | grid%map_proj = 0 |
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241 | |
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242 | DO k = kds, kde |
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243 | grid%znw(k) = 1. - REAL(k-kds)/REAL(kde-kds) |
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244 | END DO |
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245 | |
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246 | DO k=1, kde-1 |
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247 | grid%dnw(k) = grid%znw(k+1) - grid%znw(k) |
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248 | grid%rdnw(k) = 1./grid%dnw(k) |
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249 | grid%znu(k) = 0.5*(grid%znw(k+1)+grid%znw(k)) |
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250 | ENDDO |
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251 | DO k=2, kde-1 |
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252 | grid%dn(k) = 0.5*(grid%dnw(k)+grid%dnw(k-1)) |
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253 | grid%rdn(k) = 1./grid%dn(k) |
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254 | grid%fnp(k) = .5* grid%dnw(k )/grid%dn(k) |
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255 | grid%fnm(k) = .5* grid%dnw(k-1)/grid%dn(k) |
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256 | ENDDO |
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257 | |
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258 | cof1 = (2.*grid%dn(2)+grid%dn(3))/(grid%dn(2)+grid%dn(3))*grid%dnw(1)/grid%dn(2) |
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259 | cof2 = grid%dn(2) /(grid%dn(2)+grid%dn(3))*grid%dnw(1)/grid%dn(3) |
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260 | grid%cf1 = grid%fnp(2) + cof1 |
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261 | grid%cf2 = grid%fnm(2) - cof1 - cof2 |
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262 | grid%cf3 = cof2 |
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263 | |
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264 | grid%cfn = (.5*grid%dnw(kde-1)+grid%dn(kde-1))/grid%dn(kde-1) |
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265 | grid%cfn1 = -.5*grid%dnw(kde-1)/grid%dn(kde-1) |
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266 | |
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267 | |
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268 | ! Need to add perturbations to initial profile. Set up random number |
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269 | ! seed here. |
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270 | CALL random_seed |
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271 | |
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272 | ! General assumption from here after is that the initial temperature |
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273 | ! profile is isothermal at a value of T0, and the initial winds are |
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274 | ! all 0. |
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275 | |
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276 | ! find ptop for the desired ztop (ztop is input from the namelist) |
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277 | grid%p_top = p0 * EXP(-(g*config_flags%ztop)/(r_d*T0)) |
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278 | |
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279 | |
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280 | ! Values of geopotential (base, perturbation, and at p0) at the surface |
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281 | DO j = jts, jte |
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282 | DO i = its, ite |
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283 | grid%phb(i,1,j) = grid%ht(i,j)*g |
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284 | grid%php(i,1,j) = 0. ! This is perturbation geopotential |
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285 | ! Since this is an initial condition, there |
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286 | ! should be no perturbation! |
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287 | grid%ph0(i,1,j) = grid%ht(i,j)*g |
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288 | ENDDO |
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289 | ENDDO |
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290 | |
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291 | |
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292 | DO J = jts, jte |
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293 | DO I = its, ite |
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294 | |
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295 | p_surf = p0 * EXP(-(g*grid%phb(i,1,j)/g)/(r_d*T0)) |
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296 | grid%mub(i,j) = p_surf-grid%p_top |
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297 | |
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298 | ! given p (coordinate), calculate theta and compute 1/rho from equation |
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299 | ! of state |
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300 | |
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301 | DO K = kts, kte-1 |
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302 | p_level = grid%znu(k)*(p_surf - grid%p_top) + grid%p_top |
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303 | grid%pb(i,k,j) = p_level |
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304 | |
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305 | grid%t_init(i,k,j) = T0*(p0/p_level)**rcp |
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306 | grid%t_init(i,k,j) = grid%t_init(i,k,j) - t0 |
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307 | |
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308 | grid%alb(i,k,j)=(r_d/p1000mb)*(grid%t_init(i,k,j)+t0)*(grid%pb(i,k,j)/p1000mb)**cvpm |
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309 | END DO |
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310 | |
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311 | ! calculate hydrostatic balance (alternatively we could interpolate |
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312 | ! the geopotential from the sounding, but this assures that the base |
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313 | ! state is in exact hydrostatic balance with respect to the model eqns. |
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314 | |
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315 | DO k = kts+1, kte |
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316 | grid%phb(i,k,j) = grid%phb(i,k-1,j) - grid%dnw(k-1)*grid%mub(i,j)*grid%alb(i,k-1,j) |
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317 | ENDDO |
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318 | |
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319 | ENDDO |
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320 | ENDDO |
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321 | |
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322 | DO im = PARAM_FIRST_SCALAR, num_moist |
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323 | DO J = jts, jte |
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324 | DO K = kts, kte-1 |
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325 | DO I = its, ite |
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326 | grid%moist(i,k,j,im) = 0. |
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327 | END DO |
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328 | END DO |
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329 | END DO |
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330 | END DO |
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331 | |
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332 | ! Now calculate the full (hydrostatically-balanced) state for each column |
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333 | ! We will include moisture |
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334 | DO J = jts, jte |
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335 | DO I = its, ite |
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336 | |
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337 | ! At this point p_top is already set. find the DRY mass in the column |
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338 | pd_surf = p0 * EXP(-(g*grid%phb(i,1,j)/g)/(r_d*T0)) |
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339 | |
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340 | ! compute the perturbation mass (mu/mu_1/mu_2) and the full mass |
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341 | grid%mu_1(i,j) = pd_surf-grid%p_top - grid%mub(i,j) |
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342 | grid%mu_2(i,j) = grid%mu_1(i,j) |
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343 | grid%mu0(i,j) = grid%mu_1(i,j) + grid%mub(i,j) |
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344 | |
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345 | ! given the dry pressure and coordinate system, calculate the |
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346 | ! perturbation potential temperature (t/t_1/t_2) |
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347 | |
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348 | DO k = kds, kde-1 |
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349 | p_level = grid%znu(k)*(pd_surf - grid%p_top) + grid%p_top |
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350 | grid%t_1(i,k,j) = T0*(p0/p_level)**rcp |
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351 | ! Add a small perturbation to initial isothermal profile |
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352 | CALL random_number(tperturb) |
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353 | grid%t_1(i,k,j)=grid%t_1(i,k,j)*(1.0+0.004*(tperturb-0.5)) |
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354 | grid%t_1(i,k,j) = grid%t_1(i,k,j)-t0 |
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355 | grid%t_2(i,k,j) = grid%t_1(i,k,j) |
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356 | END DO |
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357 | |
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358 | |
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359 | ! integrate the hydrostatic equation (from the RHS of the bigstep |
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360 | ! vertical momentum equation) down from the top to get p. |
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361 | ! first from the top of the model to the top pressure |
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362 | |
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363 | k = kte-1 ! top level |
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364 | |
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365 | qvf1 = 0.5*(grid%moist(i,k,j,P_QV)+grid%moist(i,k,j,P_QV)) |
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366 | qvf2 = 1./(1.+qvf1) |
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367 | qvf1 = qvf1*qvf2 |
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368 | |
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369 | ! grid%p(i,k,j) = - 0.5*grid%mu_1(i,j)/grid%rdnw(k) |
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370 | grid%p(i,k,j) = - 0.5*(grid%mu_1(i,j)+qvf1*grid%mub(i,j))/grid%rdnw(k)/qvf2 |
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371 | qvf = 1. + rvovrd*grid%moist(i,k,j,P_QV) |
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372 | grid%alt(i,k,j) = (r_d/p1000mb)*(grid%t_1(i,k,j)+t0)*qvf* & |
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373 | (((grid%p(i,k,j)+grid%pb(i,k,j))/p1000mb)**cvpm) |
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374 | grid%al(i,k,j) = grid%alt(i,k,j) - grid%alb(i,k,j) |
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375 | |
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376 | ! down the column |
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377 | |
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378 | do k=kte-2,kts,-1 |
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379 | qvf1 = 0.5*(grid%moist(i,k,j,P_QV)+grid%moist(i,k+1,j,P_QV)) |
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380 | qvf2 = 1./(1.+qvf1) |
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381 | qvf1 = qvf1*qvf2 |
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382 | grid%p(i,k,j) = grid%p(i,k+1,j) - (grid%mu_1(i,j) + qvf1*grid%mub(i,j))/qvf2/grid%rdn(k+1) |
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383 | qvf = 1. + rvovrd*grid%moist(i,k,j,P_QV) |
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384 | grid%alt(i,k,j) = (r_d/p1000mb)*(grid%t_1(i,k,j)+t0)*qvf* & |
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385 | (((grid%p(i,k,j)+grid%pb(i,k,j))/p1000mb)**cvpm) |
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386 | grid%al(i,k,j) = grid%alt(i,k,j) - grid%alb(i,k,j) |
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387 | enddo |
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388 | |
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389 | ! this is the hydrostatic equation used in the model after the |
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390 | ! small timesteps. In the model, al (inverse density) |
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391 | ! is computed from the geopotential. |
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392 | |
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393 | grid%ph_1(i,1,j) = 0. |
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394 | DO k = kts+1,kte |
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395 | grid%ph_1(i,k,j) = grid%ph_1(i,k-1,j) - (1./grid%rdnw(k-1))*( & |
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396 | (grid%mub(i,j)+grid%mu_1(i,j))*grid%al(i,k-1,j)+ & |
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397 | grid%mu_1(i,j)*grid%alb(i,k-1,j) ) |
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398 | |
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399 | grid%ph_2(i,k,j) = grid%ph_1(i,k,j) |
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400 | grid%ph0(i,k,j) = grid%ph_1(i,k,j) + grid%phb(i,k,j) |
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401 | ENDDO |
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402 | |
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403 | END DO |
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404 | END DO |
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405 | |
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406 | |
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407 | |
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408 | ! Now set U & V |
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409 | DO J = jts, jte |
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410 | DO K = kts, kte-1 |
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411 | DO I = its, ite |
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412 | grid%u_1(i,k,j) = 0. |
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413 | grid%u_2(i,k,j) = 0. |
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414 | grid%v_1(i,k,j) = 0. |
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415 | grid%v_2(i,k,j) = 0. |
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416 | END DO |
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417 | END DO |
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418 | END DO |
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419 | |
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420 | |
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421 | DO j=jts, jte |
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422 | DO k=kds, kde |
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423 | DO i=its, ite |
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424 | grid%ww(i,k,j) = 0. |
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425 | grid%w_1(i,k,j) = 0. |
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426 | grid%w_2(i,k,j) = 0. |
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427 | grid%h_diabatic(i,k,j) = 0. |
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428 | END DO |
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429 | END DO |
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430 | END DO |
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431 | |
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432 | |
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433 | DO k=kts,kte |
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434 | grid%t_base(k) = grid%t_init(its,k,jts) |
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435 | grid%qv_base(k) = 0. |
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436 | grid%u_base(k) = 0. |
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437 | grid%v_base(k) = 0. |
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438 | END DO |
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439 | |
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440 | ! One subsurface layer: infinite slab at constant temperature below |
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441 | ! the surface. Surface temperature is an infinitely thin "skin" on |
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442 | ! top of a half-infinite slab. The temperature of both the skin and |
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443 | ! the slab are determined from the initial nearest-surface-air-layer |
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444 | ! temperature. |
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445 | DO J = jts, MIN(jte, jde-1) |
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446 | DO I = its, MIN(ite, ide-1) |
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447 | thtmp = grid%t_2(i,1,j)+t0 |
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448 | ptmp = grid%p(i,1,j)+grid%pb(i,1,j) |
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449 | temp(1) = thtmp * (ptmp/p1000mb)**rcp |
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450 | thtmp = grid%t_2(i,2,j)+t0 |
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451 | ptmp = grid%p(i,2,j)+grid%pb(i,2,j) |
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452 | temp(2) = thtmp * (ptmp/p1000mb)**rcp |
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453 | thtmp = grid%t_2(i,3,j)+t0 |
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454 | ptmp = grid%p(i,3,j)+grid%pb(i,3,j) |
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455 | temp(3) = thtmp * (ptmp/p1000mb)**rcp |
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456 | grid%tsk(I,J)=cf1*temp(1)+cf2*temp(2)+cf3*temp(3) |
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457 | grid%tmn(I,J)=grid%tsk(I,J)-0.5 |
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458 | END DO |
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459 | END DO |
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460 | |
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461 | RETURN |
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462 | |
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463 | END SUBROUTINE init_domain_rk |
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464 | |
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465 | !--------------------------------------------------------------------- |
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466 | |
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467 | SUBROUTINE init_module_initialize |
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468 | END SUBROUTINE init_module_initialize |
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469 | |
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470 | !--------------------------------------------------------------------- |
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471 | |
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472 | END MODULE module_initialize_ideal |
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