1 | MODULE sbcflx_tam |
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2 | #if defined key_tam |
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3 | !!====================================================================== |
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4 | !! *** MODULE sbcflx_tam *** |
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5 | !! Ocean forcing: momentum, heat and freshwater flux formulation |
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6 | !! Angent and Andjoint Module |
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7 | !!===================================================================== |
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8 | !! History of the direct module: |
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9 | !! 9.0 ! 06-06 (G. Madec) Original code |
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10 | !! History of the T&A module: |
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11 | !! 9.0 ! 08-11 (A. Vidard) Original code |
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12 | !! 3.2 ! 10-04 (A. Vidard) Update to new reference |
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13 | !!---------------------------------------------------------------------- |
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14 | |
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15 | !!---------------------------------------------------------------------- |
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16 | !! namflx : flux formulation namlist |
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17 | !! sbc_flx : flux formulation as ocean surface boundary condition |
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18 | !! (forced mode, fluxes read in NetCDF files) |
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19 | !!---------------------------------------------------------------------- |
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20 | !! question diverses |
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21 | !! * ajouter un test sur la division entier de freqh et rdttra ??? |
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22 | !! ** ajoute dans namelist: 1 year forcing files |
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23 | !! or forcing file starts at the begining of the run |
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24 | !! *** we assume that the forcing file start and end with the previous |
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25 | !! year last record and the next year first record (useful for |
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26 | !! time interpolation, required even if no time interp???) |
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27 | !! * ajouter un test sur la division de la frequence en pas de temps |
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28 | !! ==> daymod ajout de nsec_year = number of second since the begining of the year |
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29 | !! assumed to be 0 at 0h january the 1st (i.e. 24h december the 31) |
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30 | !! |
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31 | !! *** regrouper dtatem et dtasal |
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32 | !!---------------------------------------------------------------------- |
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33 | USE par_kind |
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34 | USE par_oce |
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35 | USE sbc_oce_tam |
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36 | |
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37 | IMPLICIT NONE |
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38 | PRIVATE |
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39 | |
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40 | PUBLIC sbc_flx_tan ! routine called by sbcmod_tam.F90 |
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41 | PUBLIC sbc_flx_adj ! routine called by sbcmod_tam.F90 |
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42 | PUBLIC sbc_flx_adj_tst ! routine called by tst.F90 |
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43 | |
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44 | REAL(wp) :: rhoa = 1.22 ! Air density kg/m3 |
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45 | REAL(wp) :: cdrag = 1.5e-3 ! drag coefficient |
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46 | |
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47 | !! * Substitutions |
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48 | # include "domzgr_substitute.h90" |
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49 | # include "vectopt_loop_substitute.h90" |
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50 | !!---------------------------------------------------------------------- |
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51 | !! OPA 9.0 , LOCEAN-IPSL (2006) |
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52 | !! $Id: sbcflx.F90 1200 2008-09-24 13:05:20Z rblod $ |
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53 | !! Software governed by the CeCILL licence (modipsl/doc/NEMO_CeCILL.txt) |
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54 | !!---------------------------------------------------------------------- |
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55 | |
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56 | CONTAINS |
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57 | |
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58 | SUBROUTINE sbc_flx_tan( kt ) |
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59 | !!--------------------------------------------------------------------- |
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60 | !! *** ROUTINE sbc_flx_tan *** |
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61 | !! |
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62 | !! ** Purpose of the direct routine: |
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63 | !! provide at each time step the surface ocean fluxes |
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64 | !! (momentum, heat, freshwater and runoff) |
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65 | !! |
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66 | !! ** Method : - READ each fluxes in NetCDF files: |
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67 | !! i-component of the stress utau (N/m2) |
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68 | !! j-component of the stress vtau (N/m2) |
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69 | !! net downward heat flux qtot (watt/m2) |
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70 | !! net downward radiative flux qsr (watt/m2) |
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71 | !! net upward freshwater (evapo - precip) emp (kg/m2/s) |
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72 | !! |
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73 | !! CAUTION : - never mask the surface stress fields |
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74 | !! - the stress is assumed to be in the mesh referential |
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75 | !! i.e. the (i,j) referential |
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76 | !! |
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77 | !! ** Action : update at each time-step |
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78 | !! - utau, vtau i- and j-component of the wind stress |
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79 | !! - taum wind stress module at T-point |
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80 | !! - wndm 10m wind module at T-point |
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81 | !! - qns, qsr non-slor and solar heat flux |
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82 | !! - emp, emps evaporation minus precipitation |
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83 | !!---------------------------------------------------------------------- |
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84 | INTEGER, INTENT(in) :: kt ! ocean time step |
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85 | !! |
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86 | INTEGER :: ji, jj ! dummy indices |
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87 | !! |
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88 | !!--------------------------------------------------------------------- |
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89 | ! set the ocean fluxes from read fields |
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90 | !CDIR COLLAPSE |
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91 | DO jj = 1, jpj |
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92 | DO ji = 1, jpi |
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93 | utau_tl(ji,jj) = 0.0_wp |
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94 | vtau_tl(ji,jj) = 0.0_wp |
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95 | qns_tl (ji,jj) = 0.0_wp |
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96 | qsr_tl (ji,jj) = 0.0_wp |
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97 | emp_tl (ji,jj) = 0.0_wp |
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98 | END DO |
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99 | END DO |
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100 | |
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101 | ! Initialization of emps (when no ice model) |
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102 | emps_tl(:,:) = emp_tl (:,:) |
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103 | |
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104 | ! Estimation of wind speed as a function of wind stress ( |tau|=rhoa*Cd*|U|^2 ) |
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105 | ! WARNING !!! TANGENT NOT VALID if TAU is part of the state vector. |
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106 | taum_tl(:,:) = 0.0_wp |
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107 | wndm_tl(:,:) = 0.0_wp |
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108 | ! |
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109 | END SUBROUTINE sbc_flx_tan |
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110 | SUBROUTINE sbc_flx_adj( kt ) |
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111 | !!--------------------------------------------------------------------- |
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112 | !! *** ROUTINE sbc_flx_adj *** |
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113 | !! |
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114 | !! ** Purpose of the direct routine: |
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115 | !! provide at each time step the surface ocean fluxes |
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116 | !! (momentum, heat, freshwater and runoff) |
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117 | !! |
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118 | !! ** Method : - READ each fluxes in NetCDF files: |
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119 | !! i-component of the stress utau (N/m2) |
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120 | !! j-component of the stress vtau (N/m2) |
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121 | !! net downward heat flux qtot (watt/m2) |
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122 | !! net downward radiative flux qsr (watt/m2) |
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123 | !! net upward freshwater (evapo - precip) emp (kg/m2/s) |
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124 | !! |
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125 | !! CAUTION : - never mask the surface stress fields |
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126 | !! - the stress is assumed to be in the mesh referential |
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127 | !! i.e. the (i,j) referential |
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128 | !! |
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129 | !! ** Action : update at each time-step |
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130 | !! - utau, vtau i- and j-component of the wind stress |
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131 | !! - taum wind stress module at T-point |
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132 | !! - wndm 10m wind module at T-point |
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133 | !! - qns, qsr non-slor and solar heat flux |
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134 | !! - emp, emps evaporation minus precipitation |
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135 | !!---------------------------------------------------------------------- |
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136 | INTEGER, INTENT(in) :: kt ! ocean time step |
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137 | !! |
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138 | INTEGER :: ji, jj ! dummy indices |
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139 | !! |
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140 | !!--------------------------------------------------------------------- |
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141 | ! Estimation of wind speed as a function of wind stress ( |tau|=rhoa*Cd*|U|^2 ) |
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142 | ! WARNING !!! ADJGENT NOT VALID if TAU is par of the state vector. |
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143 | taum_ad(:,:) = 0.0_wp |
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144 | wndm_ad(:,:) = 0.0_wp |
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145 | ! Initialization of emps (when no ice model) |
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146 | emp_ad (:,:) = emp_ad (:,:) + emps_ad(:,:) |
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147 | emps_ad(:,:) = 0.0_wp |
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148 | ! set the ocean fluxes from read fields |
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149 | !CDIR COLLAPSE |
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150 | DO jj = 1, jpj |
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151 | DO ji = 1, jpi |
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152 | utau_ad(ji,jj) = 0.0_wp |
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153 | vtau_ad(ji,jj) = 0.0_wp |
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154 | qns_ad (ji,jj) = 0.0_wp |
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155 | qsr_ad (ji,jj) = 0.0_wp |
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156 | emp_ad (ji,jj) = 0.0_wp |
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157 | END DO |
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158 | END DO |
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159 | ! |
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160 | END SUBROUTINE sbc_flx_adj |
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161 | SUBROUTINE sbc_flx_adj_tst( kumadt ) |
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162 | !!----------------------------------------------------------------------- |
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163 | !! |
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164 | !! *** ROUTINE sbc_flx_adj_tst *** |
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165 | !! |
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166 | !! ** Purpose : Test the adjoint routine. |
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167 | !! |
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168 | !! ** Method : Verify the scalar product |
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169 | !! |
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170 | !! ( L dx )^T W dy = dx^T L^T W dy |
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171 | !! |
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172 | !! where L = tangent routine |
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173 | !! L^T = adjoint routine |
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174 | !! W = diagonal matrix of scale factors |
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175 | !! dx = input perturbation (random field) |
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176 | !! dy = L dx |
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177 | !! |
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178 | !! |
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179 | !! History : |
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180 | !! ! 08-11 (A. Vidard) |
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181 | !!----------------------------------------------------------------------- |
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182 | !! * Modules used |
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183 | |
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184 | !! * Arguments |
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185 | INTEGER, INTENT(IN) :: & |
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186 | & kumadt ! Output unit |
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187 | |
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188 | ! adjoint is obvious, no need to test... |
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189 | END SUBROUTINE sbc_flx_adj_tst |
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190 | #endif |
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191 | !!====================================================================== |
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192 | END MODULE sbcflx_tam |
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