1 | MODULE traadv_cen2 |
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2 | !!============================================================================== |
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3 | !! *** MODULE traadv_cen2 *** |
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4 | !! Ocean active tracers: horizontal & vertical advective trend |
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5 | !!============================================================================== |
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6 | !! History : |
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7 | !! 8.2 ! 01-08 (G. Madec, E. Durand) trahad+trazad = traadv |
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8 | !! 8.5 ! 02-06 (G. Madec) F90: Free form and module |
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9 | !! 9.0 ! 04-08 (C. Talandier) New trends organization |
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10 | !! " ! 05-11 (V. Garnier) Surface pressure gradient organization |
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11 | !! " ! 06-04 (R. Benshila, G. Madec) Step reorganization |
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12 | !!---------------------------------------------------------------------- |
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13 | !! tra_adv_cen2 : update the tracer trend with the horizontal and |
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14 | !! vertical advection trends using a seconder order |
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15 | !! centered scheme. (k-j-i loops) |
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16 | !!---------------------------------------------------------------------- |
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17 | !! * Modules used |
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18 | USE oce ! ocean dynamics and active tracers |
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19 | USE dom_oce ! ocean space and time domain |
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20 | USE trdmod ! ocean active tracers trends |
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21 | USE trdmod_oce ! ocean variables trends |
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22 | USE flxrnf ! |
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23 | USE trabbl ! advective term in the BBL |
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24 | USE ocfzpt ! |
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25 | USE lib_mpp |
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26 | USE lbclnk ! ocean lateral boundary condition (or mpp link) |
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27 | USE in_out_manager ! I/O manager |
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28 | USE diaptr ! poleward transport diagnostics |
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29 | USE dynspg_oce ! choice/control of key cpp for surface pressure gradient |
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30 | USE prtctl ! Print control |
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31 | |
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32 | IMPLICIT NONE |
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33 | PRIVATE |
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34 | |
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35 | !! * Accessibility |
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36 | PUBLIC tra_adv_cen2 ! routine called by step.F90 |
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37 | |
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38 | !! * Substitutions |
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39 | # include "domzgr_substitute.h90" |
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40 | # include "vectopt_loop_substitute.h90" |
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41 | !!---------------------------------------------------------------------- |
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42 | !! OPA 9.0 , LOCEAN-IPSL (2005) |
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43 | !! $Header$ |
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44 | !! This software is governed by the CeCILL licence see modipsl/doc/NEMO_CeCILL.txt |
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45 | !!---------------------------------------------------------------------- |
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46 | |
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47 | CONTAINS |
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48 | |
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49 | SUBROUTINE tra_adv_cen2( kt, pun, pvn, pwn ) |
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50 | !!---------------------------------------------------------------------- |
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51 | !! *** ROUTINE tra_adv_cen2 *** |
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52 | !! |
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53 | !! ** Purpose : Compute the now trend due to the advection of tracers |
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54 | !! and add it to the general trend of passive tracer equations. |
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55 | !! |
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56 | !! ** Method : The advection is evaluated by a second order centered |
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57 | !! scheme using now fields (leap-frog scheme). In specific areas |
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58 | !! (vicinity of major river mouths, some straits, or where tn is |
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59 | !! approaching the freezing point) it is mixed with an upstream |
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60 | !! scheme for stability reasons. |
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61 | !! Part 0 : compute the upstream / centered flag |
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62 | !! (3D array, zind, defined at T-point (0<zind<1)) |
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63 | !! Part I : horizontal advection |
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64 | !! * centered flux: |
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65 | !! zcenu = e2u*e3u un mi(tn) |
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66 | !! zcenv = e1v*e3v vn mj(tn) |
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67 | !! * upstream flux: |
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68 | !! zupsu = e2u*e3u un (tb(i) or tb(i-1) ) [un>0 or <0] |
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69 | !! zupsv = e1v*e3v vn (tb(j) or tb(j-1) ) [vn>0 or <0] |
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70 | !! * mixed upstream / centered horizontal advection scheme |
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71 | !! zcofi = max(zind(i+1), zind(i)) |
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72 | !! zcofj = max(zind(j+1), zind(j)) |
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73 | !! zwx = zcofi * zupsu + (1-zcofi) * zcenu |
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74 | !! zwy = zcofj * zupsv + (1-zcofj) * zcenv |
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75 | !! * horizontal advective trend (divergence of the fluxes) |
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76 | !! zta = 1/(e1t*e2t*e3t) { di-1[zwx] + dj-1[zwy] } |
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77 | !! * Add this trend now to the general trend of tracer (ta,sa): |
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78 | !! (ta,sa) = (ta,sa) + ( zta , zsa ) |
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79 | !! * trend diagnostic ('key_trdtra' defined): the trend is |
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80 | !! saved for diagnostics. The trends saved is expressed as |
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81 | !! Uh.gradh(T), i.e. |
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82 | !! save trend = zta + tn divn |
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83 | !! In addition, the advective trend in the two horizontal direc- |
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84 | !! tion is also re-computed as Uh gradh(T). Indeed hadt+tn divn is |
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85 | !! equal to (in s-coordinates, and similarly in z-coord.): |
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86 | !! zta+tn*divn=1/(e1t*e2t*e3t) { mi-1( e2u*e3u un di[tn] ) |
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87 | !! +mj-1( e1v*e3v vn mj[tn] ) } |
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88 | !! C A U T I O N : the trend saved is the centered trend only. |
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89 | !! It doesn't take into account the upstream part of the scheme. |
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90 | !! NB:in z-coordinate - full step (ln_zco=T) e3u=e3v=e3t, so |
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91 | !! they vanish from the expression of the flux and divergence. |
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92 | !! |
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93 | !! Part II : vertical advection |
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94 | !! For temperature (idem for salinity) the advective trend is com- |
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95 | !! puted as follows : |
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96 | !! zta = 1/e3t dk+1[ zwz ] |
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97 | !! where the vertical advective flux, zwz, is given by : |
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98 | !! zwz = zcofk * zupst + (1-zcofk) * zcent |
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99 | !! with |
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100 | !! zupsv = upstream flux = wn * (tb(k) or tb(k-1) ) [wn>0 or <0] |
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101 | !! zcenu = centered flux = wn * mk(tn) |
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102 | !! The surface boundary condition is : |
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103 | !! rigid-lid (lk_dynspg_frd = T) : zero advective flux |
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104 | !! free-surf (lk_dynspg_fsc = T) : wn(:,:,1) * tn(:,:,1) |
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105 | !! Add this trend now to the general trend of tracer (ta,sa): |
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106 | !! (ta,sa) = (ta,sa) + ( zta , zsa ) |
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107 | !! Trend diagnostic ('key_trdtra' defined): the trend is |
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108 | !! saved for diagnostics. The trends saved is expressed as : |
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109 | !! save trend = w.gradz(T) = zta - tn divn. |
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110 | !! |
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111 | !! ** Action : - update (ta,sa) with the now advective tracer trends |
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112 | !! - save trends in (ttrdh,ttrd,strdhi,strd) ('key_trdtra') |
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113 | !! |
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114 | !!---------------------------------------------------------------------- |
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115 | !! * Modules used |
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116 | USE oce , zwx => ua, & ! use ua as workspace |
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117 | & zwy => va ! use va as workspace |
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118 | |
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119 | !! * Arguments |
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120 | INTEGER , INTENT( in ) :: kt ! ocean time-step index |
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121 | REAL(wp), INTENT( in ), DIMENSION(jpi,jpj,jpk) :: & |
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122 | pun, pvn, pwn ! now ocean velocity fields |
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123 | |
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124 | !! * Local save |
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125 | REAL(wp), DIMENSION(jpi,jpj), SAVE :: & |
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126 | zbtr2 |
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127 | |
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128 | !! * Local declarations |
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129 | INTEGER :: ji, jj, jk ! dummy loop indices |
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130 | REAL(wp) :: & |
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131 | zbtr, zta, zsa, zfui, zfvj, & ! temporary scalars |
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132 | zhw, ze3tr, zcofi, zcofj, & ! " " |
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133 | zupsut, zupsvt, zupsus, zupsvs, & ! " " |
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134 | zfp_ui, zfp_vj, zfm_ui, zfm_vj, & ! " " |
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135 | zcofk, zupst, zupss, zcent, & ! " " |
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136 | zcens, zfp_w, zfm_w, & ! " " |
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137 | zcenut, zcenvt, zcenus, zcenvs ! " " |
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138 | REAL(wp), DIMENSION(jpi,jpj,jpk) :: & |
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139 | zwz, zww, zind, & ! temporary workspace arrays |
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140 | ztdta, ztdsa ! " " |
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141 | !!---------------------------------------------------------------------- |
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142 | |
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143 | IF( kt == nit000 ) THEN |
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144 | IF(lwp) WRITE(numout,*) |
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145 | IF(lwp) WRITE(numout,*) 'tra_adv_cen2 : 2nd order centered advection scheme' |
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146 | IF(lwp) WRITE(numout,*) '~~~~~~~~~~~~ Vector optimization case' |
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147 | IF(lwp) WRITE(numout,*) |
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148 | |
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149 | zbtr2(:,:) = 1. / ( e1t(:,:) * e2t(:,:) ) |
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150 | ENDIF |
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151 | |
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152 | ! Save ta and sa trends |
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153 | IF( l_trdtra ) THEN |
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154 | ztdta(:,:,:) = ta(:,:,:) |
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155 | ztdsa(:,:,:) = sa(:,:,:) |
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156 | l_adv = 'ce2' |
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157 | ENDIF |
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158 | |
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159 | ! Upstream / centered scheme indicator |
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160 | ! ------------------------------------ |
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161 | |
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162 | DO jk = 1, jpk |
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163 | DO jj = 1, jpj |
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164 | DO ji = 1, jpi |
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165 | zind(ji,jj,jk) = MAX ( upsrnfh(ji,jj) * upsrnfz(jk), & ! changing advection scheme near runoff |
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166 | & upsadv(ji,jj) & ! in the vicinity of some straits |
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167 | #if defined key_ice_lim |
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168 | & , tmask(ji,jj,jk) & ! half upstream tracer fluxes |
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169 | & * MAX( 0., SIGN( 1., fzptn(ji,jj) & ! if tn < ("freezing"+0.1 ) |
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170 | & +0.1-tn(ji,jj,jk) ) ) & |
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171 | #endif |
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172 | & ) |
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173 | END DO |
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174 | END DO |
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175 | END DO |
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176 | |
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177 | |
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178 | ! I. Horizontal advective fluxes |
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179 | ! ------------------------------ |
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180 | |
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181 | ! 1. Second order centered tracer flux at u and v-points |
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182 | ! ------------------------------------------------------- |
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183 | |
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184 | ! ! =============== |
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185 | DO jk = 1, jpkm1 ! Horizontal slab |
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186 | ! ! =============== |
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187 | DO jj = 1, jpjm1 |
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188 | DO ji = 1, fs_jpim1 ! vector opt. |
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189 | ! upstream indicator |
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190 | zcofi = MAX( zind(ji+1,jj,jk), zind(ji,jj,jk) ) |
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191 | zcofj = MAX( zind(ji,jj+1,jk), zind(ji,jj,jk) ) |
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192 | ! volume fluxes * 1/2 |
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193 | #if defined key_zco |
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194 | zfui = 0.5 * e2u(ji,jj) * pun(ji,jj,jk) |
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195 | zfvj = 0.5 * e1v(ji,jj) * pvn(ji,jj,jk) |
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196 | #else |
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197 | zfui = 0.5 * e2u(ji,jj) * fse3u(ji,jj,jk) * pun(ji,jj,jk) |
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198 | zfvj = 0.5 * e1v(ji,jj) * fse3v(ji,jj,jk) * pvn(ji,jj,jk) |
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199 | #endif |
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200 | ! upstream scheme |
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201 | zfp_ui = zfui + ABS( zfui ) |
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202 | zfp_vj = zfvj + ABS( zfvj ) |
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203 | zfm_ui = zfui - ABS( zfui ) |
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204 | zfm_vj = zfvj - ABS( zfvj ) |
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205 | zupsut = zfp_ui * tb(ji,jj,jk) + zfm_ui * tb(ji+1,jj ,jk) |
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206 | zupsvt = zfp_vj * tb(ji,jj,jk) + zfm_vj * tb(ji ,jj+1,jk) |
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207 | zupsus = zfp_ui * sb(ji,jj,jk) + zfm_ui * sb(ji+1,jj ,jk) |
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208 | zupsvs = zfp_vj * sb(ji,jj,jk) + zfm_vj * sb(ji ,jj+1,jk) |
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209 | ! centered scheme |
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210 | zcenut = zfui * ( tn(ji,jj,jk) + tn(ji+1,jj ,jk) ) |
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211 | zcenvt = zfvj * ( tn(ji,jj,jk) + tn(ji ,jj+1,jk) ) |
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212 | zcenus = zfui * ( sn(ji,jj,jk) + sn(ji+1,jj ,jk) ) |
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213 | zcenvs = zfvj * ( sn(ji,jj,jk) + sn(ji ,jj+1,jk) ) |
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214 | ! mixed centered / upstream scheme |
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215 | zwx(ji,jj,jk) = zcofi * zupsut + (1.-zcofi) * zcenut |
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216 | zwy(ji,jj,jk) = zcofj * zupsvt + (1.-zcofj) * zcenvt |
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217 | zww(ji,jj,jk) = zcofi * zupsus + (1.-zcofi) * zcenus |
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218 | zwz(ji,jj,jk) = zcofj * zupsvs + (1.-zcofj) * zcenvs |
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219 | END DO |
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220 | END DO |
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221 | |
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222 | ! 2. Tracer flux divergence at t-point added to the general trend |
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223 | ! --------------------------------------------------------------- |
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224 | |
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225 | DO jj = 2, jpjm1 |
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226 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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227 | #if defined key_zco |
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228 | zbtr = zbtr2(ji,jj) |
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229 | #else |
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230 | zbtr = zbtr2(ji,jj) / fse3t(ji,jj,jk) |
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231 | #endif |
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232 | ! horizontal advective trends |
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233 | zta = - zbtr * ( zwx(ji,jj,jk) - zwx(ji-1,jj ,jk) & |
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234 | & + zwy(ji,jj,jk) - zwy(ji ,jj-1,jk) ) |
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235 | zsa = - zbtr * ( zww(ji,jj,jk) - zww(ji-1,jj ,jk) & |
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236 | & + zwz(ji,jj,jk) - zwz(ji ,jj-1,jk) ) |
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237 | ! add it to the general tracer trends |
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238 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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239 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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240 | END DO |
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241 | END DO |
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242 | ! ! =============== |
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243 | END DO ! End of slab |
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244 | ! ! =============== |
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245 | |
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246 | ! 3. Save the horizontal advective trends for diagnostic |
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247 | ! ------------------------------------------------------ |
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248 | IF( l_trdtra ) THEN |
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249 | ! Recompute the hoizontal advection zta & zsa trends computed |
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250 | ! at the step 2. above in making the difference between the new |
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251 | ! trends and the previous one ta()/sa - ztdta()/ztdsa() and add |
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252 | ! the term tn()/sn()*hdivn() to recover the Uh gradh(T/S) trends |
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253 | ztdta(:,:,:) = ta(:,:,:) - ztdta(:,:,:) + tn(:,:,:) * hdivn(:,:,:) |
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254 | ztdsa(:,:,:) = sa(:,:,:) - ztdsa(:,:,:) + sn(:,:,:) * hdivn(:,:,:) |
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255 | |
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256 | CALL trd_mod(ztdta, ztdsa, jpttdlad, 'TRA', kt) |
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257 | |
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258 | ! Save the new ta and sa trends |
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259 | ztdta(:,:,:) = ta(:,:,:) |
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260 | ztdsa(:,:,:) = sa(:,:,:) |
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261 | |
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262 | ENDIF |
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263 | |
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264 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ta, clinfo1=' cen2 had - Ta: ', mask1=tmask, & |
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265 | & tab3d_2=sa, clinfo2= ' Sa: ', mask2=tmask, clinfo3='tra' ) |
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266 | |
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267 | ! "zonal" mean advective heat and salt transport |
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268 | IF( ln_diaptr .AND. ( MOD( kt, nf_ptr ) == 0 ) ) THEN |
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269 | IF( lk_zco ) THEN |
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270 | DO jk = 1, jpkm1 |
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271 | DO jj = 2, jpjm1 |
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272 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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273 | zwy(ji,jj,jk) = zwy(ji,jj,jk) * fse3v(ji,jj,jk) |
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274 | zwz(ji,jj,jk) = zwz(ji,jj,jk) * fse3v(ji,jj,jk) |
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275 | END DO |
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276 | END DO |
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277 | END DO |
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278 | ENDIF |
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279 | pht_adv(:) = ptr_vj( zwy(:,:,:) ) |
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280 | pst_adv(:) = ptr_vj( zwz(:,:,:) ) |
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281 | ENDIF |
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282 | |
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283 | ! II. Vertical advection |
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284 | ! ---------------------- |
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285 | |
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286 | ! Bottom value : flux set to zero |
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287 | zwx(:,:,jpk) = 0.e0 ; zwy(:,:,jpk) = 0.e0 |
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288 | |
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289 | ! Surface value |
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290 | IF( lk_dynspg_rl ) THEN |
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291 | ! rigid lid : flux set to zero |
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292 | zwx(:,:, 1 ) = 0.e0 ; zwy(:,:, 1 ) = 0.e0 |
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293 | ELSE |
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294 | ! free surface |
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295 | zwx(:,:, 1 ) = pwn(:,:,1) * tn(:,:,1) |
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296 | zwy(:,:, 1 ) = pwn(:,:,1) * sn(:,:,1) |
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297 | ENDIF |
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298 | |
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299 | ! 1. Vertical advective fluxes |
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300 | ! ---------------------------- |
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301 | |
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302 | ! Second order centered tracer flux at w-point |
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303 | |
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304 | DO jk = 2, jpk |
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305 | DO jj = 2, jpjm1 |
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306 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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307 | ! upstream indicator |
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308 | zcofk = MAX( zind(ji,jj,jk-1), zind(ji,jj,jk) ) |
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309 | ! velocity * 1/2 |
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310 | zhw = 0.5 * pwn(ji,jj,jk) |
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311 | ! upstream scheme |
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312 | zfp_w = zhw + ABS( zhw ) |
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313 | zfm_w = zhw - ABS( zhw ) |
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314 | zupst = zfp_w * tb(ji,jj,jk) + zfm_w * tb(ji,jj,jk-1) |
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315 | zupss = zfp_w * sb(ji,jj,jk) + zfm_w * sb(ji,jj,jk-1) |
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316 | ! centered scheme |
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317 | zcent = zhw * ( tn(ji,jj,jk) + tn(ji,jj,jk-1) ) |
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318 | zcens = zhw * ( sn(ji,jj,jk) + sn(ji,jj,jk-1) ) |
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319 | ! mixed centered / upstream scheme |
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320 | zwx(ji,jj,jk) = zcofk * zupst + (1.-zcofk) * zcent |
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321 | zwy(ji,jj,jk) = zcofk * zupss + (1.-zcofk) * zcens |
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322 | END DO |
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323 | END DO |
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324 | END DO |
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325 | |
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326 | |
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327 | ! 2. Tracer flux divergence at t-point added to the general trend |
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328 | ! ------------------------- |
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329 | |
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330 | DO jk = 1, jpkm1 |
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331 | DO jj = 2, jpjm1 |
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332 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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333 | ze3tr = 1. / fse3t(ji,jj,jk) |
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334 | ! vertical advective trends |
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335 | zta = - ze3tr * ( zwx(ji,jj,jk) - zwx(ji,jj,jk+1) ) |
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336 | zsa = - ze3tr * ( zwy(ji,jj,jk) - zwy(ji,jj,jk+1) ) |
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337 | ! add it to the general tracer trends |
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338 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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339 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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340 | END DO |
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341 | END DO |
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342 | END DO |
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343 | |
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344 | ! 3. Save the vertical advective trends for diagnostic |
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345 | ! ---------------------------------------------------- |
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346 | IF( l_trdtra ) THEN |
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347 | ! Recompute the vertical advection zta & zsa trends computed |
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348 | ! at the step 2. above in making the difference between the new |
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349 | ! trends and the previous one: ta()/sa - ztdta()/ztdsa() and substract |
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350 | ! the term tn()/sn()*hdivn() to recover the W gradz(T/S) trends |
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351 | ztdta(:,:,:) = ta(:,:,:) - ztdta(:,:,:) - tn(:,:,:) * hdivn(:,:,:) |
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352 | ztdsa(:,:,:) = sa(:,:,:) - ztdsa(:,:,:) - sn(:,:,:) * hdivn(:,:,:) |
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353 | |
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354 | CALL trd_mod(ztdta, ztdsa, jpttdzad, 'TRA', kt) |
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355 | ENDIF |
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356 | |
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357 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ta, clinfo1=' cen2 zad - Ta: ', mask1=tmask, & |
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358 | & tab3d_2=sa, clinfo2= ' Sa: ', mask2=tmask, clinfo3='tra' ) |
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359 | |
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360 | |
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361 | END SUBROUTINE tra_adv_cen2 |
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362 | |
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363 | !!====================================================================== |
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364 | END MODULE traadv_cen2 |
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