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 : 8.2 ! 01-08 (G. Madec, E. Durand) trahad+trazad=traadv |
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7 | !! 8.5 ! 02-06 (G. Madec) F90: Free form and module |
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8 | !! 9.0 ! 04-08 (C. Talandier) New trends organization |
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9 | !! " " ! 05-11 (V. Garnier) Surface pressure gradient organization |
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10 | !! " " ! 06-04 (R. Benshila, G. Madec) Step reorganization |
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11 | !! " " ! 06-07 (G. madec) add ups_orca_set routine |
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12 | !!---------------------------------------------------------------------- |
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13 | |
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14 | !!---------------------------------------------------------------------- |
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15 | !! tra_adv_cen2 : update the tracer trend with the horizontal and |
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16 | !! vertical advection trends using a seconder order |
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17 | !! ups_orca_set : allow mixed upstream/centered scheme in specific |
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18 | !! area (set for orca 2 and 4 only) |
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19 | !!---------------------------------------------------------------------- |
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20 | USE oce ! ocean dynamics and active tracers |
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21 | USE dom_oce ! ocean space and time domain |
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22 | USE sbc_oce ! surface boundary condition: ocean |
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23 | USE dynspg_oce ! choice/control of key cpp for surface pressure gradient |
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24 | USE trdmod_oce ! ocean variables trends |
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25 | USE eosbn2 ! equation of state |
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26 | USE trdmod ! ocean active tracers trends |
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27 | USE closea ! closed sea |
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28 | USE trabbl ! advective term in the BBL |
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29 | USE sbcmod ! surface Boundary Condition |
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30 | USE sbcrnf ! river runoffs |
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31 | USE in_out_manager ! I/O manager |
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32 | USE lib_mpp |
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33 | USE lbclnk ! ocean lateral boundary condition (or mpp link) |
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34 | USE diaptr ! poleward transport diagnostics |
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35 | USE prtctl ! Print control |
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36 | USE zdf_oce ! ocean vertical physics |
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37 | |
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38 | IMPLICIT NONE |
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39 | PRIVATE |
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40 | |
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41 | PUBLIC tra_adv_cen2 ! routine called by step.F90 |
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42 | PUBLIC ups_orca_set ! routine used by traadv_cen2_jki.F90 |
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43 | |
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44 | REAL(wp), PUBLIC, DIMENSION(jpi,jpj) :: upsmsk !: mixed upstream/centered scheme near some straits |
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45 | ! ! and in closed seas (orca 2 and 4 configurations) |
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46 | |
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47 | REAL(wp), DIMENSION(jpi,jpj) :: btr2 ! inverse of T-point surface [1/(e1t*e2t)] |
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48 | |
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49 | !! * Substitutions |
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50 | # include "domzgr_substitute.h90" |
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51 | # include "vectopt_loop_substitute.h90" |
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52 | !!---------------------------------------------------------------------- |
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53 | !! OPA 9.0 , LOCEAN-IPSL (2006) |
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54 | !! $Id$ |
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55 | !! Software governed by the CeCILL licence (modipsl/doc/NEMO_CeCILL.txt) |
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56 | !!---------------------------------------------------------------------- |
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57 | |
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58 | CONTAINS |
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59 | |
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60 | SUBROUTINE tra_adv_cen2( kt, pun, pvn, pwn ) |
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61 | !!---------------------------------------------------------------------- |
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62 | !! *** ROUTINE tra_adv_cen2 *** |
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63 | !! |
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64 | !! ** Purpose : Compute the now trend due to the advection of tracers |
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65 | !! and add it to the general trend of passive tracer equations. |
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66 | !! |
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67 | !! ** Method : The advection is evaluated by a second order centered |
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68 | !! scheme using now fields (leap-frog scheme). In specific areas |
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69 | !! (vicinity of major river mouths, some straits, or where tn is |
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70 | !! approaching the freezing point) it is mixed with an upstream |
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71 | !! scheme for stability reasons. |
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72 | !! Part 0 : compute the upstream / centered flag |
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73 | !! (3D array, zind, defined at T-point (0<zind<1)) |
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74 | !! Part I : horizontal advection |
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75 | !! * centered flux: |
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76 | !! zcenu = e2u*e3u un mi(tn) |
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77 | !! zcenv = e1v*e3v vn mj(tn) |
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78 | !! * upstream flux: |
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79 | !! zupsu = e2u*e3u un (tb(i) or tb(i-1) ) [un>0 or <0] |
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80 | !! zupsv = e1v*e3v vn (tb(j) or tb(j-1) ) [vn>0 or <0] |
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81 | !! * mixed upstream / centered horizontal advection scheme |
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82 | !! zcofi = max(zind(i+1), zind(i)) |
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83 | !! zcofj = max(zind(j+1), zind(j)) |
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84 | !! zwx = zcofi * zupsu + (1-zcofi) * zcenu |
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85 | !! zwy = zcofj * zupsv + (1-zcofj) * zcenv |
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86 | !! * horizontal advective trend (divergence of the fluxes) |
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87 | !! zta = 1/(e1t*e2t*e3t) { di-1[zwx] + dj-1[zwy] } |
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88 | !! * Add this trend now to the general trend of tracer (ta,sa): |
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89 | !! (ta,sa) = (ta,sa) + ( zta , zsa ) |
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90 | !! * trend diagnostic ('key_trdtra' defined): the trend is |
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91 | !! saved for diagnostics. The trends saved is expressed as |
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92 | !! Uh.gradh(T), i.e. |
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93 | !! save trend = zta + tn divn |
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94 | !! In addition, the advective trend in the two horizontal direc- |
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95 | !! tion is also re-computed as Uh gradh(T). Indeed hadt+tn divn is |
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96 | !! equal to (in s-coordinates, and similarly in z-coord.): |
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97 | !! zta+tn*divn=1/(e1t*e2t*e3t) { mi-1( e2u*e3u un di[tn] ) |
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98 | !! +mj-1( e1v*e3v vn mj[tn] ) } |
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99 | !! NB:in z-coordinate - full step (ln_zco=T) e3u=e3v=e3t, so |
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100 | !! they vanish from the expression of the flux and divergence. |
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101 | !! |
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102 | !! Part II : vertical advection |
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103 | !! For temperature (idem for salinity) the advective trend is com- |
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104 | !! puted as follows : |
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105 | !! zta = 1/e3t dk+1[ zwz ] |
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106 | !! where the vertical advective flux, zwz, is given by : |
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107 | !! zwz = zcofk * zupst + (1-zcofk) * zcent |
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108 | !! with |
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109 | !! zupsv = upstream flux = wn * (tb(k) or tb(k-1) ) [wn>0 or <0] |
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110 | !! zcenu = centered flux = wn * mk(tn) |
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111 | !! The surface boundary condition is : |
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112 | !! variable volume (lk_vvl = T) : zero advective flux |
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113 | !! lin. free-surf (lk_vvl = F) : wn(:,:,1) * tn(:,:,1) |
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114 | !! Add this trend now to the general trend of tracer (ta,sa): |
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115 | !! (ta,sa) = (ta,sa) + ( zta , zsa ) |
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116 | !! Trend diagnostic ('key_trdtra' defined): the trend is |
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117 | !! saved for diagnostics. The trends saved is expressed as : |
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118 | !! save trend = w.gradz(T) = zta - tn divn. |
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119 | !! |
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120 | !! ** Action : - update (ta,sa) with the now advective tracer trends |
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121 | !! - save trends in (ztrdt,ztrds) ('key_trdtra') |
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122 | !!---------------------------------------------------------------------- |
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123 | USE oce, ONLY : zwx => ua ! use ua as workspace |
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124 | USE oce, ONLY : zwy => va ! use va as workspace |
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125 | !! |
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126 | INTEGER , INTENT(in) :: kt ! ocean time-step index |
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127 | REAL(wp), INTENT(in), DIMENSION(jpi,jpj,jpk) :: pun ! ocean velocity u-component |
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128 | REAL(wp), INTENT(in), DIMENSION(jpi,jpj,jpk) :: pvn ! ocean velocity v-component |
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129 | REAL(wp), INTENT(in), DIMENSION(jpi,jpj,jpk) :: pwn ! ocean velocity w-component |
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130 | !! |
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131 | INTEGER :: ji, jj, jk ! dummy loop indices |
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132 | REAL(wp) :: zta, zsa, zbtr, zhw, ze3tr, & ! temporary scalars |
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133 | & zfp_ui, zfp_vj, zfp_w , zfui , & ! " " |
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134 | & zfm_ui, zfm_vj, zfm_w , zfvj , & ! " " |
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135 | & zcofi , zcofj , zcofk , & ! " " |
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136 | & zupsut, zupsus, zcenut, zcenus, & ! " " |
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137 | & zupsvt, zupsvs, zcenvt, zcenvs, & ! " " |
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138 | & zupst , zupss , zcent , zcens , & ! " " |
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139 | & z_hdivn_x, z_hdivn_y, z_hdivn |
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140 | REAL(wp) :: zice ! - - |
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141 | REAL(wp), DIMENSION(jpi,jpj) :: ztfreez ! 2D workspace |
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142 | REAL(wp), DIMENSION(jpi,jpj,jpk) :: zwz, ztrdt, zind ! 3D workspace |
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143 | REAL(wp), DIMENSION(jpi,jpj,jpk) :: zww, ztrds ! " " |
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144 | !!---------------------------------------------------------------------- |
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145 | |
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146 | IF( kt == nit000 ) THEN |
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147 | IF(lwp) WRITE(numout,*) |
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148 | IF(lwp) WRITE(numout,*) 'tra_adv_cen2 : 2nd order centered advection scheme' |
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149 | IF(lwp) WRITE(numout,*) '~~~~~~~~~~~~ Vector optimization case' |
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150 | IF(lwp) WRITE(numout,*) |
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151 | ! |
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152 | upsmsk(:,:) = 0.e0 ! not upstream by default |
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153 | ! |
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154 | IF( cp_cfg == "orca" ) CALL ups_orca_set ! set mixed Upstream/centered scheme near some straits |
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155 | ! ! and in closed seas (orca2 and orca4 only) |
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156 | ! |
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157 | btr2(:,:) = 1. / ( e1t(:,:) * e2t(:,:) ) ! inverse of T-point surface |
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158 | IF ( jp_cfg == 2 ) THEN |
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159 | ! Increase the background in the surface layers |
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160 | avmb(1) = 10. * avmb(1) ; avtb(1) = 10. * avtb(1) |
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161 | avmb(2) = 10. * avmb(2) ; avtb(2) = 10. * avtb(2) |
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162 | avmb(3) = 5. * avmb(3) ; avtb(3) = 5. * avtb(3) |
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163 | avmb(4) = 2.5 * avmb(4) ; avtb(4) = 2.5 * avtb(4) |
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164 | ENDIF |
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165 | ENDIF |
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166 | |
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167 | ! Upstream / centered scheme indicator |
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168 | ! ------------------------------------ |
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169 | !!gm not strickly exact : the freezing point should be computed at each ocean levels... |
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170 | !!gm not a big deal since cen2 is no more used in global ice-ocean simulations |
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171 | ztfreez(:,:) = tfreez( sn(:,:,1) ) |
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172 | DO jk = 1, jpk |
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173 | DO jj = 1, jpj |
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174 | DO ji = 1, jpi |
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175 | ! ! below ice covered area (if tn < "freezing"+0.1 ) |
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176 | IF( tn(ji,jj,jk) <= ztfreez(ji,jj) + 0.1 ) THEN ; zice = 1.e0 |
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177 | ELSE ; zice = 0.e0 |
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178 | ENDIF |
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179 | zind(ji,jj,jk) = MAX ( & |
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180 | rnfmsk(ji,jj) * rnfmsk_z(jk), & ! near runoff mouths (& closed sea outflows) |
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181 | upsmsk(ji,jj) , & ! some of some straits |
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182 | zice & ! below ice covered area (if tn < "freezing"+0.1 ) |
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183 | & ) * tmask(ji,jj,jk) |
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184 | END DO |
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185 | END DO |
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186 | END DO |
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187 | |
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188 | ! I. Horizontal advective fluxes |
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189 | ! ------------------------------ |
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190 | ! Second order centered tracer flux at u and v-points |
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191 | ! ----------------------------------------------------- |
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192 | ! ! =============== |
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193 | DO jk = 1, jpkm1 ! Horizontal slab |
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194 | ! ! =============== |
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195 | DO jj = 1, jpjm1 |
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196 | DO ji = 1, fs_jpim1 ! vector opt. |
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197 | ! upstream indicator |
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198 | zcofi = MAX( zind(ji+1,jj,jk), zind(ji,jj,jk) ) |
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199 | zcofj = MAX( zind(ji,jj+1,jk), zind(ji,jj,jk) ) |
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200 | ! volume fluxes * 1/2 |
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201 | #if defined key_zco |
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202 | zfui = 0.5 * e2u(ji,jj) * pun(ji,jj,jk) |
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203 | zfvj = 0.5 * e1v(ji,jj) * pvn(ji,jj,jk) |
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204 | #else |
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205 | zfui = 0.5 * e2u(ji,jj) * fse3u(ji,jj,jk) * pun(ji,jj,jk) |
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206 | zfvj = 0.5 * e1v(ji,jj) * fse3v(ji,jj,jk) * pvn(ji,jj,jk) |
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207 | #endif |
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208 | ! upstream scheme |
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209 | zfp_ui = zfui + ABS( zfui ) |
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210 | zfp_vj = zfvj + ABS( zfvj ) |
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211 | zfm_ui = zfui - ABS( zfui ) |
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212 | zfm_vj = zfvj - ABS( zfvj ) |
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213 | zupsut = zfp_ui * tb(ji,jj,jk) + zfm_ui * tb(ji+1,jj ,jk) |
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214 | zupsvt = zfp_vj * tb(ji,jj,jk) + zfm_vj * tb(ji ,jj+1,jk) |
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215 | zupsus = zfp_ui * sb(ji,jj,jk) + zfm_ui * sb(ji+1,jj ,jk) |
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216 | zupsvs = zfp_vj * sb(ji,jj,jk) + zfm_vj * sb(ji ,jj+1,jk) |
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217 | ! centered scheme |
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218 | zcenut = zfui * ( tn(ji,jj,jk) + tn(ji+1,jj ,jk) ) |
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219 | zcenvt = zfvj * ( tn(ji,jj,jk) + tn(ji ,jj+1,jk) ) |
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220 | zcenus = zfui * ( sn(ji,jj,jk) + sn(ji+1,jj ,jk) ) |
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221 | zcenvs = zfvj * ( sn(ji,jj,jk) + sn(ji ,jj+1,jk) ) |
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222 | ! mixed centered / upstream scheme |
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223 | zwx(ji,jj,jk) = zcofi * zupsut + (1.-zcofi) * zcenut |
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224 | zwy(ji,jj,jk) = zcofj * zupsvt + (1.-zcofj) * zcenvt |
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225 | zww(ji,jj,jk) = zcofi * zupsus + (1.-zcofi) * zcenus |
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226 | zwz(ji,jj,jk) = zcofj * zupsvs + (1.-zcofj) * zcenvs |
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227 | END DO |
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228 | END DO |
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229 | |
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230 | ! Tracer flux divergence at t-point added to the general trend |
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231 | ! -------------------------------------------------------------- |
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232 | DO jj = 2, jpjm1 |
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233 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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234 | #if defined key_zco |
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235 | zbtr = btr2(ji,jj) |
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236 | #else |
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237 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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238 | #endif |
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239 | ! horizontal advective trends |
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240 | zta = - zbtr * ( zwx(ji,jj,jk) - zwx(ji-1,jj ,jk) & |
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241 | & + zwy(ji,jj,jk) - zwy(ji ,jj-1,jk) ) |
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242 | zsa = - zbtr * ( zww(ji,jj,jk) - zww(ji-1,jj ,jk) & |
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243 | & + zwz(ji,jj,jk) - zwz(ji ,jj-1,jk) ) |
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244 | ! add it to the general tracer trends |
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245 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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246 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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247 | END DO |
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248 | END DO |
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249 | ! ! =============== |
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250 | END DO ! End of slab |
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251 | ! ! =============== |
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252 | |
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253 | ! Save the horizontal advective trends for diagnostic |
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254 | ! ----------------------------------------------------- |
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255 | IF( l_trdtra ) THEN |
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256 | ! T/S ZONAL advection trends |
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257 | ztrdt(:,:,:) = 0.e0 ; ztrds(:,:,:) = 0.e0 |
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258 | ! |
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259 | DO jk = 1, jpkm1 |
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260 | DO jj = 2, jpjm1 |
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261 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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262 | !-- Compute zonal divergence by splitting hdivn (see divcur.F90) |
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263 | ! N.B. This computation is not valid along OBCs (if any) |
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264 | #if defined key_zco |
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265 | zbtr = btr2(ji,jj) |
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266 | z_hdivn_x = ( e2u(ji ,jj) * pun(ji ,jj,jk) & |
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267 | & - e2u(ji-1,jj) * pun(ji-1,jj,jk) ) * zbtr |
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268 | #else |
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269 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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270 | z_hdivn_x = ( e2u(ji ,jj) * fse3u(ji ,jj,jk) * pun(ji ,jj,jk) & |
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271 | & - e2u(ji-1,jj) * fse3u(ji-1,jj,jk) * pun(ji-1,jj,jk) ) * zbtr |
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272 | #endif |
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273 | ztrdt(ji,jj,jk) = - zbtr * ( zwx(ji,jj,jk) - zwx(ji-1,jj,jk) ) + tn(ji,jj,jk) * z_hdivn_x |
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274 | ztrds(ji,jj,jk) = - zbtr * ( zww(ji,jj,jk) - zww(ji-1,jj,jk) ) + sn(ji,jj,jk) * z_hdivn_x |
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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 | CALL trd_mod(ztrdt, ztrds, jptra_trd_xad, 'TRA', kt) |
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279 | ! |
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280 | ! T/S MERIDIONAL advection trends |
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281 | DO jk = 1, jpkm1 |
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282 | DO jj = 2, jpjm1 |
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283 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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284 | !-- Compute merid. divergence by splitting hdivn (see divcur.F90) |
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285 | ! N.B. This computation is not valid along OBCs (if any) |
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286 | #if defined key_zco |
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287 | zbtr = btr2(ji,jj) |
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288 | z_hdivn_y = ( e1v(ji,jj ) * pvn(ji,jj ,jk) & |
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289 | & - e1v(ji,jj-1) * pvn(ji,jj-1,jk) ) * zbtr |
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290 | #else |
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291 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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292 | z_hdivn_y = ( e1v(ji, jj) * fse3v(ji,jj ,jk) * pvn(ji,jj ,jk) & |
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293 | & - e1v(ji,jj-1) * fse3v(ji,jj-1,jk) * pvn(ji,jj-1,jk) ) * zbtr |
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294 | #endif |
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295 | ztrdt(ji,jj,jk) = - zbtr * ( zwy(ji,jj,jk) - zwy(ji,jj-1,jk) ) + tn(ji,jj,jk) * z_hdivn_y |
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296 | ztrds(ji,jj,jk) = - zbtr * ( zwz(ji,jj,jk) - zwz(ji,jj-1,jk) ) + sn(ji,jj,jk) * z_hdivn_y |
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297 | END DO |
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298 | END DO |
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299 | END DO |
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300 | CALL trd_mod(ztrdt, ztrds, jptra_trd_yad, 'TRA', kt) |
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301 | ! |
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302 | ! Save the horizontal up-to-date ta/sa trends |
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303 | ztrdt(:,:,:) = ta(:,:,:) |
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304 | ztrds(:,:,:) = sa(:,:,:) |
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305 | ENDIF |
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306 | |
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307 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ta, clinfo1=' cen2 had - Ta: ', mask1=tmask, & |
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308 | & tab3d_2=sa, clinfo2= ' Sa: ', mask2=tmask, clinfo3='tra' ) |
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309 | |
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310 | ! "zonal" mean advective heat and salt transport |
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311 | ! ---------------------------------------------- |
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312 | |
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313 | IF( ln_diaptr .AND. ( MOD( kt, nf_ptr ) == 0 ) ) THEN |
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314 | IF( lk_zco ) THEN |
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315 | DO jk = 1, jpkm1 |
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316 | DO jj = 2, jpjm1 |
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317 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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318 | zwy(ji,jj,jk) = zwy(ji,jj,jk) * fse3v(ji,jj,jk) |
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319 | zwz(ji,jj,jk) = zwz(ji,jj,jk) * fse3v(ji,jj,jk) |
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320 | END DO |
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321 | END DO |
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322 | END DO |
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323 | ENDIF |
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324 | pht_adv(:) = ptr_vj( zwy(:,:,:) ) |
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325 | pst_adv(:) = ptr_vj( zwz(:,:,:) ) |
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326 | ENDIF |
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327 | |
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328 | ! II. Vertical advection |
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329 | ! ---------------------- |
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330 | |
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331 | ! Bottom value : flux set to zero |
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332 | zwx(:,:,jpk) = 0.e0 ; zwy(:,:,jpk) = 0.e0 |
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333 | |
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334 | ! Surface value |
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335 | IF( lk_vvl ) THEN |
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336 | ! variable volume: flux set to zero |
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337 | zwx(:,:, 1 ) = 0.e0 ; zwy(:,:, 1 ) = 0.e0 |
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338 | ELSE |
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339 | ! free surface-constant volume |
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340 | zwx(:,:, 1 ) = pwn(:,:,1) * tn(:,:,1) |
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341 | zwy(:,:, 1 ) = pwn(:,:,1) * sn(:,:,1) |
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342 | ENDIF |
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343 | |
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344 | ! 1. Vertical advective fluxes |
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345 | ! ---------------------------- |
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346 | ! Second order centered tracer flux at w-point |
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347 | DO jk = 2, jpk |
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348 | DO jj = 2, jpjm1 |
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349 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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350 | ! upstream indicator |
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351 | zcofk = MAX( zind(ji,jj,jk-1), zind(ji,jj,jk) ) |
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352 | ! velocity * 1/2 |
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353 | zhw = 0.5 * pwn(ji,jj,jk) |
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354 | ! upstream scheme |
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355 | zfp_w = zhw + ABS( zhw ) |
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356 | zfm_w = zhw - ABS( zhw ) |
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357 | zupst = zfp_w * tb(ji,jj,jk) + zfm_w * tb(ji,jj,jk-1) |
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358 | zupss = zfp_w * sb(ji,jj,jk) + zfm_w * sb(ji,jj,jk-1) |
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359 | ! centered scheme |
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360 | zcent = zhw * ( tn(ji,jj,jk) + tn(ji,jj,jk-1) ) |
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361 | zcens = zhw * ( sn(ji,jj,jk) + sn(ji,jj,jk-1) ) |
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362 | ! mixed centered / upstream scheme |
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363 | zwx(ji,jj,jk) = zcofk * zupst + (1.-zcofk) * zcent |
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364 | zwy(ji,jj,jk) = zcofk * zupss + (1.-zcofk) * zcens |
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365 | END DO |
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366 | END DO |
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367 | END DO |
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368 | |
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369 | ! 2. Tracer flux divergence at t-point added to the general trend |
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370 | ! ------------------------- |
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371 | DO jk = 1, jpkm1 |
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372 | DO jj = 2, jpjm1 |
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373 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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374 | ze3tr = 1. / fse3t(ji,jj,jk) |
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375 | ! vertical advective trends |
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376 | zta = - ze3tr * ( zwx(ji,jj,jk) - zwx(ji,jj,jk+1) ) |
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377 | zsa = - ze3tr * ( zwy(ji,jj,jk) - zwy(ji,jj,jk+1) ) |
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378 | ! add it to the general tracer trends |
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379 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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380 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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381 | END DO |
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382 | END DO |
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383 | END DO |
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384 | |
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385 | ! 3. Save the vertical advective trends for diagnostic |
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386 | ! ---------------------------------------------------- |
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387 | IF( l_trdtra ) THEN |
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388 | ! Recompute the vertical advection zta & zsa trends computed |
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389 | ! at the step 2. above in making the difference between the new |
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390 | ! trends and the previous one: ta()/sa - ztrdt()/ztrds() and substract |
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391 | ! the term tn()/sn()*hdivn() to recover the W gradz(T/S) trends |
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392 | |
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393 | DO jk = 1, jpkm1 |
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394 | DO jj = 2, jpjm1 |
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395 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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396 | #if defined key_zco |
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397 | zbtr = btr2(ji,jj) |
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398 | z_hdivn_x = e2u(ji,jj)*pun(ji,jj,jk) - e2u(ji-1,jj)*pun(ji-1,jj,jk) |
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399 | z_hdivn_y = e1v(ji,jj)*pvn(ji,jj,jk) - e1v(ji,jj-1)*pvn(ji,jj-1,jk) |
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400 | #else |
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401 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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402 | z_hdivn_x = e2u(ji,jj)*fse3u(ji,jj,jk)*pun(ji,jj,jk) - e2u(ji-1,jj)*fse3u(ji-1,jj,jk)*pun(ji-1,jj,jk) |
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403 | z_hdivn_y = e1v(ji,jj)*fse3v(ji,jj,jk)*pvn(ji,jj,jk) - e1v(ji,jj-1)*fse3v(ji,jj-1,jk)*pvn(ji,jj-1,jk) |
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404 | #endif |
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405 | z_hdivn = (z_hdivn_x + z_hdivn_y) * zbtr |
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406 | ztrdt(ji,jj,jk) = ta(ji,jj,jk) - ztrdt(ji,jj,jk) - tn(ji,jj,jk) * z_hdivn |
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407 | ztrds(ji,jj,jk) = sa(ji,jj,jk) - ztrds(ji,jj,jk) - sn(ji,jj,jk) * z_hdivn |
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408 | END DO |
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409 | END DO |
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410 | END DO |
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411 | CALL trd_mod(ztrdt, ztrds, jptra_trd_zad, 'TRA', kt) |
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412 | ENDIF |
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413 | |
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414 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ta, clinfo1=' cen2 zad - Ta: ', mask1=tmask, & |
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415 | & tab3d_2=sa, clinfo2= ' Sa: ', mask2=tmask, clinfo3='tra' ) |
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416 | ! |
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417 | END SUBROUTINE tra_adv_cen2 |
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418 | |
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419 | |
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420 | SUBROUTINE ups_orca_set |
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421 | !!---------------------------------------------------------------------- |
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422 | !! *** ROUTINE ups_orca_set *** |
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423 | !! |
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424 | !! ** Purpose : add a portion of upstream scheme in area where the |
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425 | !! centered scheme generates too strong overshoot |
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426 | !! |
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427 | !! ** Method : orca (R4 and R2) confiiguration setting. Set upsmsk |
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428 | !! array to nozero value in some straith. |
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429 | !! |
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430 | !! ** Action : - upsmsk set to 1 at some strait, 0 elsewhere for orca |
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431 | !!---------------------------------------------------------------------- |
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432 | INTEGER :: ii0, ii1, ij0, ij1 ! temporary integers |
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433 | !!---------------------------------------------------------------------- |
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434 | |
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435 | ! mixed upstream/centered scheme near river mouths |
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436 | ! ------------------------------------------------ |
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437 | SELECT CASE ( jp_cfg ) |
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438 | ! ! ======================= |
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439 | CASE ( 4 ) ! ORCA_R4 configuration |
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440 | ! ! ======================= |
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441 | ! ! Gibraltar Strait |
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442 | ii0 = 70 ; ii1 = 71 |
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443 | ij0 = 52 ; ij1 = 53 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.50 |
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444 | ! |
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445 | ! ! ======================= |
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446 | CASE ( 2 ) ! ORCA_R2 configuration |
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447 | ! ! ======================= |
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448 | ! ! Gibraltar Strait |
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449 | ij0 = 102 ; ij1 = 102 |
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450 | ii0 = 138 ; ii1 = 138 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.20 |
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451 | ii0 = 139 ; ii1 = 139 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.40 |
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452 | ii0 = 140 ; ii1 = 140 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.50 |
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453 | ij0 = 101 ; ij1 = 102 |
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454 | ii0 = 141 ; ii1 = 141 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.50 |
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455 | ! ! Bab el Mandeb Strait |
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456 | ij0 = 87 ; ij1 = 88 |
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457 | ii0 = 164 ; ii1 = 164 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.10 |
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458 | ij0 = 88 ; ij1 = 88 |
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459 | ii0 = 163 ; ii1 = 163 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.25 |
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460 | ii0 = 162 ; ii1 = 162 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.40 |
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461 | ii0 = 160 ; ii1 = 161 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.50 |
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462 | ij0 = 89 ; ij1 = 89 |
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463 | ii0 = 158 ; ii1 = 160 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.25 |
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464 | ij0 = 90 ; ij1 = 90 |
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465 | ii0 = 160 ; ii1 = 160 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.25 |
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466 | ! ! Sound Strait |
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467 | ij0 = 116 ; ij1 = 116 |
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468 | ii0 = 144 ; ii1 = 144 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.25 |
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469 | ii0 = 145 ; ii1 = 147 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.50 |
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470 | ii0 = 148 ; ii1 = 148 ; upsmsk( mi0(ii0):mi1(ii1) , mj0(ij0):mj1(ij1) ) = 0.25 |
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471 | ! |
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472 | END SELECT |
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473 | |
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474 | ! mixed upstream/centered scheme over closed seas |
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475 | ! ----------------------------------------------- |
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476 | CALL clo_ups( upsmsk(:,:) ) |
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477 | ! |
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478 | END SUBROUTINE ups_orca_set |
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479 | |
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480 | !!====================================================================== |
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481 | END MODULE traadv_cen2 |
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