[3] | 1 | MODULE traadv_cen2 |
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[719] | 2 | !!============================================================================== |
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| 3 | !! *** MODULE traadv_cen2 *** |
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[3] | 4 | !! Ocean active tracers: horizontal & vertical advective trend |
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[719] | 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 ! 05-11 (V. Garnier) Surface pressure gradient organization |
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| 9 | !! " " ! 06-04 (R. Benshila, G. Madec) Step reorganization |
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[3] | 10 | !!---------------------------------------------------------------------- |
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[503] | 11 | |
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| 12 | !!---------------------------------------------------------------------- |
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[457] | 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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[3] | 16 | !!---------------------------------------------------------------------- |
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| 17 | USE oce ! ocean dynamics and active tracers |
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| 18 | USE dom_oce ! ocean space and time domain |
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[719] | 19 | USE trdmod ! ocean active tracers trends |
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[708] | 20 | USE trdmod_oce ! ocean variables trends |
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[719] | 21 | USE flxrnf ! |
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[3] | 22 | USE trabbl ! advective term in the BBL |
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[74] | 23 | USE ocfzpt ! |
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[3] | 24 | USE lib_mpp |
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[74] | 25 | USE lbclnk ! ocean lateral boundary condition (or mpp link) |
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[719] | 26 | USE in_out_manager ! I/O manager |
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[132] | 27 | USE diaptr ! poleward transport diagnostics |
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[719] | 28 | USE dynspg_oce ! choice/control of key cpp for surface pressure gradient |
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[258] | 29 | USE prtctl ! Print control |
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[3] | 30 | |
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| 31 | IMPLICIT NONE |
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| 32 | PRIVATE |
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| 33 | |
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[719] | 34 | PUBLIC tra_adv_cen2 ! routine called by step.F90 |
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[3] | 35 | |
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[503] | 36 | REAL(wp), DIMENSION(jpi,jpj) :: btr2 ! inverse of T-point surface [1/(e1t*e2t)] |
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| 37 | |
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[3] | 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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[719] | 42 | !! OPA 9.0 , LOCEAN-IPSL (2005) |
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| 43 | !! $Header$ |
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[503] | 44 | !! Software governed by the CeCILL licence (modipsl/doc/NEMO_CeCILL.txt) |
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[3] | 45 | !!---------------------------------------------------------------------- |
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| 46 | |
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| 47 | CONTAINS |
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| 48 | |
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[457] | 49 | SUBROUTINE tra_adv_cen2( kt, pun, pvn, pwn ) |
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[3] | 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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[457] | 59 | !! approaching the freezing point) it is mixed with an upstream |
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[3] | 60 | !! scheme for stability reasons. |
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[457] | 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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[3] | 65 | !! zcenu = e2u*e3u un mi(tn) |
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| 66 | !! zcenv = e1v*e3v vn mj(tn) |
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[457] | 67 | !! * upstream flux: |
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[3] | 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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[457] | 70 | !! * mixed upstream / centered horizontal advection scheme |
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[3] | 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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[457] | 75 | !! * horizontal advective trend (divergence of the fluxes) |
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[3] | 76 | !! zta = 1/(e1t*e2t*e3t) { di-1[zwx] + dj-1[zwy] } |
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[457] | 77 | !! * Add this trend now to the general trend of tracer (ta,sa): |
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[3] | 78 | !! (ta,sa) = (ta,sa) + ( zta , zsa ) |
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[457] | 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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[3] | 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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[457] | 88 | !! NB:in z-coordinate - full step (ln_zco=T) e3u=e3v=e3t, so |
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| 89 | !! they vanish from the expression of the flux and divergence. |
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[3] | 90 | !! |
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| 91 | !! Part II : vertical advection |
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| 92 | !! For temperature (idem for salinity) the advective trend is com- |
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| 93 | !! puted as follows : |
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| 94 | !! zta = 1/e3t dk+1[ zwz ] |
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| 95 | !! where the vertical advective flux, zwz, is given by : |
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| 96 | !! zwz = zcofk * zupst + (1-zcofk) * zcent |
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[457] | 97 | !! with |
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[3] | 98 | !! zupsv = upstream flux = wn * (tb(k) or tb(k-1) ) [wn>0 or <0] |
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| 99 | !! zcenu = centered flux = wn * mk(tn) |
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[457] | 100 | !! The surface boundary condition is : |
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| 101 | !! rigid-lid (lk_dynspg_frd = T) : zero advective flux |
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| 102 | !! free-surf (lk_dynspg_fsc = T) : wn(:,:,1) * tn(:,:,1) |
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[3] | 103 | !! Add this trend now to the general trend of tracer (ta,sa): |
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| 104 | !! (ta,sa) = (ta,sa) + ( zta , zsa ) |
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[457] | 105 | !! Trend diagnostic ('key_trdtra' defined): the trend is |
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| 106 | !! saved for diagnostics. The trends saved is expressed as : |
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[3] | 107 | !! save trend = w.gradz(T) = zta - tn divn. |
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| 108 | !! |
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[457] | 109 | !! ** Action : - update (ta,sa) with the now advective tracer trends |
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[503] | 110 | !! - save trends in (ztrdt,ztrds) ('key_trdtra') |
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| 111 | !!---------------------------------------------------------------------- |
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| 112 | USE oce, ONLY : zwx => ua ! use ua as workspace |
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| 113 | USE oce, ONLY : zwy => va ! use va as workspace |
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[3] | 114 | !! |
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[503] | 115 | INTEGER , INTENT(in) :: kt ! ocean time-step index |
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| 116 | REAL(wp), INTENT(in), DIMENSION(jpi,jpj,jpk) :: pun ! ocean velocity u-component |
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| 117 | REAL(wp), INTENT(in), DIMENSION(jpi,jpj,jpk) :: pvn ! ocean velocity v-component |
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| 118 | REAL(wp), INTENT(in), DIMENSION(jpi,jpj,jpk) :: pwn ! ocean velocity w-component |
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| 119 | !! |
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| 120 | INTEGER :: ji, jj, jk ! dummy loop indices |
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[719] | 121 | REAL(wp) :: & |
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| 122 | zbtr, zta, zsa, zfui, zfvj, & ! temporary scalars |
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| 123 | zhw, ze3tr, zcofi, zcofj, & ! " " |
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| 124 | zupsut, zupsvt, zupsus, zupsvs, & ! " " |
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| 125 | zfp_ui, zfp_vj, zfm_ui, zfm_vj, & ! " " |
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| 126 | zcofk, zupst, zupss, zcent, & ! " " |
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| 127 | zcens, zfp_w, zfm_w, & ! " " |
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| 128 | zcenut, zcenvt, zcenus, zcenvs, & ! " " |
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| 129 | z_hdivn_x, z_hdivn_y, z_hdivn |
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| 130 | REAL(wp), DIMENSION(jpi,jpj,jpk) :: zwz, ztrdt, zind ! 3D workspace |
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[503] | 131 | REAL(wp), DIMENSION(jpi,jpj,jpk) :: zww, ztrds ! " " |
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[3] | 132 | !!---------------------------------------------------------------------- |
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| 133 | |
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| 134 | IF( kt == nit000 ) THEN |
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| 135 | IF(lwp) WRITE(numout,*) |
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| 136 | IF(lwp) WRITE(numout,*) 'tra_adv_cen2 : 2nd order centered advection scheme' |
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| 137 | IF(lwp) WRITE(numout,*) '~~~~~~~~~~~~ Vector optimization case' |
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| 138 | IF(lwp) WRITE(numout,*) |
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[719] | 139 | ! |
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| 140 | btr2(:,:) = 1. / ( e1t(:,:) * e2t(:,:) ) |
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[3] | 141 | ENDIF |
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| 142 | |
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| 143 | ! Upstream / centered scheme indicator |
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| 144 | ! ------------------------------------ |
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| 145 | DO jk = 1, jpk |
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| 146 | DO jj = 1, jpj |
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| 147 | DO ji = 1, jpi |
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[719] | 148 | zind(ji,jj,jk) = MAX ( upsrnfh(ji,jj) * upsrnfz(jk), & ! changing advection scheme near runoff |
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| 149 | & upsadv(ji,jj) & ! in the vicinity of some straits |
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[3] | 150 | #if defined key_ice_lim |
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[719] | 151 | & , tmask(ji,jj,jk) & ! half upstream tracer fluxes |
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| 152 | & * MAX( 0., SIGN( 1., fzptn(ji,jj) & ! if tn < ("freezing"+0.1 ) |
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| 153 | & +0.1-tn(ji,jj,jk) ) ) & |
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[3] | 154 | #endif |
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| 155 | & ) |
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| 156 | END DO |
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| 157 | END DO |
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| 158 | END DO |
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| 159 | |
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[719] | 160 | |
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| 161 | ! Horizontal advective fluxes |
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| 162 | ! ----------------------------- |
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[3] | 163 | ! ! =============== |
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| 164 | DO jk = 1, jpkm1 ! Horizontal slab |
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| 165 | ! ! =============== |
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| 166 | DO jj = 1, jpjm1 |
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| 167 | DO ji = 1, fs_jpim1 ! vector opt. |
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| 168 | ! upstream indicator |
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| 169 | zcofi = MAX( zind(ji+1,jj,jk), zind(ji,jj,jk) ) |
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| 170 | zcofj = MAX( zind(ji,jj+1,jk), zind(ji,jj,jk) ) |
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| 171 | ! volume fluxes * 1/2 |
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[457] | 172 | #if defined key_zco |
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| 173 | zfui = 0.5 * e2u(ji,jj) * pun(ji,jj,jk) |
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| 174 | zfvj = 0.5 * e1v(ji,jj) * pvn(ji,jj,jk) |
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[3] | 175 | #else |
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[457] | 176 | zfui = 0.5 * e2u(ji,jj) * fse3u(ji,jj,jk) * pun(ji,jj,jk) |
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| 177 | zfvj = 0.5 * e1v(ji,jj) * fse3v(ji,jj,jk) * pvn(ji,jj,jk) |
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[3] | 178 | #endif |
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| 179 | ! upstream scheme |
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| 180 | zfp_ui = zfui + ABS( zfui ) |
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| 181 | zfp_vj = zfvj + ABS( zfvj ) |
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| 182 | zfm_ui = zfui - ABS( zfui ) |
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| 183 | zfm_vj = zfvj - ABS( zfvj ) |
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| 184 | zupsut = zfp_ui * tb(ji,jj,jk) + zfm_ui * tb(ji+1,jj ,jk) |
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| 185 | zupsvt = zfp_vj * tb(ji,jj,jk) + zfm_vj * tb(ji ,jj+1,jk) |
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| 186 | zupsus = zfp_ui * sb(ji,jj,jk) + zfm_ui * sb(ji+1,jj ,jk) |
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| 187 | zupsvs = zfp_vj * sb(ji,jj,jk) + zfm_vj * sb(ji ,jj+1,jk) |
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| 188 | ! centered scheme |
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| 189 | zcenut = zfui * ( tn(ji,jj,jk) + tn(ji+1,jj ,jk) ) |
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| 190 | zcenvt = zfvj * ( tn(ji,jj,jk) + tn(ji ,jj+1,jk) ) |
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| 191 | zcenus = zfui * ( sn(ji,jj,jk) + sn(ji+1,jj ,jk) ) |
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| 192 | zcenvs = zfvj * ( sn(ji,jj,jk) + sn(ji ,jj+1,jk) ) |
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| 193 | ! mixed centered / upstream scheme |
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| 194 | zwx(ji,jj,jk) = zcofi * zupsut + (1.-zcofi) * zcenut |
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| 195 | zwy(ji,jj,jk) = zcofj * zupsvt + (1.-zcofj) * zcenvt |
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| 196 | zww(ji,jj,jk) = zcofi * zupsus + (1.-zcofi) * zcenus |
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| 197 | zwz(ji,jj,jk) = zcofj * zupsvs + (1.-zcofj) * zcenvs |
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| 198 | END DO |
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| 199 | END DO |
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| 200 | |
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[503] | 201 | ! Tracer flux divergence at t-point added to the general trend |
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| 202 | ! -------------------------------------------------------------- |
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[3] | 203 | DO jj = 2, jpjm1 |
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| 204 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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[457] | 205 | #if defined key_zco |
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[503] | 206 | zbtr = btr2(ji,jj) |
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[457] | 207 | #else |
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[503] | 208 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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[3] | 209 | #endif |
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[719] | 210 | ! horizontal advective trends |
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| 211 | zta = - zbtr * ( zwx(ji,jj,jk) - zwx(ji-1,jj ,jk) & |
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[3] | 212 | & + zwy(ji,jj,jk) - zwy(ji ,jj-1,jk) ) |
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| 213 | zsa = - zbtr * ( zww(ji,jj,jk) - zww(ji-1,jj ,jk) & |
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| 214 | & + zwz(ji,jj,jk) - zwz(ji ,jj-1,jk) ) |
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[719] | 215 | ! add it to the general tracer trends |
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| 216 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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[3] | 217 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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| 218 | END DO |
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| 219 | END DO |
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| 220 | ! ! =============== |
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| 221 | END DO ! End of slab |
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| 222 | ! ! =============== |
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| 223 | |
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[503] | 224 | ! Save the horizontal advective trends for diagnostic |
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| 225 | ! ----------------------------------------------------- |
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| 226 | IF( l_trdtra ) THEN |
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| 227 | ! T/S ZONAL advection trends |
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| 228 | ztrdt(:,:,:) = 0.e0 ; ztrds(:,:,:) = 0.e0 |
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| 229 | ! |
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| 230 | DO jk = 1, jpkm1 |
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| 231 | DO jj = 2, jpjm1 |
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| 232 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| 233 | !-- Compute zonal divergence by splitting hdivn (see divcur.F90) |
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| 234 | ! N.B. This computation is not valid along OBCs (if any) |
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| 235 | #if defined key_zco |
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| 236 | zbtr = btr2(ji,jj) |
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| 237 | z_hdivn_x = ( e2u(ji ,jj) * pun(ji ,jj,jk) & |
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| 238 | & - e2u(ji-1,jj) * pun(ji-1,jj,jk) ) * zbtr |
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| 239 | #else |
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| 240 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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| 241 | z_hdivn_x = ( e2u(ji ,jj) * fse3u(ji ,jj,jk) * pun(ji ,jj,jk) & |
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| 242 | & - e2u(ji-1,jj) * fse3u(ji-1,jj,jk) * pun(ji-1,jj,jk) ) * zbtr |
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| 243 | #endif |
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| 244 | 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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| 245 | 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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| 246 | END DO |
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| 247 | END DO |
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| 248 | END DO |
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| 249 | CALL trd_mod(ztrdt, ztrds, jptra_trd_xad, 'TRA', kt) |
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| 250 | ! |
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| 251 | ! T/S MERIDIONAL advection trends |
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| 252 | DO jk = 1, jpkm1 |
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| 253 | DO jj = 2, jpjm1 |
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| 254 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| 255 | !-- Compute merid. divergence by splitting hdivn (see divcur.F90) |
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| 256 | ! N.B. This computation is not valid along OBCs (if any) |
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| 257 | #if defined key_zco |
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| 258 | zbtr = btr2(ji,jj) |
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| 259 | z_hdivn_y = ( e1v(ji,jj ) * pvn(ji,jj ,jk) & |
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| 260 | & - e1v(ji,jj-1) * pvn(ji,jj-1,jk) ) * zbtr |
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| 261 | #else |
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| 262 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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| 263 | z_hdivn_y = ( e1v(ji, jj) * fse3v(ji,jj ,jk) * pvn(ji,jj ,jk) & |
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| 264 | & - e1v(ji,jj-1) * fse3v(ji,jj-1,jk) * pvn(ji,jj-1,jk) ) * zbtr |
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| 265 | #endif |
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| 266 | 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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| 267 | 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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| 268 | END DO |
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| 269 | END DO |
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| 270 | END DO |
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| 271 | CALL trd_mod(ztrdt, ztrds, jptra_trd_yad, 'TRA', kt) |
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| 272 | ! |
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| 273 | ! Save the horizontal up-to-date ta/sa trends |
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| 274 | ztrdt(:,:,:) = ta(:,:,:) |
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| 275 | ztrds(:,:,:) = sa(:,:,:) |
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[216] | 276 | ENDIF |
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| 277 | |
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[457] | 278 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ta, clinfo1=' cen2 had - Ta: ', mask1=tmask, & |
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| 279 | & tab3d_2=sa, clinfo2= ' Sa: ', mask2=tmask, clinfo3='tra' ) |
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[3] | 280 | |
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[719] | 281 | ! 4. "zonal" mean advective heat and salt transport |
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| 282 | ! ------------------------------------------------- |
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| 283 | |
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[132] | 284 | IF( ln_diaptr .AND. ( MOD( kt, nf_ptr ) == 0 ) ) THEN |
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[457] | 285 | IF( lk_zco ) THEN |
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| 286 | DO jk = 1, jpkm1 |
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| 287 | DO jj = 2, jpjm1 |
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| 288 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| 289 | zwy(ji,jj,jk) = zwy(ji,jj,jk) * fse3v(ji,jj,jk) |
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| 290 | zwz(ji,jj,jk) = zwz(ji,jj,jk) * fse3v(ji,jj,jk) |
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| 291 | END DO |
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[3] | 292 | END DO |
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| 293 | END DO |
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[457] | 294 | ENDIF |
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[132] | 295 | pht_adv(:) = ptr_vj( zwy(:,:,:) ) |
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| 296 | pst_adv(:) = ptr_vj( zwz(:,:,:) ) |
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[3] | 297 | ENDIF |
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| 298 | |
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| 299 | ! II. Vertical advection |
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| 300 | ! ---------------------- |
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| 301 | |
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| 302 | ! Bottom value : flux set to zero |
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| 303 | zwx(:,:,jpk) = 0.e0 ; zwy(:,:,jpk) = 0.e0 |
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| 304 | |
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| 305 | ! Surface value |
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[592] | 306 | IF( lk_dynspg_rl .OR. lk_vvl ) THEN |
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| 307 | ! rigid lid or variable volume: flux set to zero |
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[359] | 308 | zwx(:,:, 1 ) = 0.e0 ; zwy(:,:, 1 ) = 0.e0 |
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| 309 | ELSE |
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| 310 | ! free surface |
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[457] | 311 | zwx(:,:, 1 ) = pwn(:,:,1) * tn(:,:,1) |
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| 312 | zwy(:,:, 1 ) = pwn(:,:,1) * sn(:,:,1) |
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[200] | 313 | ENDIF |
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[3] | 314 | |
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[719] | 315 | ! 1. Vertical advective fluxes |
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[3] | 316 | ! ---------------------------- |
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[719] | 317 | ! Second order centered tracer flux at w-point |
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[3] | 318 | DO jk = 2, jpk |
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| 319 | DO jj = 2, jpjm1 |
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| 320 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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[719] | 321 | ! upstream indicator |
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| 322 | zcofk = MAX( zind(ji,jj,jk-1), zind(ji,jj,jk) ) |
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| 323 | ! velocity * 1/2 |
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| 324 | zhw = 0.5 * pwn(ji,jj,jk) |
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| 325 | ! upstream scheme |
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| 326 | zfp_w = zhw + ABS( zhw ) |
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[3] | 327 | zfm_w = zhw - ABS( zhw ) |
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| 328 | zupst = zfp_w * tb(ji,jj,jk) + zfm_w * tb(ji,jj,jk-1) |
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| 329 | zupss = zfp_w * sb(ji,jj,jk) + zfm_w * sb(ji,jj,jk-1) |
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[719] | 330 | ! centered scheme |
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| 331 | zcent = zhw * ( tn(ji,jj,jk) + tn(ji,jj,jk-1) ) |
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[3] | 332 | zcens = zhw * ( sn(ji,jj,jk) + sn(ji,jj,jk-1) ) |
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[719] | 333 | ! mixed centered / upstream scheme |
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| 334 | zwx(ji,jj,jk) = zcofk * zupst + (1.-zcofk) * zcent |
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[3] | 335 | zwy(ji,jj,jk) = zcofk * zupss + (1.-zcofk) * zcens |
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| 336 | END DO |
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| 337 | END DO |
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| 338 | END DO |
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| 339 | |
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| 340 | ! 2. Tracer flux divergence at t-point added to the general trend |
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| 341 | ! ------------------------- |
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| 342 | DO jk = 1, jpkm1 |
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| 343 | DO jj = 2, jpjm1 |
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| 344 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| 345 | ze3tr = 1. / fse3t(ji,jj,jk) |
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[719] | 346 | ! vertical advective trends |
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| 347 | zta = - ze3tr * ( zwx(ji,jj,jk) - zwx(ji,jj,jk+1) ) |
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[3] | 348 | zsa = - ze3tr * ( zwy(ji,jj,jk) - zwy(ji,jj,jk+1) ) |
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[719] | 349 | ! add it to the general tracer trends |
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| 350 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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[3] | 351 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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| 352 | END DO |
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| 353 | END DO |
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| 354 | END DO |
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| 355 | |
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[216] | 356 | ! 3. Save the vertical advective trends for diagnostic |
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| 357 | ! ---------------------------------------------------- |
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| 358 | IF( l_trdtra ) THEN |
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| 359 | ! Recompute the vertical advection zta & zsa trends computed |
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| 360 | ! at the step 2. above in making the difference between the new |
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[503] | 361 | ! trends and the previous one: ta()/sa - ztrdt()/ztrds() and substract |
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[216] | 362 | ! the term tn()/sn()*hdivn() to recover the W gradz(T/S) trends |
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| 363 | |
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[503] | 364 | DO jk = 1, jpkm1 |
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| 365 | DO jj = 2, jpjm1 |
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| 366 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| 367 | #if defined key_zco |
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| 368 | zbtr = btr2(ji,jj) |
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| 369 | z_hdivn_x = e2u(ji,jj)*pun(ji,jj,jk) - e2u(ji-1,jj)*pun(ji-1,jj,jk) |
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| 370 | z_hdivn_y = e1v(ji,jj)*pvn(ji,jj,jk) - e1v(ji,jj-1)*pvn(ji,jj-1,jk) |
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| 371 | #else |
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| 372 | zbtr = btr2(ji,jj) / fse3t(ji,jj,jk) |
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| 373 | 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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| 374 | 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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| 375 | #endif |
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| 376 | z_hdivn = (z_hdivn_x + z_hdivn_y) * zbtr |
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| 377 | ztrdt(ji,jj,jk) = ta(ji,jj,jk) - ztrdt(ji,jj,jk) - tn(ji,jj,jk) * z_hdivn |
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| 378 | ztrds(ji,jj,jk) = sa(ji,jj,jk) - ztrds(ji,jj,jk) - sn(ji,jj,jk) * z_hdivn |
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| 379 | END DO |
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| 380 | END DO |
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| 381 | END DO |
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| 382 | CALL trd_mod(ztrdt, ztrds, jptra_trd_zad, 'TRA', kt) |
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[216] | 383 | ENDIF |
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| 384 | |
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[457] | 385 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ta, clinfo1=' cen2 zad - Ta: ', mask1=tmask, & |
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| 386 | & tab3d_2=sa, clinfo2= ' Sa: ', mask2=tmask, clinfo3='tra' ) |
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[503] | 387 | ! |
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[3] | 388 | END SUBROUTINE tra_adv_cen2 |
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| 389 | |
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| 390 | !!====================================================================== |
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| 391 | END MODULE traadv_cen2 |
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