[1565] | 1 | MODULE sshwzv |
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[3] | 2 | !!============================================================================== |
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[1438] | 3 | !! *** MODULE sshwzv *** |
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| 4 | !! Ocean dynamics : sea surface height and vertical velocity |
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[3] | 5 | !!============================================================================== |
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[1438] | 6 | !! History : 3.1 ! 2009-02 (G. Madec, M. Leclair) Original code |
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[2148] | 7 | !! 3.3 ! 2010-04 (M. Leclair, G. Madec) modified LF-RA |
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[2236] | 8 | !! - ! 2010-05 (K. Mogensen, A. Weaver, M. Martin, D. Lea) Assimilation interface |
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| 9 | !! - ! 2010-09 (D.Storkey and E.O'Dea) bug fixes for BDY module |
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[3] | 10 | !!---------------------------------------------------------------------- |
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[1438] | 11 | |
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[3] | 12 | !!---------------------------------------------------------------------- |
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[1438] | 13 | !! ssh_wzv : after ssh & now vertical velocity |
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| 14 | !! ssh_nxt : filter ans swap the ssh arrays |
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| 15 | !!---------------------------------------------------------------------- |
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[3] | 16 | USE oce ! ocean dynamics and tracers variables |
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| 17 | USE dom_oce ! ocean space and time domain variables |
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[888] | 18 | USE sbc_oce ! surface boundary condition: ocean |
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| 19 | USE domvvl ! Variable volume |
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[1565] | 20 | USE divcur ! hor. divergence and curl (div & cur routines) |
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[1438] | 21 | USE iom ! I/O library |
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| 22 | USE restart ! only for lrst_oce |
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[3] | 23 | USE in_out_manager ! I/O manager |
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[258] | 24 | USE prtctl ! Print control |
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[592] | 25 | USE phycst |
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| 26 | USE lbclnk ! ocean lateral boundary condition (or mpp link) |
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[1241] | 27 | USE obc_par ! open boundary cond. parameter |
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| 28 | USE obc_oce |
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[2236] | 29 | USE bdy_oce |
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[1756] | 30 | USE diaar5, ONLY : lk_diaar5 |
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[1482] | 31 | USE iom |
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[2236] | 32 | USE sbcrnf, ONLY : h_rnf, nk_rnf ! River runoff |
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[2487] | 33 | #if defined key_agrif |
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| 34 | USE agrif_opa_update |
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| 35 | USE agrif_opa_interp |
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| 36 | #endif |
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[2236] | 37 | #if defined key_asminc |
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| 38 | USE asminc ! Assimilation increment |
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| 39 | #endif |
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[592] | 40 | |
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[3] | 41 | IMPLICIT NONE |
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| 42 | PRIVATE |
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| 43 | |
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[1438] | 44 | PUBLIC ssh_wzv ! called by step.F90 |
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| 45 | PUBLIC ssh_nxt ! called by step.F90 |
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[3] | 46 | |
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| 47 | !! * Substitutions |
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| 48 | # include "domzgr_substitute.h90" |
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[1438] | 49 | # include "vectopt_loop_substitute.h90" |
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[3] | 50 | !!---------------------------------------------------------------------- |
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[2287] | 51 | !! NEMO/OPA 3.3 , NEMO Consortium (2010) |
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[888] | 52 | !! $Id$ |
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[2287] | 53 | !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt) |
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[592] | 54 | !!---------------------------------------------------------------------- |
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[3] | 55 | |
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| 56 | CONTAINS |
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| 57 | |
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[1438] | 58 | SUBROUTINE ssh_wzv( kt ) |
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[3] | 59 | !!---------------------------------------------------------------------- |
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[1438] | 60 | !! *** ROUTINE ssh_wzv *** |
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| 61 | !! |
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| 62 | !! ** Purpose : compute the after ssh (ssha), the now vertical velocity |
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| 63 | !! and update the now vertical coordinate (lk_vvl=T). |
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[3] | 64 | !! |
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[2148] | 65 | !! ** Method : - Using the incompressibility hypothesis, the vertical |
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[1438] | 66 | !! velocity is computed by integrating the horizontal divergence |
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| 67 | !! from the bottom to the surface minus the scale factor evolution. |
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| 68 | !! The boundary conditions are w=0 at the bottom (no flux) and. |
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[3] | 69 | !! |
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[1438] | 70 | !! ** action : ssha : after sea surface height |
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| 71 | !! wn : now vertical velocity |
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[2148] | 72 | !! sshu_a, sshv_a, sshf_a : after sea surface height (lk_vvl=T) |
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| 73 | !! hu, hv, hur, hvr : ocean depth and its inverse at u-,v-points |
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| 74 | !! |
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| 75 | !! Reference : Leclair, M., and G. Madec, 2009, Ocean Modelling. |
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[3] | 76 | !!---------------------------------------------------------------------- |
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[1756] | 77 | USE oce, ONLY : z3d => ta ! use ta as 3D workspace |
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| 78 | !! |
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[1438] | 79 | INTEGER, INTENT(in) :: kt ! time step |
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| 80 | !! |
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| 81 | INTEGER :: ji, jj, jk ! dummy loop indices |
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| 82 | REAL(wp) :: zcoefu, zcoefv, zcoeff ! temporary scalars |
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[2148] | 83 | REAL(wp) :: z2dt, z1_2dt, z1_rau0 ! temporary scalars |
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[1438] | 84 | REAL(wp), DIMENSION(jpi,jpj) :: zhdiv ! 2D workspace |
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[1756] | 85 | REAL(wp), DIMENSION(jpi,jpj) :: z2d ! 2D workspace |
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[3] | 86 | !!---------------------------------------------------------------------- |
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| 87 | |
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| 88 | IF( kt == nit000 ) THEN |
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[2148] | 89 | ! |
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[3] | 90 | IF(lwp) WRITE(numout,*) |
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[1438] | 91 | IF(lwp) WRITE(numout,*) 'ssh_wzv : after sea surface height and now vertical velocity ' |
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| 92 | IF(lwp) WRITE(numout,*) '~~~~~~~ ' |
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| 93 | ! |
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| 94 | wn(:,:,jpk) = 0.e0 ! bottom boundary condition: w=0 (set once for all) |
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| 95 | ! |
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| 96 | IF( lk_vvl ) THEN ! before and now Sea SSH at u-, v-, f-points (vvl case only) |
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| 97 | DO jj = 1, jpjm1 |
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| 98 | DO ji = 1, jpim1 ! caution: use of Vector Opt. not possible |
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| 99 | zcoefu = 0.5 * umask(ji,jj,1) / ( e1u(ji,jj) * e2u(ji,jj) ) |
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| 100 | zcoefv = 0.5 * vmask(ji,jj,1) / ( e1v(ji,jj) * e2v(ji,jj) ) |
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| 101 | zcoeff = 0.25 * umask(ji,jj,1) * umask(ji,jj+1,1) |
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| 102 | sshu_b(ji,jj) = zcoefu * ( e1t(ji ,jj) * e2t(ji ,jj) * sshb(ji ,jj) & |
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| 103 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * sshb(ji+1,jj) ) |
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| 104 | sshv_b(ji,jj) = zcoefv * ( e1t(ji,jj ) * e2t(ji,jj ) * sshb(ji,jj ) & |
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| 105 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * sshb(ji,jj+1) ) |
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| 106 | sshu_n(ji,jj) = zcoefu * ( e1t(ji ,jj) * e2t(ji ,jj) * sshn(ji ,jj) & |
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| 107 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * sshn(ji+1,jj) ) |
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| 108 | sshv_n(ji,jj) = zcoefv * ( e1t(ji,jj ) * e2t(ji,jj ) * sshn(ji,jj ) & |
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| 109 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * sshn(ji,jj+1) ) |
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| 110 | END DO |
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| 111 | END DO |
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| 112 | CALL lbc_lnk( sshu_b, 'U', 1. ) ; CALL lbc_lnk( sshu_n, 'U', 1. ) |
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| 113 | CALL lbc_lnk( sshv_b, 'V', 1. ) ; CALL lbc_lnk( sshv_n, 'V', 1. ) |
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[2148] | 114 | DO jj = 1, jpjm1 |
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| 115 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 116 | sshf_n(ji,jj) = 0.5 * umask(ji,jj,1) * umask(ji,jj+1,1) & |
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| 117 | & / ( e1f(ji,jj ) * e2f(ji,jj ) ) & |
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| 118 | & * ( e1u(ji,jj ) * e2u(ji,jj ) * sshu_n(ji,jj ) & |
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| 119 | & + e1u(ji,jj+1) * e2u(ji,jj+1) * sshu_n(ji,jj+1) ) |
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| 120 | END DO |
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| 121 | END DO |
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| 122 | CALL lbc_lnk( sshf_n, 'F', 1. ) |
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[1438] | 123 | ENDIF |
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| 124 | ! |
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[3] | 125 | ENDIF |
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| 126 | |
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[2148] | 127 | ! !------------------------------------------! |
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| 128 | IF( lk_vvl ) THEN ! Regridding: Update Now Vertical coord. ! (only in vvl case) |
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| 129 | ! !------------------------------------------! |
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[1565] | 130 | DO jk = 1, jpkm1 |
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[2148] | 131 | fsdept(:,:,jk) = fsdept_n(:,:,jk) ! now local depths stored in fsdep. arrays |
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[1565] | 132 | fsdepw(:,:,jk) = fsdepw_n(:,:,jk) |
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| 133 | fsde3w(:,:,jk) = fsde3w_n(:,:,jk) |
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| 134 | ! |
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[2148] | 135 | fse3t (:,:,jk) = fse3t_n (:,:,jk) ! vertical scale factors stored in fse3. arrays |
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[1565] | 136 | fse3u (:,:,jk) = fse3u_n (:,:,jk) |
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| 137 | fse3v (:,:,jk) = fse3v_n (:,:,jk) |
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| 138 | fse3f (:,:,jk) = fse3f_n (:,:,jk) |
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| 139 | fse3w (:,:,jk) = fse3w_n (:,:,jk) |
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| 140 | fse3uw(:,:,jk) = fse3uw_n(:,:,jk) |
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| 141 | fse3vw(:,:,jk) = fse3vw_n(:,:,jk) |
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| 142 | END DO |
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[2148] | 143 | ! |
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| 144 | hu(:,:) = hu_0(:,:) + sshu_n(:,:) ! now ocean depth (at u- and v-points) |
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[1565] | 145 | hv(:,:) = hv_0(:,:) + sshv_n(:,:) |
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[2148] | 146 | ! ! now masked inverse of the ocean depth (at u- and v-points) |
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[1565] | 147 | hur(:,:) = umask(:,:,1) / ( hu(:,:) + 1.e0 - umask(:,:,1) ) |
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| 148 | hvr(:,:) = vmask(:,:,1) / ( hv(:,:) + 1.e0 - vmask(:,:,1) ) |
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[2236] | 149 | ! |
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[1565] | 150 | ENDIF |
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[2148] | 151 | ! |
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[2392] | 152 | CALL div_cur( kt ) ! Horizontal divergence & Relative vorticity |
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| 153 | ! |
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[2148] | 154 | z2dt = 2. * rdt ! set time step size (Euler/Leapfrog) |
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[1607] | 155 | IF( neuler == 0 .AND. kt == nit000 ) z2dt =rdt |
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[3] | 156 | |
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[1438] | 157 | ! !------------------------------! |
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| 158 | ! ! After Sea Surface Height ! |
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| 159 | ! !------------------------------! |
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| 160 | zhdiv(:,:) = 0.e0 |
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| 161 | DO jk = 1, jpkm1 ! Horizontal divergence of barotropic transports |
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| 162 | zhdiv(:,:) = zhdiv(:,:) + fse3t(:,:,jk) * hdivn(:,:,jk) |
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| 163 | END DO |
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| 164 | ! ! Sea surface elevation time stepping |
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[2148] | 165 | ! In forward Euler time stepping case, the same formulation as in the leap-frog case can be used |
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[2266] | 166 | ! because emp_b field is initialized with the vlaues of emp field. Hence, 0.5 * ( emp + emp_b ) = emp |
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[2148] | 167 | z1_rau0 = 0.5 / rau0 |
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[2266] | 168 | ssha(:,:) = ( sshb(:,:) - z2dt * ( z1_rau0 * ( emp_b(:,:) + emp(:,:) ) + zhdiv(:,:) ) ) & |
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[2148] | 169 | & * tmask(:,:,1) |
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[1438] | 170 | |
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[2487] | 171 | #if defined key_agrif |
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| 172 | CALL agrif_ssh(kt) |
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| 173 | #endif |
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[1438] | 174 | #if defined key_obc |
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[2148] | 175 | IF( Agrif_Root() ) THEN |
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[1438] | 176 | ssha(:,:) = ssha(:,:) * obctmsk(:,:) |
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[2148] | 177 | CALL lbc_lnk( ssha, 'T', 1. ) ! absolutly compulsory !! (jmm) |
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[1438] | 178 | ENDIF |
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| 179 | #endif |
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[2236] | 180 | #if defined key_bdy |
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| 181 | ssha(:,:) = ssha(:,:) * bdytmask(:,:) |
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| 182 | CALL lbc_lnk( ssha, 'T', 1. ) |
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| 183 | #endif |
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| 184 | |
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[1438] | 185 | ! ! Sea Surface Height at u-,v- and f-points (vvl case only) |
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| 186 | IF( lk_vvl ) THEN ! (required only in key_vvl case) |
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| 187 | DO jj = 1, jpjm1 |
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[1694] | 188 | DO ji = 1, jpim1 ! NO Vector Opt. |
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[1438] | 189 | sshu_a(ji,jj) = 0.5 * umask(ji,jj,1) / ( e1u(ji ,jj) * e2u(ji ,jj) ) & |
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| 190 | & * ( e1t(ji ,jj) * e2t(ji ,jj) * ssha(ji ,jj) & |
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| 191 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * ssha(ji+1,jj) ) |
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| 192 | sshv_a(ji,jj) = 0.5 * vmask(ji,jj,1) / ( e1v(ji,jj ) * e2v(ji,jj ) ) & |
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| 193 | & * ( e1t(ji,jj ) * e2t(ji,jj ) * ssha(ji,jj ) & |
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| 194 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * ssha(ji,jj+1) ) |
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[592] | 195 | END DO |
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| 196 | END DO |
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[2148] | 197 | ! Boundaries conditions |
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| 198 | CALL lbc_lnk( sshu_a, 'U', 1. ) |
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[1438] | 199 | CALL lbc_lnk( sshv_a, 'V', 1. ) |
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| 200 | ENDIF |
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[2236] | 201 | ! Include the IAU weighted SSH increment |
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| 202 | #if defined key_asminc |
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| 203 | IF( ( lk_asminc ).AND.( ln_sshinc ).AND.( ln_asmiau ) ) THEN |
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| 204 | CALL ssh_asm_inc( kt ) |
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| 205 | ssha(:,:) = ssha(:,:) + z2dt * ssh_iau(:,:) |
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| 206 | ENDIF |
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| 207 | #endif |
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| 208 | |
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[1438] | 209 | ! !------------------------------! |
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| 210 | ! ! Now Vertical Velocity ! |
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| 211 | ! !------------------------------! |
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[2148] | 212 | z1_2dt = 1.e0 / z2dt |
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| 213 | DO jk = jpkm1, 1, -1 ! integrate from the bottom the hor. divergence |
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| 214 | ! - ML - need 3 lines here because replacement of fse3t by its expression yields too long lines otherwise |
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| 215 | wn(:,:,jk) = wn(:,:,jk+1) - fse3t_n(:,:,jk) * hdivn(:,:,jk) & |
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| 216 | & - ( fse3t_a(:,:,jk) - fse3t_b(:,:,jk) ) & |
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| 217 | & * tmask(:,:,jk) * z1_2dt |
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[2236] | 218 | #if defined key_bdy |
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| 219 | wn(:,:,jk) = wn(:,:,jk) * bdytmask(:,:) |
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| 220 | #endif |
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[1438] | 221 | END DO |
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[2148] | 222 | |
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| 223 | ! !------------------------------! |
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| 224 | ! ! outputs ! |
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| 225 | ! !------------------------------! |
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[1756] | 226 | CALL iom_put( "woce", wn ) ! vertical velocity |
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| 227 | CALL iom_put( "ssh" , sshn ) ! sea surface height |
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| 228 | CALL iom_put( "ssh2", sshn(:,:) * sshn(:,:) ) ! square of sea surface height |
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[2148] | 229 | IF( lk_diaar5 ) THEN ! vertical mass transport & its square value |
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| 230 | ! Caution: in the VVL case, it only correponds to the baroclinic mass transport. |
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[1756] | 231 | z2d(:,:) = rau0 * e1t(:,:) * e2t(:,:) |
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| 232 | DO jk = 1, jpk |
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| 233 | z3d(:,:,jk) = wn(:,:,jk) * z2d(:,:) |
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| 234 | END DO |
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[2148] | 235 | CALL iom_put( "w_masstr" , z3d ) |
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| 236 | CALL iom_put( "w_masstr2", z3d(:,:,:) * z3d(:,:,:) ) |
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[1756] | 237 | ENDIF |
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[1438] | 238 | ! |
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[2148] | 239 | IF(ln_ctl) CALL prt_ctl( tab2d_1=ssha, clinfo1=' ssha - : ', mask1=tmask, ovlap=1 ) |
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| 240 | ! |
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[1438] | 241 | END SUBROUTINE ssh_wzv |
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[592] | 242 | |
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| 243 | |
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[1438] | 244 | SUBROUTINE ssh_nxt( kt ) |
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| 245 | !!---------------------------------------------------------------------- |
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| 246 | !! *** ROUTINE ssh_nxt *** |
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| 247 | !! |
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| 248 | !! ** Purpose : achieve the sea surface height time stepping by |
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| 249 | !! applying Asselin time filter and swapping the arrays |
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| 250 | !! ssha already computed in ssh_wzv |
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| 251 | !! |
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[2148] | 252 | !! ** Method : - apply Asselin time fiter to now ssh (excluding the forcing |
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| 253 | !! from the filter, see Leclair and Madec 2010) and swap : |
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| 254 | !! sshn = ssha + atfp * ( sshb -2 sshn + ssha ) |
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| 255 | !! - atfp * rdt * ( emp_b - emp ) / rau0 |
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| 256 | !! sshn = ssha |
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[1438] | 257 | !! |
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| 258 | !! ** action : - sshb, sshn : before & now sea surface height |
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| 259 | !! ready for the next time step |
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[2148] | 260 | !! |
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| 261 | !! Reference : Leclair, M., and G. Madec, 2009, Ocean Modelling. |
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[1438] | 262 | !!---------------------------------------------------------------------- |
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[2148] | 263 | INTEGER, INTENT(in) :: kt ! ocean time-step index |
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[1438] | 264 | !! |
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[2148] | 265 | INTEGER :: ji, jj ! dummy loop indices |
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| 266 | REAL(wp) :: zec ! temporary scalar |
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[1438] | 267 | !!---------------------------------------------------------------------- |
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[592] | 268 | |
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[1438] | 269 | IF( kt == nit000 ) THEN |
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| 270 | IF(lwp) WRITE(numout,*) |
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| 271 | IF(lwp) WRITE(numout,*) 'ssh_nxt : next sea surface height (Asselin time filter + swap)' |
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| 272 | IF(lwp) WRITE(numout,*) '~~~~~~~ ' |
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| 273 | ENDIF |
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[592] | 274 | |
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[2148] | 275 | ! !--------------------------! |
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| 276 | IF( lk_vvl ) THEN ! Variable volume levels ! |
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| 277 | ! !--------------------------! |
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| 278 | ! |
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| 279 | ! ssh at t-, u-, v, f-points |
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| 280 | !=========================== |
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[1438] | 281 | IF( neuler == 0 .AND. kt == nit000 ) THEN ! Euler time-stepping at first time-step : no filter |
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| 282 | sshn (:,:) = ssha (:,:) ! now <-- after (before already = now) |
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| 283 | sshu_n(:,:) = sshu_a(:,:) |
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| 284 | sshv_n(:,:) = sshv_a(:,:) |
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[2148] | 285 | DO jj = 1, jpjm1 |
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| 286 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 287 | sshf_n(ji,jj) = 0.5 * umask(ji,jj,1) * umask(ji,jj+1,1) & |
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| 288 | & / ( e1f(ji,jj ) * e2f(ji,jj ) ) & |
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| 289 | & * ( e1u(ji,jj ) * e2u(ji,jj ) * sshu_n(ji,jj ) & |
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| 290 | & + e1u(ji,jj+1) * e2u(ji,jj+1) * sshu_n(ji,jj+1) ) |
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| 291 | END DO |
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| 292 | END DO |
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| 293 | ! Boundaries conditions |
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| 294 | CALL lbc_lnk( sshf_n, 'F', 1. ) |
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[1438] | 295 | ELSE ! Leap-Frog time-stepping: Asselin filter + swap |
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[2148] | 296 | zec = atfp * rdt / rau0 |
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[1438] | 297 | DO jj = 1, jpj |
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| 298 | DO ji = 1, jpi ! before <-- now filtered |
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[2148] | 299 | sshb (ji,jj) = sshn (ji,jj) + atfp * ( sshb(ji,jj) - 2 * sshn(ji,jj) + ssha(ji,jj) ) & |
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| 300 | & - zec * ( emp_b(ji,jj) - emp(ji,jj) ) * tmask(ji,jj,1) |
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[1438] | 301 | sshn (ji,jj) = ssha (ji,jj) ! now <-- after |
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| 302 | sshu_n(ji,jj) = sshu_a(ji,jj) |
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| 303 | sshv_n(ji,jj) = sshv_a(ji,jj) |
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| 304 | END DO |
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| 305 | END DO |
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[2148] | 306 | DO jj = 1, jpjm1 |
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| 307 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 308 | sshf_n(ji,jj) = 0.5 * umask(ji,jj,1) * umask(ji,jj+1,1) & |
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| 309 | & / ( e1f(ji,jj ) * e2f(ji,jj ) ) & |
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| 310 | & * ( e1u(ji,jj ) * e2u(ji,jj ) * sshu_n(ji,jj ) & |
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| 311 | & + e1u(ji,jj+1) * e2u(ji,jj+1) * sshu_n(ji,jj+1) ) |
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| 312 | END DO |
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| 313 | END DO |
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| 314 | ! Boundaries conditions |
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| 315 | CALL lbc_lnk( sshf_n, 'F', 1. ) |
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| 316 | DO jj = 1, jpjm1 |
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| 317 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 318 | sshu_b(ji,jj) = 0.5 * umask(ji,jj,1) / ( e1u(ji ,jj) * e2u(ji ,jj) ) & |
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| 319 | & * ( e1t(ji ,jj) * e2t(ji ,jj) * sshb(ji ,jj) & |
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| 320 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * sshb(ji+1,jj) ) |
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| 321 | sshv_b(ji,jj) = 0.5 * vmask(ji,jj,1) / ( e1v(ji,jj ) * e2v(ji,jj ) ) & |
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| 322 | & * ( e1t(ji,jj ) * e2t(ji,jj ) * sshb(ji,jj ) & |
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| 323 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * sshb(ji,jj+1) ) |
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| 324 | END DO |
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| 325 | END DO |
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| 326 | ! Boundaries conditions |
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| 327 | CALL lbc_lnk( sshu_b, 'U', 1. ) |
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| 328 | CALL lbc_lnk( sshv_b, 'V', 1. ) |
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[1438] | 329 | ENDIF |
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[2148] | 330 | ! !--------------------------! |
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| 331 | ELSE ! fixed levels ! |
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| 332 | ! !--------------------------! |
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[1438] | 333 | ! |
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[2148] | 334 | ! ssh at t-point only |
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| 335 | !==================== |
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[1438] | 336 | IF( neuler == 0 .AND. kt == nit000 ) THEN ! Euler time-stepping at first time-step : no filter |
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| 337 | sshn(:,:) = ssha(:,:) ! now <-- after (before already = now) |
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| 338 | ! |
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| 339 | ELSE ! Leap-Frog time-stepping: Asselin filter + swap |
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| 340 | DO jj = 1, jpj |
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| 341 | DO ji = 1, jpi ! before <-- now filtered |
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[2148] | 342 | sshb(ji,jj) = sshn(ji,jj) + atfp * ( sshb(ji,jj) - 2 * sshn(ji,jj) + ssha(ji,jj) ) |
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[1438] | 343 | sshn(ji,jj) = ssha(ji,jj) ! now <-- after |
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| 344 | END DO |
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| 345 | END DO |
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| 346 | ENDIF |
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| 347 | ! |
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| 348 | ENDIF |
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| 349 | ! |
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[2487] | 350 | ! Update velocity at AGRIF zoom boundaries |
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| 351 | #id defined key_agrif |
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| 352 | IF ( .NOT.Agrif_Root() ) CALL Agrif_Update_Dyn( kt ) |
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| 353 | #endif |
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| 354 | ! |
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[2148] | 355 | IF(ln_ctl) CALL prt_ctl( tab2d_1=sshb, clinfo1=' sshb - : ', mask1=tmask, ovlap=1 ) |
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[1438] | 356 | ! |
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| 357 | END SUBROUTINE ssh_nxt |
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[3] | 358 | |
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| 359 | !!====================================================================== |
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[1565] | 360 | END MODULE sshwzv |
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