| 1 | MODULE sshwzv |
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| 2 | !!============================================================================== |
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| 3 | !! *** MODULE sshwzv *** |
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| 4 | !! Ocean dynamics : sea surface height and vertical velocity |
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| 5 | !!============================================================================== |
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| 6 | !! History : 3.1 ! 2009-02 (G. Madec, M. Leclair) Original code |
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| 7 | !! 3.3 ! 2010-04 (M. Leclair, G. Madec) modified LF-RA |
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| 8 | !!---------------------------------------------------------------------- |
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| 9 | |
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| 10 | !!---------------------------------------------------------------------- |
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| 11 | !! ssh_wzv : after ssh & now vertical velocity |
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| 12 | !! ssh_nxt : filter ans swap the ssh arrays |
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| 13 | !!---------------------------------------------------------------------- |
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| 14 | USE oce ! ocean dynamics and tracers variables |
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| 15 | USE dom_oce ! ocean space and time domain variables |
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| 16 | USE sbc_oce ! surface boundary condition: ocean |
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| 17 | USE domvvl ! Variable volume |
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| 18 | USE divcur ! hor. divergence and curl (div & cur routines) |
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| 19 | USE cla_div ! cross land: hor. divergence (div_cla routine) |
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| 20 | USE iom ! I/O library |
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| 21 | USE restart ! only for lrst_oce |
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| 22 | USE in_out_manager ! I/O manager |
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| 23 | USE prtctl ! Print control |
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| 24 | USE phycst |
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| 25 | USE lbclnk ! ocean lateral boundary condition (or mpp link) |
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| 26 | USE obc_par ! open boundary cond. parameter |
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| 27 | USE obc_oce |
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| 28 | USE diaar5, ONLY : lk_diaar5 |
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| 29 | USE iom |
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| 30 | |
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| 31 | IMPLICIT NONE |
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| 32 | PRIVATE |
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| 33 | |
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| 34 | PUBLIC ssh_wzv ! called by step.F90 |
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| 35 | PUBLIC ssh_nxt ! called by step.F90 |
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| 36 | |
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| 37 | !! * Substitutions |
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| 38 | # include "domzgr_substitute.h90" |
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| 39 | # include "vectopt_loop_substitute.h90" |
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| 40 | !!---------------------------------------------------------------------- |
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| 41 | !! NEMO/OPA 3.3 , LOCEAN-IPSL (2010) |
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| 42 | !! $Id$ |
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| 43 | !! Software governed by the CeCILL licence (modipsl/doc/NEMO_CeCILL.txt) |
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| 44 | !!---------------------------------------------------------------------- |
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| 45 | |
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| 46 | CONTAINS |
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| 47 | |
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| 48 | SUBROUTINE ssh_wzv( kt ) |
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| 49 | !!---------------------------------------------------------------------- |
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| 50 | !! *** ROUTINE ssh_wzv *** |
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| 51 | !! |
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| 52 | !! ** Purpose : compute the after ssh (ssha), the now vertical velocity |
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| 53 | !! and update the now vertical coordinate (lk_vvl=T). |
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| 54 | !! |
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| 55 | !! ** Method : - Using the incompressibility hypothesis, the vertical |
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| 56 | !! velocity is computed by integrating the horizontal divergence |
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| 57 | !! from the bottom to the surface minus the scale factor evolution. |
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| 58 | !! The boundary conditions are w=0 at the bottom (no flux) and. |
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| 59 | !! |
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| 60 | !! ** action : ssha : after sea surface height |
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| 61 | !! wn : now vertical velocity |
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| 62 | !! sshu_a, sshv_a, sshf_a : after sea surface height (lk_vvl=T) |
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| 63 | !! hu, hv, hur, hvr : ocean depth and its inverse at u-,v-points |
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| 64 | !! |
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| 65 | !! Reference : Leclair, M., and G. Madec, 2009, Ocean Modelling. |
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| 66 | !!---------------------------------------------------------------------- |
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| 67 | USE oce, ONLY : z3d => ta ! use ta as 3D workspace |
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| 68 | !! |
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| 69 | INTEGER, INTENT(in) :: kt ! time step |
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| 70 | !! |
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| 71 | INTEGER :: ji, jj, jk ! dummy loop indices |
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| 72 | REAL(wp) :: zcoefu, zcoefv, zcoeff ! temporary scalars |
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| 73 | REAL(wp) :: z2dt, z1_2dt, z1_rau0 ! temporary scalars |
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| 74 | REAL(wp), DIMENSION(jpi,jpj) :: zhdiv ! 2D workspace |
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| 75 | REAL(wp), DIMENSION(jpi,jpj) :: z2d ! 2D workspace |
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| 76 | !!---------------------------------------------------------------------- |
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| 77 | |
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| 78 | IF( kt == nit000 ) THEN |
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| 79 | ! |
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| 80 | IF(lwp) WRITE(numout,*) |
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| 81 | IF(lwp) WRITE(numout,*) 'ssh_wzv : after sea surface height and now vertical velocity ' |
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| 82 | IF(lwp) WRITE(numout,*) '~~~~~~~ ' |
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| 83 | ! |
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| 84 | wn(:,:,jpk) = 0.e0 ! bottom boundary condition: w=0 (set once for all) |
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| 85 | ! |
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| 86 | IF( lk_vvl ) THEN ! before and now Sea SSH at u-, v-, f-points (vvl case only) |
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| 87 | DO jj = 1, jpjm1 |
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| 88 | DO ji = 1, jpim1 ! caution: use of Vector Opt. not possible |
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| 89 | zcoefu = 0.5 * umask(ji,jj,1) / ( e1u(ji,jj) * e2u(ji,jj) ) |
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| 90 | zcoefv = 0.5 * vmask(ji,jj,1) / ( e1v(ji,jj) * e2v(ji,jj) ) |
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| 91 | zcoeff = 0.25 * umask(ji,jj,1) * umask(ji,jj+1,1) |
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| 92 | sshu_b(ji,jj) = zcoefu * ( e1t(ji ,jj) * e2t(ji ,jj) * sshb(ji ,jj) & |
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| 93 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * sshb(ji+1,jj) ) |
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| 94 | sshv_b(ji,jj) = zcoefv * ( e1t(ji,jj ) * e2t(ji,jj ) * sshb(ji,jj ) & |
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| 95 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * sshb(ji,jj+1) ) |
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| 96 | sshu_n(ji,jj) = zcoefu * ( e1t(ji ,jj) * e2t(ji ,jj) * sshn(ji ,jj) & |
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| 97 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * sshn(ji+1,jj) ) |
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| 98 | sshv_n(ji,jj) = zcoefv * ( e1t(ji,jj ) * e2t(ji,jj ) * sshn(ji,jj ) & |
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| 99 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * sshn(ji,jj+1) ) |
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| 100 | END DO |
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| 101 | END DO |
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| 102 | CALL lbc_lnk( sshu_b, 'U', 1. ) ; CALL lbc_lnk( sshu_n, 'U', 1. ) |
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| 103 | CALL lbc_lnk( sshv_b, 'V', 1. ) ; CALL lbc_lnk( sshv_n, 'V', 1. ) |
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| 104 | DO jj = 1, jpjm1 |
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| 105 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 106 | sshf_n(ji,jj) = 0.5 * umask(ji,jj,1) * umask(ji,jj+1,1) & |
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| 107 | & / ( e1f(ji,jj ) * e2f(ji,jj ) ) & |
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| 108 | & * ( e1u(ji,jj ) * e2u(ji,jj ) * sshu_n(ji,jj ) & |
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| 109 | & + e1u(ji,jj+1) * e2u(ji,jj+1) * sshu_n(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( sshf_n, 'F', 1. ) |
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| 113 | ENDIF |
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| 114 | ! |
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| 115 | ENDIF |
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| 116 | |
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| 117 | ! !------------------------------------------! |
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| 118 | IF( lk_vvl ) THEN ! Regridding: Update Now Vertical coord. ! (only in vvl case) |
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| 119 | ! !------------------------------------------! |
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| 120 | DO jk = 1, jpkm1 |
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| 121 | fsdept(:,:,jk) = fsdept_n(:,:,jk) ! now local depths stored in fsdep. arrays |
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| 122 | fsdepw(:,:,jk) = fsdepw_n(:,:,jk) |
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| 123 | fsde3w(:,:,jk) = fsde3w_n(:,:,jk) |
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| 124 | ! |
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| 125 | fse3t (:,:,jk) = fse3t_n (:,:,jk) ! vertical scale factors stored in fse3. arrays |
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| 126 | fse3u (:,:,jk) = fse3u_n (:,:,jk) |
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| 127 | fse3v (:,:,jk) = fse3v_n (:,:,jk) |
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| 128 | fse3f (:,:,jk) = fse3f_n (:,:,jk) |
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| 129 | fse3w (:,:,jk) = fse3w_n (:,:,jk) |
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| 130 | fse3uw(:,:,jk) = fse3uw_n(:,:,jk) |
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| 131 | fse3vw(:,:,jk) = fse3vw_n(:,:,jk) |
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| 132 | END DO |
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| 133 | ! |
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| 134 | hu(:,:) = hu_0(:,:) + sshu_n(:,:) ! now ocean depth (at u- and v-points) |
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| 135 | hv(:,:) = hv_0(:,:) + sshv_n(:,:) |
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| 136 | ! ! now masked inverse of the ocean depth (at u- and v-points) |
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| 137 | hur(:,:) = umask(:,:,1) / ( hu(:,:) + 1.e0 - umask(:,:,1) ) |
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| 138 | hvr(:,:) = vmask(:,:,1) / ( hv(:,:) + 1.e0 - vmask(:,:,1) ) |
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| 139 | ! |
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| 140 | ENDIF |
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| 141 | |
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| 142 | CALL div_cur( kt ) ! Horizontal divergence & Relative vorticity |
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| 143 | IF( n_cla == 1 ) CALL div_cla( kt ) ! Cross Land Advection (Update Hor. divergence) |
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| 144 | |
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| 145 | z2dt = 2. * rdt ! set time step size (Euler/Leapfrog) |
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| 146 | IF( neuler == 0 .AND. kt == nit000 ) z2dt =rdt |
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| 147 | |
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| 148 | ! !------------------------------! |
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| 149 | ! ! After Sea Surface Height ! |
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| 150 | ! !------------------------------! |
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| 151 | zhdiv(:,:) = 0.e0 |
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| 152 | DO jk = 1, jpkm1 ! Horizontal divergence of barotropic transports |
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| 153 | zhdiv(:,:) = zhdiv(:,:) + fse3t(:,:,jk) * hdivn(:,:,jk) |
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| 154 | END DO |
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| 155 | ! ! Sea surface elevation time stepping |
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| 156 | ! In forward Euler time stepping case, the same formulation as in the leap-frog case can be used |
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| 157 | ! because emp_b field is initialized with the vlaues of emp field. Hence, 0.5 * ( emp + emp_b ) = emp |
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| 158 | z1_rau0 = 0.5 / rau0 |
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| 159 | ssha(:,:) = ( sshb(:,:) - z2dt * ( z1_rau0 * ( emp_b(:,:) + emp(:,:) ) + zhdiv(:,:) ) ) * tmask(:,:,1) |
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| 160 | |
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| 161 | #if defined key_obc |
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| 162 | IF( Agrif_Root() ) THEN |
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| 163 | ssha(:,:) = ssha(:,:) * obctmsk(:,:) |
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| 164 | CALL lbc_lnk( ssha, 'T', 1. ) ! absolutly compulsory !! (jmm) |
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| 165 | ENDIF |
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| 166 | #endif |
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| 167 | ! ! Sea Surface Height at u-,v- and f-points (vvl case only) |
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| 168 | IF( lk_vvl ) THEN ! (required only in key_vvl case) |
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| 169 | DO jj = 1, jpjm1 |
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| 170 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 171 | sshu_a(ji,jj) = 0.5 * umask(ji,jj,1) / ( e1u(ji ,jj) * e2u(ji ,jj) ) & |
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| 172 | & * ( e1t(ji ,jj) * e2t(ji ,jj) * ssha(ji ,jj) & |
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| 173 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * ssha(ji+1,jj) ) |
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| 174 | sshv_a(ji,jj) = 0.5 * vmask(ji,jj,1) / ( e1v(ji,jj ) * e2v(ji,jj ) ) & |
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| 175 | & * ( e1t(ji,jj ) * e2t(ji,jj ) * ssha(ji,jj ) & |
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| 176 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * ssha(ji,jj+1) ) |
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| 177 | END DO |
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| 178 | END DO |
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| 179 | ! Boundaries conditions |
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| 180 | CALL lbc_lnk( sshu_a, 'U', 1. ) |
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| 181 | CALL lbc_lnk( sshv_a, 'V', 1. ) |
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| 182 | ENDIF |
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| 183 | ! !----------------------------------------! |
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| 184 | ! ! vertical scale factor laplacian ! |
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| 185 | ! !----------------------------------------! |
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| 186 | ! Needed for Robert-Asselin time filter and for Brown & Campana semi implicit hydrostatic presure gradient |
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| 187 | DO jk = 1, jpk |
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| 188 | fse3t_d(:,:,jk) = fse3t_b(:,:,jk) & |
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| 189 | & - 2.e0 * fse3t_n(:,:,jk) & |
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| 190 | & + fse3t_a(:,:,jk) |
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| 191 | ENDDO |
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| 192 | ! !------------------------------! |
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| 193 | ! ! Now Vertical Velocity ! |
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| 194 | ! !------------------------------! |
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| 195 | z1_2dt = 1.e0 / z2dt |
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| 196 | DO jk = jpkm1, 1, -1 ! integrate from the bottom the hor. divergence |
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| 197 | ! - ML - need 3 lines here because replacement of fse3t by its expression yields too long lines otherwise |
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| 198 | wn(:,:,jk) = wn(:,:,jk+1) - fse3t_n(:,:,jk) * hdivn(:,:,jk) & |
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| 199 | & - ( fse3t_a(:,:,jk) - fse3t_b(:,:,jk) ) & |
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| 200 | & * tmask(:,:,jk) * z1_2dt |
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| 201 | END DO |
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| 202 | |
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| 203 | ! !------------------------------! |
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| 204 | ! ! outputs ! |
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| 205 | ! !------------------------------! |
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| 206 | CALL iom_put( "woce", wn ) ! vertical velocity |
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| 207 | CALL iom_put( "ssh" , sshn ) ! sea surface height |
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| 208 | CALL iom_put( "ssh2", sshn(:,:) * sshn(:,:) ) ! square of sea surface height |
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| 209 | IF( lk_diaar5 ) THEN ! vertical mass transport & its square value |
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| 210 | ! Caution: in the VVL case, it only correponds to the baroclinic mass transport. |
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| 211 | z2d(:,:) = rau0 * e1t(:,:) * e2t(:,:) |
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| 212 | DO jk = 1, jpk |
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| 213 | z3d(:,:,jk) = wn(:,:,jk) * z2d(:,:) |
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| 214 | END DO |
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| 215 | CALL iom_put( "w_masstr" , z3d ) |
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| 216 | CALL iom_put( "w_masstr2", z3d(:,:,:) * z3d(:,:,:) ) |
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| 217 | ENDIF |
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| 218 | ! |
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| 219 | IF(ln_ctl) CALL prt_ctl( tab2d_1=ssha, clinfo1=' ssha - : ', mask1=tmask, ovlap=1 ) |
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| 220 | ! |
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| 221 | END SUBROUTINE ssh_wzv |
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| 222 | |
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| 223 | |
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| 224 | SUBROUTINE ssh_nxt( kt ) |
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| 225 | !!---------------------------------------------------------------------- |
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| 226 | !! *** ROUTINE ssh_nxt *** |
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| 227 | !! |
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| 228 | !! ** Purpose : achieve the sea surface height time stepping by |
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| 229 | !! applying Asselin time filter and swapping the arrays |
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| 230 | !! ssha already computed in ssh_wzv |
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| 231 | !! |
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| 232 | !! ** Method : - apply Asselin time fiter to now ssh (excluding the forcing |
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| 233 | !! from the filter, see Leclair and Madec 2010) and swap : |
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| 234 | !! sshn = ssha + atfp * ( sshb -2 sshn + ssha ) |
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| 235 | !! - atfp * rdt * ( emp_b - emp ) / rau0 |
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| 236 | !! sshn = ssha |
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| 237 | !! |
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| 238 | !! ** action : - sshb, sshn : before & now sea surface height |
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| 239 | !! ready for the next time step |
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| 240 | !! |
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| 241 | !! Reference : Leclair, M., and G. Madec, 2009, Ocean Modelling. |
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| 242 | !!---------------------------------------------------------------------- |
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| 243 | INTEGER, INTENT(in) :: kt ! ocean time-step index |
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| 244 | !! |
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| 245 | INTEGER :: ji, jj ! dummy loop indices |
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| 246 | REAL(wp) :: zec ! temporary scalar |
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| 247 | !!---------------------------------------------------------------------- |
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| 248 | |
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| 249 | IF( kt == nit000 ) THEN |
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| 250 | IF(lwp) WRITE(numout,*) |
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| 251 | IF(lwp) WRITE(numout,*) 'ssh_nxt : next sea surface height (Asselin time filter + swap)' |
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| 252 | IF(lwp) WRITE(numout,*) '~~~~~~~ ' |
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| 253 | ENDIF |
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| 254 | |
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| 255 | ! !--------------------------! |
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| 256 | IF( lk_vvl ) THEN ! Variable volume levels ! |
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| 257 | ! !--------------------------! |
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| 258 | ! |
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| 259 | ! ssh at t-, u-, v, f-points |
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| 260 | !=========================== |
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| 261 | IF( neuler == 0 .AND. kt == nit000 ) THEN ! Euler time-stepping at first time-step : no filter |
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| 262 | sshn (:,:) = ssha (:,:) ! now <-- after (before already = now) |
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| 263 | sshu_n(:,:) = sshu_a(:,:) |
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| 264 | sshv_n(:,:) = sshv_a(:,:) |
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| 265 | DO jj = 1, jpjm1 |
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| 266 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 267 | sshf_n(ji,jj) = 0.5 * umask(ji,jj,1) * umask(ji,jj+1,1) & |
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| 268 | & / ( e1f(ji,jj ) * e2f(ji,jj ) ) & |
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| 269 | & * ( e1u(ji,jj ) * e2u(ji,jj ) * sshu_n(ji,jj ) & |
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| 270 | & + e1u(ji,jj+1) * e2u(ji,jj+1) * sshu_n(ji,jj+1) ) |
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| 271 | END DO |
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| 272 | END DO |
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| 273 | ! Boundaries conditions |
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| 274 | CALL lbc_lnk( sshf_n, 'F', 1. ) |
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| 275 | ELSE ! Leap-Frog time-stepping: Asselin filter + swap |
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| 276 | zec = atfp * rdt / rau0 |
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| 277 | DO jj = 1, jpj |
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| 278 | DO ji = 1, jpi ! before <-- now filtered |
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| 279 | sshb (ji,jj) = sshn (ji,jj) + atfp * ( sshb (ji,jj) - 2 * sshn (ji,jj) + ssha (ji,jj) ) & |
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| 280 | & - zec * ( emp_b(ji,jj) - emp(ji,jj) ) * tmask(ji,jj,1) |
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| 281 | sshn (ji,jj) = ssha (ji,jj) ! now <-- after |
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| 282 | sshu_n(ji,jj) = sshu_a(ji,jj) |
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| 283 | sshv_n(ji,jj) = sshv_a(ji,jj) |
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| 284 | END DO |
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| 285 | END DO |
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| 286 | DO jj = 1, jpjm1 |
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| 287 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 288 | sshf_n(ji,jj) = 0.5 * umask(ji,jj,1) * umask(ji,jj+1,1) & |
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| 289 | & / ( e1f(ji,jj ) * e2f(ji,jj ) ) & |
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| 290 | & * ( e1u(ji,jj ) * e2u(ji,jj ) * sshu_n(ji,jj ) & |
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| 291 | & + e1u(ji,jj+1) * e2u(ji,jj+1) * sshu_n(ji,jj+1) ) |
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| 292 | END DO |
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| 293 | END DO |
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| 294 | ! Boundaries conditions |
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| 295 | CALL lbc_lnk( sshf_n, 'F', 1. ) |
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| 296 | DO jj = 1, jpjm1 |
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| 297 | DO ji = 1, jpim1 ! NO Vector Opt. |
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| 298 | sshu_b(ji,jj) = 0.5 * umask(ji,jj,1) / ( e1u(ji ,jj) * e2u(ji ,jj) ) & |
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| 299 | & * ( e1t(ji ,jj) * e2t(ji ,jj) * sshb(ji ,jj) & |
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| 300 | & + e1t(ji+1,jj) * e2t(ji+1,jj) * sshb(ji+1,jj) ) |
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| 301 | sshv_b(ji,jj) = 0.5 * vmask(ji,jj,1) / ( e1v(ji,jj ) * e2v(ji,jj ) ) & |
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| 302 | & * ( e1t(ji,jj ) * e2t(ji,jj ) * sshb(ji,jj ) & |
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| 303 | & + e1t(ji,jj+1) * e2t(ji,jj+1) * sshb(ji,jj+1) ) |
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| 304 | END DO |
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| 305 | END DO |
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| 306 | ! Boundaries conditions |
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| 307 | CALL lbc_lnk( sshu_b, 'U', 1. ) |
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| 308 | CALL lbc_lnk( sshv_b, 'V', 1. ) |
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| 309 | ENDIF |
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| 310 | ! !--------------------------! |
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| 311 | ELSE ! fixed levels ! |
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| 312 | ! !--------------------------! |
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| 313 | ! |
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| 314 | ! ssh at t-point only |
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| 315 | !==================== |
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| 316 | IF( neuler == 0 .AND. kt == nit000 ) THEN ! Euler time-stepping at first time-step : no filter |
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| 317 | sshn(:,:) = ssha(:,:) ! now <-- after (before already = now) |
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| 318 | ! |
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| 319 | ELSE ! Leap-Frog time-stepping: Asselin filter + swap |
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| 320 | DO jj = 1, jpj |
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| 321 | DO ji = 1, jpi ! before <-- now filtered |
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| 322 | sshb(ji,jj) = sshn(ji,jj) + atfp * ( sshb(ji,jj) - 2 * sshn(ji,jj) + ssha(ji,jj) ) |
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| 323 | sshn(ji,jj) = ssha(ji,jj) ! now <-- after |
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| 324 | END DO |
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| 325 | END DO |
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| 326 | ENDIF |
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| 327 | ! |
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| 328 | ENDIF |
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| 329 | ! |
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| 330 | IF(ln_ctl) CALL prt_ctl( tab2d_1=sshb, clinfo1=' sshb - : ', mask1=tmask, ovlap=1 ) |
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| 331 | ! |
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| 332 | END SUBROUTINE ssh_nxt |
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| 333 | |
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| 334 | !!====================================================================== |
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| 335 | END MODULE sshwzv |
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