[358] | 1 | MODULE dynspg |
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| 2 | !!====================================================================== |
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| 3 | !! *** MODULE dynspg *** |
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| 4 | !! Ocean dynamics: surface pressure gradient control |
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| 5 | !!====================================================================== |
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[1566] | 6 | !! History : 1.0 ! 2005-12 (C. Talandier, G. Madec, V. Garnier) Original code |
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| 7 | !! 3.2 ! 2009-07 (R. Benshila) Suppression of rigid-lid option |
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[503] | 8 | !!---------------------------------------------------------------------- |
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[358] | 9 | |
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| 10 | !!---------------------------------------------------------------------- |
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| 11 | !! dyn_spg : update the dynamics trend with the lateral diffusion |
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| 12 | !! dyn_spg_ctl : initialization, namelist read, and parameters control |
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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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[2715] | 16 | USE phycst ! physical constants |
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[2528] | 17 | USE sbc_oce ! surface boundary condition: ocean |
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| 18 | USE sbcapr ! surface boundary condition: atmospheric pressure |
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[367] | 19 | USE dynspg_oce ! surface pressure gradient variables |
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[358] | 20 | USE dynspg_exp ! surface pressure gradient (dyn_spg_exp routine) |
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| 21 | USE dynspg_ts ! surface pressure gradient (dyn_spg_ts routine) |
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| 22 | USE dynspg_flt ! surface pressure gradient (dyn_spg_flt routine) |
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[2528] | 23 | USE dynadv ! dynamics: vector invariant versus flux form |
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[358] | 24 | USE trdmod ! ocean dynamics trends |
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| 25 | USE trdmod_oce ! ocean variables trends |
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| 26 | USE prtctl ! Print control (prt_ctl routine) |
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| 27 | USE in_out_manager ! I/O manager |
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[2715] | 28 | USE lib_mpp ! MPP library |
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| 29 | USE solver ! solver initialization |
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[3294] | 30 | USE wrk_nemo ! Memory Allocation |
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| 31 | USE timing ! Timing |
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[358] | 32 | |
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[3294] | 33 | |
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[358] | 34 | IMPLICIT NONE |
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| 35 | PRIVATE |
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| 36 | |
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[2528] | 37 | PUBLIC dyn_spg ! routine called by step module |
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| 38 | PUBLIC dyn_spg_init ! routine called by opa module |
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[358] | 39 | |
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[503] | 40 | INTEGER :: nspg = 0 ! type of surface pressure gradient scheme defined from lk_dynspg_... |
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[358] | 41 | |
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| 42 | !! * Substitutions |
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| 43 | # include "domzgr_substitute.h90" |
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| 44 | # include "vectopt_loop_substitute.h90" |
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| 45 | !!---------------------------------------------------------------------- |
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[1566] | 46 | !! NEMO/OPA 3.2 , LODYC-IPSL (2009) |
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[1152] | 47 | !! $Id$ |
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[2715] | 48 | !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt) |
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[358] | 49 | !!---------------------------------------------------------------------- |
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| 50 | CONTAINS |
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| 51 | |
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| 52 | SUBROUTINE dyn_spg( kt, kindic ) |
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| 53 | !!---------------------------------------------------------------------- |
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| 54 | !! *** ROUTINE dyn_spg *** |
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| 55 | !! |
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[1566] | 56 | !! ** Purpose : achieve the momentum time stepping by computing the |
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[2528] | 57 | !! last trend, the surface pressure gradient including the |
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| 58 | !! atmospheric pressure forcing (ln_apr_dyn=T), and performing |
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[1566] | 59 | !! the Leap-Frog integration. |
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| 60 | !!gm In the current version only the filtered solution provide |
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| 61 | !!gm the after velocity, in the 2 other (ua,va) are still the trends |
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| 62 | !! |
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| 63 | !! ** Method : Three schemes: |
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| 64 | !! - explicit computation : the spg is evaluated at now |
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| 65 | !! - filtered computation : the Roulet & madec (2000) technique is used |
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| 66 | !! - split-explicit computation: a time splitting technique is used |
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| 67 | !! |
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[2528] | 68 | !! ln_apr_dyn=T : the atmospheric pressure forcing is applied |
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| 69 | !! as the gradient of the inverse barometer ssh: |
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| 70 | !! apgu = - 1/rau0 di[apr] = 0.5*grav di[ssh_ib+ssh_ibb] |
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| 71 | !! apgv = - 1/rau0 dj[apr] = 0.5*grav dj[ssh_ib+ssh_ibb] |
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| 72 | !! Note that as all external forcing a time averaging over a two rdt |
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| 73 | !! period is used to prevent the divergence of odd and even time step. |
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| 74 | !! |
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[1566] | 75 | !! N.B. : When key_esopa is used all the scheme are tested, regardless |
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| 76 | !! of the physical meaning of the results. |
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[358] | 77 | !!---------------------------------------------------------------------- |
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[2715] | 78 | ! |
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[1566] | 79 | INTEGER, INTENT(in ) :: kt ! ocean time-step index |
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| 80 | INTEGER, INTENT( out) :: kindic ! solver flag |
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[2715] | 81 | ! |
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[2528] | 82 | INTEGER :: ji, jj, jk ! dummy loop indices |
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| 83 | REAL(wp) :: z2dt, zg_2 ! temporary scalar |
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[3294] | 84 | REAL(wp), POINTER, DIMENSION(:,:,:) :: ztrdu, ztrdv |
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[358] | 85 | !!---------------------------------------------------------------------- |
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[3294] | 86 | ! |
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| 87 | IF( nn_timing == 1 ) CALL timing_start('dyn_spg') |
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| 88 | ! |
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[358] | 89 | |
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[1566] | 90 | !!gm NOTA BENE : the dynspg_exp and dynspg_ts should be modified so that |
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| 91 | !!gm they return the after velocity, not the trends (as in trazdf_imp...) |
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| 92 | !!gm In this case, change/simplify dynnxt |
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| 93 | |
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| 94 | |
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[358] | 95 | IF( l_trddyn ) THEN ! temporary save of ta and sa trends |
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[3294] | 96 | CALL wrk_alloc( jpi, jpj, jpk, ztrdu, ztrdv ) |
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[358] | 97 | ztrdu(:,:,:) = ua(:,:,:) |
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| 98 | ztrdv(:,:,:) = va(:,:,:) |
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| 99 | ENDIF |
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| 100 | |
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[2528] | 101 | IF( ln_apr_dyn ) THEN !== Atmospheric pressure gradient ==! |
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| 102 | zg_2 = grav * 0.5 |
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| 103 | DO jj = 2, jpjm1 ! gradient of Patm using inverse barometer ssh |
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| 104 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| 105 | spgu(ji,jj) = zg_2 * ( ssh_ib (ji+1,jj) - ssh_ib (ji,jj) & |
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| 106 | & + ssh_ibb(ji+1,jj) - ssh_ibb(ji,jj) ) /e1u(ji,jj) |
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| 107 | spgv(ji,jj) = zg_2 * ( ssh_ib (ji,jj+1) - ssh_ib (ji,jj) & |
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[3322] | 108 | & + ssh_ibb(ji,jj+1) - ssh_ibb(ji,jj) ) /e2v(ji,jj) |
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[2528] | 109 | END DO |
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| 110 | END DO |
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| 111 | DO jk = 1, jpkm1 ! Add the apg to the general trend |
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| 112 | DO jj = 2, jpjm1 |
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| 113 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| 114 | ua(ji,jj,jk) = ua(ji,jj,jk) + spgu(ji,jj) |
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| 115 | va(ji,jj,jk) = va(ji,jj,jk) + spgv(ji,jj) |
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| 116 | END DO |
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| 117 | END DO |
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| 118 | END DO |
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| 119 | ENDIF |
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| 120 | |
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| 121 | |
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[358] | 122 | SELECT CASE ( nspg ) ! compute surf. pressure gradient trend and add it to the general trend |
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[789] | 123 | ! |
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[1566] | 124 | CASE ( 0 ) ; CALL dyn_spg_exp( kt ) ! explicit |
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| 125 | CASE ( 1 ) ; CALL dyn_spg_ts ( kt ) ! time-splitting |
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| 126 | CASE ( 2 ) ; CALL dyn_spg_flt( kt, kindic ) ! filtered |
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[789] | 127 | ! |
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[1566] | 128 | CASE ( -1 ) ! esopa: test all possibility with control print |
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| 129 | CALL dyn_spg_exp( kt ) |
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| 130 | CALL prt_ctl( tab3d_1=ua, clinfo1=' spg0 - Ua: ', mask1=umask, & |
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| 131 | & tab3d_2=va, clinfo2= ' Va: ', mask2=vmask, clinfo3='dyn' ) |
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| 132 | CALL dyn_spg_ts ( kt ) |
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| 133 | CALL prt_ctl( tab3d_1=ua, clinfo1=' spg1 - Ua: ', mask1=umask, & |
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| 134 | & tab3d_2=va, clinfo2= ' Va: ', mask2=vmask, clinfo3='dyn' ) |
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| 135 | CALL dyn_spg_flt( kt, kindic ) |
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| 136 | CALL prt_ctl( tab3d_1=ua, clinfo1=' spg2 - Ua: ', mask1=umask, & |
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| 137 | & tab3d_2=va, clinfo2= ' Va: ', mask2=vmask, clinfo3='dyn' ) |
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[358] | 138 | END SELECT |
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[503] | 139 | ! |
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[1566] | 140 | IF( l_trddyn ) THEN ! save the surface pressure gradient trends for further diagnostics |
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[358] | 141 | SELECT CASE ( nspg ) |
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[1528] | 142 | CASE ( 0, 1 ) |
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[358] | 143 | ztrdu(:,:,:) = ua(:,:,:) - ztrdu(:,:,:) |
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| 144 | ztrdv(:,:,:) = va(:,:,:) - ztrdv(:,:,:) |
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[1528] | 145 | CASE( 2 ) |
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[358] | 146 | z2dt = 2. * rdt |
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| 147 | IF( neuler == 0 .AND. kt == nit000 ) z2dt = rdt |
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| 148 | ztrdu(:,:,:) = ( ua(:,:,:) - ub(:,:,:) ) / z2dt - ztrdu(:,:,:) |
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| 149 | ztrdv(:,:,:) = ( va(:,:,:) - vb(:,:,:) ) / z2dt - ztrdv(:,:,:) |
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| 150 | END SELECT |
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[503] | 151 | CALL trd_mod( ztrdu, ztrdv, jpdyn_trd_spg, 'DYN', kt ) |
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[3294] | 152 | ! |
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| 153 | CALL wrk_dealloc( jpi, jpj, jpk, ztrdu, ztrdv ) |
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[358] | 154 | ENDIF |
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| 155 | ! ! print mean trends (used for debugging) |
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| 156 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ua, clinfo1=' spg - Ua: ', mask1=umask, & |
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| 157 | & tab3d_2=va, clinfo2= ' Va: ', mask2=vmask, clinfo3='dyn' ) |
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[503] | 158 | ! |
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[3294] | 159 | IF( nn_timing == 1 ) CALL timing_stop('dyn_spg') |
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[2715] | 160 | ! |
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[358] | 161 | END SUBROUTINE dyn_spg |
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| 162 | |
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| 163 | |
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[2528] | 164 | SUBROUTINE dyn_spg_init |
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[358] | 165 | !!--------------------------------------------------------------------- |
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[2528] | 166 | !! *** ROUTINE dyn_spg_init *** |
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[358] | 167 | !! |
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| 168 | !! ** Purpose : Control the consistency between cpp options for |
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[1566] | 169 | !! surface pressure gradient schemes |
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[358] | 170 | !!---------------------------------------------------------------------- |
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| 171 | INTEGER :: ioptio |
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| 172 | !!---------------------------------------------------------------------- |
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[3294] | 173 | ! |
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| 174 | IF( nn_timing == 1 ) CALL timing_start('dyn_spg_init') |
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| 175 | ! |
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[1566] | 176 | IF(lwp) THEN ! Control print |
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[358] | 177 | WRITE(numout,*) |
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[2528] | 178 | WRITE(numout,*) 'dyn_spg_init : choice of the surface pressure gradient scheme' |
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[358] | 179 | WRITE(numout,*) '~~~~~~~~~~~' |
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| 180 | WRITE(numout,*) ' Explicit free surface lk_dynspg_exp = ', lk_dynspg_exp |
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| 181 | WRITE(numout,*) ' Free surface with time splitting lk_dynspg_ts = ', lk_dynspg_ts |
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| 182 | WRITE(numout,*) ' Filtered free surface cst volume lk_dynspg_flt = ', lk_dynspg_flt |
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| 183 | ENDIF |
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| 184 | |
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[2715] | 185 | ! ! allocate dyn_spg arrays |
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| 186 | IF( lk_dynspg_ts ) THEN |
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| 187 | IF( dynspg_oce_alloc() /= 0 ) CALL ctl_stop('STOP', 'dyn_spg_init: failed to allocate dynspg_oce arrays') |
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| 188 | IF( dyn_spg_ts_alloc() /= 0 ) CALL ctl_stop('STOP', 'dyn_spg_init: failed to allocate dynspg_ts arrays') |
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| 189 | ENDIF |
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| 190 | |
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[1566] | 191 | ! ! Control of surface pressure gradient scheme options |
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[358] | 192 | ioptio = 0 |
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| 193 | IF(lk_dynspg_exp) ioptio = ioptio + 1 |
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| 194 | IF(lk_dynspg_ts ) ioptio = ioptio + 1 |
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| 195 | IF(lk_dynspg_flt) ioptio = ioptio + 1 |
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[1566] | 196 | ! |
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[474] | 197 | IF( ( ioptio > 1 .AND. .NOT. lk_esopa ) .OR. ioptio == 0 ) & |
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| 198 | & CALL ctl_stop( ' Choose only one surface pressure gradient scheme with a key cpp' ) |
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[1566] | 199 | ! |
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[358] | 200 | IF( lk_esopa ) nspg = -1 |
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| 201 | IF( lk_dynspg_exp) nspg = 0 |
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| 202 | IF( lk_dynspg_ts ) nspg = 1 |
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| 203 | IF( lk_dynspg_flt) nspg = 2 |
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[1566] | 204 | ! |
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[372] | 205 | IF( lk_esopa ) nspg = -1 |
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[1566] | 206 | ! |
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| 207 | IF(lwp) THEN |
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[358] | 208 | WRITE(numout,*) |
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[1528] | 209 | IF( nspg == -1 ) WRITE(numout,*) ' ESOPA test All scheme used' |
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[372] | 210 | IF( nspg == 0 ) WRITE(numout,*) ' explicit free surface' |
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| 211 | IF( nspg == 1 ) WRITE(numout,*) ' free surface with time splitting scheme' |
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| 212 | IF( nspg == 2 ) WRITE(numout,*) ' filtered free surface' |
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[358] | 213 | ENDIF |
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| 214 | |
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[2715] | 215 | #if defined key_dynspg_flt || defined key_esopa |
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| 216 | CALL solver_init( nit000 ) ! Elliptic solver initialisation |
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| 217 | #endif |
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| 218 | |
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[1566] | 219 | ! ! Control of timestep choice |
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[1241] | 220 | IF( lk_dynspg_ts .OR. lk_dynspg_exp ) THEN |
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[2528] | 221 | IF( nn_cla == 1 ) CALL ctl_stop( 'Crossland advection not implemented for this free surface formulation' ) |
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[358] | 222 | ENDIF |
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| 223 | |
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[2528] | 224 | ! ! Control of momentum formulation |
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| 225 | IF( lk_dynspg_ts .AND. lk_vvl ) THEN |
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| 226 | IF( .NOT.ln_dynadv_vec ) CALL ctl_stop( 'Flux form not implemented for this free surface formulation' ) |
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| 227 | ENDIF |
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[1566] | 228 | ! |
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[3294] | 229 | IF( nn_timing == 1 ) CALL timing_stop('dyn_spg_init') |
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| 230 | ! |
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[2528] | 231 | END SUBROUTINE dyn_spg_init |
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[358] | 232 | |
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| 233 | !!====================================================================== |
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| 234 | END MODULE dynspg |
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