| 1 | MODULE trcsbc |
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| 2 | !!============================================================================== |
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| 3 | !! *** MODULE trcsbc *** |
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| 4 | !! Ocean passive tracers: surface boundary condition |
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| 5 | !!====================================================================== |
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| 6 | !! History : 8.2 ! 1998-10 (G. Madec, G. Roullet, M. Imbard) Original code |
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| 7 | !! 8.2 ! 2001-02 (D. Ludicone) sea ice and free surface |
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| 8 | !! 8.5 ! 2002-06 (G. Madec) F90: Free form and module |
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| 9 | !! 9.0 ! 2004-03 (C. Ethe) adapted for passive tracers |
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| 10 | !! ! 2006-08 (C. Deltel) Diagnose ML trends for passive tracers |
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| 11 | !!============================================================================== |
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| 12 | #if defined key_top |
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| 13 | !!---------------------------------------------------------------------- |
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| 14 | !! 'key_top' TOP models |
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| 15 | !!---------------------------------------------------------------------- |
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| 16 | !! trc_sbc : update the tracer trend at ocean surface |
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| 17 | !!---------------------------------------------------------------------- |
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| 18 | USE par_trc ! need jptra, number of passive tracers |
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| 19 | USE oce_trc ! ocean dynamics and active tracers variables |
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| 20 | USE trc ! ocean passive tracers variables |
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| 21 | USE prtctl ! Print control for debbuging |
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| 22 | USE iom |
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| 23 | USE trd_oce |
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| 24 | USE trdtra |
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| 25 | |
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| 26 | IMPLICIT NONE |
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| 27 | PRIVATE |
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| 28 | |
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| 29 | PUBLIC trc_sbc ! routine called by trctrp.F90 |
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| 30 | PUBLIC trc_sbc_RK3 ! routine called by stprk3_stg.F90 |
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| 31 | |
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| 32 | !! * Substitutions |
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| 33 | # include "do_loop_substitute.h90" |
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| 34 | # include "domzgr_substitute.h90" |
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| 35 | !!---------------------------------------------------------------------- |
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| 36 | !! NEMO/TOP 4.0 , NEMO Consortium (2018) |
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| 37 | !! $Id$ |
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| 38 | !! Software governed by the CeCILL license (see ./LICENSE) |
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| 39 | !!---------------------------------------------------------------------- |
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| 40 | CONTAINS |
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| 41 | |
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| 42 | SUBROUTINE trc_sbc ( kt, Kmm, ptr, Krhs ) |
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| 43 | !!---------------------------------------------------------------------- |
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| 44 | !! *** ROUTINE trc_sbc *** |
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| 45 | !! |
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| 46 | !! ** Purpose : Compute the tracer surface boundary condition trend of |
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| 47 | !! (concentration/dilution effect) and add it to the general |
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| 48 | !! trend of tracer equations. |
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| 49 | !! |
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| 50 | !! ** Method : |
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| 51 | !! * concentration/dilution effect: |
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| 52 | !! The surface freshwater flux modify the ocean volume |
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| 53 | !! and thus the concentration of a tracer as : |
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| 54 | !! tr(Krhs) = tr(Krhs) + emp * tr(Kmm) / e3t_ + fmmflx * tri / e3t for k=1 |
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| 55 | !! - tr(Kmm) , the concentration of tracer in the ocean |
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| 56 | !! - tri, the concentration of tracer in the sea-ice |
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| 57 | !! - emp, the surface freshwater budget (evaporation minus precipitation + fmmflx) |
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| 58 | !! given in kg/m2/s is divided by 1035 kg/m3 (density of ocean water) to obtain m/s. |
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| 59 | !! - fmmflx, the flux asscociated to freezing-melting of sea-ice |
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| 60 | !! In linear free surface case (ln_linssh=T), the volume of the |
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| 61 | !! ocean does not change with the water exchanges at the (air+ice)-sea |
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| 62 | !! |
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| 63 | !! ** Action : - Update the 1st level of tr(:,:,:,:,Krhs) with the trend associated |
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| 64 | !! with the tracer surface boundary condition |
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| 65 | !! |
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| 66 | !!---------------------------------------------------------------------- |
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| 67 | INTEGER, INTENT(in ) :: kt ! ocean time-step index |
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| 68 | INTEGER, INTENT(in ) :: Kmm, Krhs ! time level indices |
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| 69 | REAL(wp), DIMENSION(jpi,jpj,jpk,jptra,jpt), INTENT(inout) :: ptr ! passive tracers and RHS of tracer equation |
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| 70 | ! |
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| 71 | INTEGER :: ji, jj, jn ! dummy loop indices |
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| 72 | REAL(wp) :: zse3t, zrtrn, zfact ! local scalars |
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| 73 | REAL(wp) :: zdtra ! - - |
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| 74 | CHARACTER (len=22) :: charout |
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| 75 | REAL(wp), ALLOCATABLE, DIMENSION(:,:,:) :: ztrtrd |
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| 76 | !!--------------------------------------------------------------------- |
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| 77 | ! |
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| 78 | IF( ln_timing ) CALL timing_start('trc_sbc') |
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| 79 | ! |
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| 80 | ! Allocate temporary workspace |
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| 81 | IF( l_trdtrc ) ALLOCATE( ztrtrd(jpi,jpj,jpk) ) |
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| 82 | ! |
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| 83 | zrtrn = 1.e-15_wp |
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| 84 | |
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| 85 | IF( kt == nittrc000 ) THEN |
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| 86 | IF(lwp) WRITE(numout,*) |
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| 87 | IF(lwp) WRITE(numout,*) 'trc_sbc : Passive tracers surface boundary condition' |
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| 88 | IF(lwp) WRITE(numout,*) '~~~~~~~ ' |
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| 89 | ! |
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| 90 | IF( ln_rsttr .AND. .NOT.ln_top_euler .AND. & ! Restart: read in restart file |
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| 91 | iom_varid( numrtr, 'sbc_'//TRIM(ctrcnm(1))//'_b', ldstop = .FALSE. ) > 0 ) THEN |
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| 92 | IF(lwp) WRITE(numout,*) ' nittrc000-1 surface tracer content forcing fields read in the restart file' |
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| 93 | zfact = 0.5_wp |
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| 94 | DO jn = 1, jptra |
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| 95 | CALL iom_get( numrtr, jpdom_auto, 'sbc_'//TRIM(ctrcnm(jn))//'_b', sbc_trc_b(:,:,jn) ) ! before tracer content sbc |
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| 96 | END DO |
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| 97 | ELSE ! No restart or restart not found: Euler forward time stepping |
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| 98 | zfact = 1._wp |
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| 99 | sbc_trc_b(:,:,:) = 0._wp |
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| 100 | ENDIF |
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| 101 | ELSE ! Swap of forcing fields |
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| 102 | IF( ln_top_euler ) THEN |
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| 103 | zfact = 1._wp |
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| 104 | sbc_trc_b(:,:,:) = 0._wp |
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| 105 | ELSE |
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| 106 | zfact = 0.5_wp |
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| 107 | sbc_trc_b(:,:,:) = sbc_trc(:,:,:) |
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| 108 | ENDIF |
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| 109 | ! |
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| 110 | ENDIF |
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| 111 | |
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| 112 | ! 0. initialization |
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| 113 | SELECT CASE ( nn_ice_tr ) |
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| 114 | |
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| 115 | CASE ( -1 ) ! ! No tracers in sea ice ( trc_i = 0 ) |
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| 116 | ! |
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| 117 | DO jn = 1, jptra |
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| 118 | DO_2D( 0, 0, 0, 1 ) |
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| 119 | sbc_trc(ji,jj,jn) = 0._wp |
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| 120 | END_2D |
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| 121 | END DO |
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| 122 | ! |
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| 123 | IF( ln_linssh ) THEN !* linear free surface |
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| 124 | DO jn = 1, jptra |
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| 125 | DO_2D( 0, 0, 0, 1 ) |
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| 126 | sbc_trc(ji,jj,jn) = sbc_trc(ji,jj,jn) + r1_rho0 * emp(ji,jj) * ptr(ji,jj,1,jn,Kmm) !==>> add concentration/dilution effect due to constant volume cell |
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| 127 | END_2D |
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| 128 | END DO |
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| 129 | ENDIF |
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| 130 | ! |
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| 131 | CASE ( 0 ) ! Same concentration in sea ice and in the ocean ( trc_i = ptr(...,Kmm) ) |
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| 132 | ! |
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| 133 | DO jn = 1, jptra |
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| 134 | DO_2D( 0, 0, 0, 1 ) |
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| 135 | sbc_trc(ji,jj,jn) = - fmmflx(ji,jj) * r1_rho0 * ptr(ji,jj,1,jn,Kmm) |
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| 136 | END_2D |
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| 137 | END DO |
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| 138 | ! |
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| 139 | IF( ln_linssh ) THEN !* linear free surface |
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| 140 | DO jn = 1, jptra |
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| 141 | DO_2D( 0, 0, 0, 1 ) |
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| 142 | sbc_trc(ji,jj,jn) = sbc_trc(ji,jj,jn) + r1_rho0 * emp(ji,jj) * ptr(ji,jj,1,jn,Kmm) !==>> add concentration/dilution effect due to constant volume cell |
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| 143 | END_2D |
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| 144 | END DO |
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| 145 | ENDIF |
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| 146 | ! |
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| 147 | CASE ( 1 ) ! Specific treatment of sea ice fluxes with an imposed concentration in sea ice |
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| 148 | ! |
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| 149 | DO jn = 1, jptra |
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| 150 | DO_2D( 0, 0, 0, 1 ) |
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| 151 | sbc_trc(ji,jj,jn) = - fmmflx(ji,jj) * r1_rho0 * trc_i(ji,jj,jn) |
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| 152 | END_2D |
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| 153 | END DO |
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| 154 | ! |
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| 155 | IF( ln_linssh ) THEN !* linear free surface |
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| 156 | DO jn = 1, jptra |
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| 157 | DO_2D( 0, 0, 0, 1 ) |
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| 158 | sbc_trc(ji,jj,jn) = sbc_trc(ji,jj,jn) + r1_rho0 * emp(ji,jj) * ptr(ji,jj,1,jn,Kmm) !==>> add concentration/dilution effect due to constant volume cell |
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| 159 | END_2D |
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| 160 | END DO |
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| 161 | ENDIF |
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| 162 | ! |
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| 163 | DO jn = 1, jptra |
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| 164 | DO_2D( 0, 0, 0, 1 ) |
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| 165 | zse3t = rDt_trc / e3t(ji,jj,1,Kmm) |
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| 166 | zdtra = ptr(ji,jj,1,jn,Kmm) + sbc_trc(ji,jj,jn) * zse3t |
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| 167 | IF( zdtra < 0. ) sbc_trc(ji,jj,jn) = MAX( zdtra, -ptr(ji,jj,1,jn,Kmm) / zse3t ) ! avoid negative concentration that can occurs if trc_i > ptr |
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| 168 | END_2D |
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| 169 | END DO |
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| 170 | ! |
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| 171 | END SELECT |
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| 172 | ! |
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| 173 | CALL lbc_lnk( 'trcsbc', sbc_trc(:,:,:), 'T', 1.0_wp ) |
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| 174 | ! Concentration dilution effect on tracers due to evaporation & precipitation |
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| 175 | DO jn = 1, jptra |
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| 176 | ! |
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| 177 | IF( l_trdtrc ) ztrtrd(:,:,:) = ptr(:,:,:,jn,Krhs) ! save trends |
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| 178 | ! |
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| 179 | DO_2D( 0, 0, 0, 1 ) |
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| 180 | zse3t = zfact / e3t(ji,jj,1,Kmm) |
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| 181 | ptr(ji,jj,1,jn,Krhs) = ptr(ji,jj,1,jn,Krhs) + ( sbc_trc_b(ji,jj,jn) + sbc_trc(ji,jj,jn) ) * zse3t |
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| 182 | END_2D |
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| 183 | ! |
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| 184 | IF( l_trdtrc ) THEN |
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| 185 | ztrtrd(:,:,:) = ptr(:,:,:,jn,Krhs) - ztrtrd(:,:,:) |
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| 186 | CALL trd_tra( kt, Kmm, Krhs, 'TRC', jn, jptra_nsr, ztrtrd ) |
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| 187 | END IF |
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| 188 | ! ! =========== |
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| 189 | END DO ! tracer loop |
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| 190 | ! ! =========== |
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| 191 | ! |
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| 192 | ! Write in the tracer restar file |
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| 193 | ! ******************************* |
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| 194 | IF( lrst_trc .AND. .NOT.ln_top_euler ) THEN |
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| 195 | IF(lwp) WRITE(numout,*) |
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| 196 | IF(lwp) WRITE(numout,*) 'sbc : ocean surface tracer content forcing fields written in tracer restart file ', & |
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| 197 | & 'at it= ', kt,' date= ', ndastp |
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| 198 | IF(lwp) WRITE(numout,*) '~~~~' |
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| 199 | DO jn = 1, jptra |
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| 200 | CALL iom_rstput( kt, nitrst, numrtw, 'sbc_'//TRIM(ctrcnm(jn))//'_b', sbc_trc(:,:,jn) ) |
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| 201 | END DO |
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| 202 | ENDIF |
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| 203 | ! |
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| 204 | IF( sn_cfctl%l_prttrc ) THEN |
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| 205 | WRITE(charout, FMT="('sbc ')") ; CALL prt_ctl_info( charout, cdcomp = 'top' ) |
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| 206 | CALL prt_ctl( tab4d_1=ptr(:,:,:,:,Krhs), mask1=tmask, clinfo=ctrcnm, clinfo3='trd' ) |
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| 207 | ENDIF |
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| 208 | IF( l_trdtrc ) DEALLOCATE( ztrtrd ) |
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| 209 | ! |
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| 210 | IF( ln_timing ) CALL timing_stop('trc_sbc') |
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| 211 | ! |
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| 212 | END SUBROUTINE trc_sbc |
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| 213 | |
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| 214 | |
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| 215 | SUBROUTINE trc_sbc_RK3 ( kt, Kmm, ptr, Krhs, kstg ) |
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| 216 | !!---------------------------------------------------------------------- |
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| 217 | !! *** ROUTINE trc_sbc_RK3 *** |
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| 218 | !! |
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| 219 | !! ** Purpose : Compute the tracer surface boundary condition trend of |
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| 220 | !! (concentration/dilution effect) and add it to the general |
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| 221 | !! trend of tracer equations. |
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| 222 | !! |
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| 223 | !! ** Method : |
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| 224 | !! * concentration/dilution effect: |
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| 225 | !! The surface freshwater flux modify the ocean volume |
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| 226 | !! and thus the concentration of a tracer as : |
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| 227 | !! tr(Krhs) = tr(Krhs) + emp * tr(Kmm) / e3t_ for k=1 |
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| 228 | !! where emp, the surface freshwater budget (evaporation minus |
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| 229 | !! precipitation ) given in kg/m2/s is divided |
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| 230 | !! by 1035 kg/m3 (density of ocean water) to obtain m/s. |
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| 231 | !! |
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| 232 | !! ** Action : - Update the 1st level of tr(:,:,:,:,Krhs) with the trend associated |
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| 233 | !! with the tracer surface boundary condition |
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| 234 | !! |
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| 235 | !!---------------------------------------------------------------------- |
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| 236 | INTEGER , INTENT(in ) :: kt, Kmm, Krhs ! ocean time-step and time-level indices |
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| 237 | INTEGER , INTENT(in ) :: kstg ! RK3 stage index |
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| 238 | REAL(wp), DIMENSION(jpi,jpj,jpk,jptra,jpt), INTENT(inout) :: ptr ! passive tracers and RHS of tracer equation |
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| 239 | ! |
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| 240 | INTEGER :: ji, jj, jn ! dummy loop indices |
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| 241 | REAL(wp) :: z1_rho0_e3t ! local scalars |
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| 242 | REAL(wp) :: zftra, zdtra, ztfx ! - - |
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| 243 | CHARACTER (len=22) :: charout |
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| 244 | REAL(wp), ALLOCATABLE, DIMENSION(:,:,:) :: ztrtrd |
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| 245 | !!--------------------------------------------------------------------- |
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| 246 | ! |
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| 247 | IF( ln_timing ) CALL timing_start('trc_sbc_RK3') |
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| 248 | ! |
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| 249 | IF( kt == nittrc000 ) THEN |
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| 250 | IF(lwp) WRITE(numout,*) |
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| 251 | IF(lwp) WRITE(numout,*) 'trc_sbc_RK3 : Passive tracers surface boundary condition' |
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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 | !!st note that trc_sbc can be removed only re-use in atf (not relevant for RK3) |
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| 256 | SELECT CASE( kstg ) |
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| 257 | ! |
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| 258 | CASE( 1 , 2 ) != stage 1 and 2 =! only in non linear ssh |
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| 259 | ! |
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| 260 | IF( .NOT.ln_linssh ) THEN !* only passive tracer fluxes associated with mass fluxes |
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| 261 | ! ! no passive tracer concentration modification due to ssh variation |
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| 262 | !!st emp includes fmm see iceupdate.F90 |
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| 263 | !!not sure about trc_i case... (1) |
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| 264 | DO jn = 1, jptra |
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| 265 | DO_2D( 0, 0, 0, 0 ) !!st WHY 1 : exterior here ? |
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| 266 | z1_rho0_e3t = r1_rho0 / e3t(ji,jj,1,Kmm) |
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| 267 | ptr(ji,jj,1,jn,Krhs) = ptr(ji,jj,1,jn,Krhs) - emp(ji,jj) * ptr(ji,jj,1,jn,Kmm) * z1_rho0_e3t |
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| 268 | END_2D |
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| 269 | END DO |
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| 270 | ! |
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| 271 | ENDIF |
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| 272 | ! |
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| 273 | CASE( 3 ) |
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| 274 | ! |
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| 275 | ! Allocate temporary workspace |
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| 276 | IF( l_trdtrc ) ALLOCATE( ztrtrd(jpi,jpj,jpk) ) |
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| 277 | ! |
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| 278 | DO jn = 1, jptra |
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| 279 | IF( l_trdtrc ) ztrtrd(:,:,:) = ptr(:,:,:,jn,Krhs) ! save trends |
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| 280 | END DO |
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| 281 | ! |
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| 282 | IF( ln_linssh ) THEN !* linear free surface (add concentration/dilution effect artificially since no volume variation) |
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| 283 | ! |
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| 284 | SELECT CASE ( nn_ice_tr ) |
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| 285 | ! |
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| 286 | CASE ( -1 ) ! No tracers in sea ice (null concentration in sea ice) |
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| 287 | ! |
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| 288 | DO jn = 1, jptra |
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| 289 | DO_2D( 0, 0, 0, 0 ) |
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| 290 | z1_rho0_e3t = r1_rho0 / e3t(ji,jj,1,Kmm) |
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| 291 | ptr(ji,jj,1,jn,Krhs) = ptr(ji,jj,1,jn,Krhs) + emp(ji,jj) * r1_rho0 * ptr(ji,jj,1,jn,Kmm) |
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| 292 | END_2D |
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| 293 | END DO |
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| 294 | ! |
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| 295 | CASE ( 0 ) ! Same concentration in sea ice and in the ocean fmm contribution to concentration/dilution effect has to be removed |
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| 296 | ! |
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| 297 | DO jn = 1, jptra |
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| 298 | DO_2D( 0, 0, 0, 1 ) |
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| 299 | z1_rho0_e3t = r1_rho0 / e3t(ji,jj,1,Kmm) |
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| 300 | ptr(ji,jj,1,jn,Krhs) = ptr(ji,jj,1,jn,Krhs) + ( emp(ji,jj) - fmmflx(ji,jj) ) * r1_rho0 * ptr(ji,jj,1,jn,Kmm) |
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| 301 | END_2D |
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| 302 | END DO |
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| 303 | ! |
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| 304 | CASE ( 1 ) ! Specific treatment of sea ice fluxes with an imposed concentration in sea ice !!st TODO : check Christian new implementation |
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| 305 | ! |
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| 306 | DO jn = 1, jptra |
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| 307 | DO_2D( 0, 0, 0, 0 ) |
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| 308 | z1_rho0_e3t = r1_rho0 / e3t(ji,jj,1,Kmm) |
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| 309 | ! tracer flux at the ice/ocean interface (tracer/m2/s) |
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| 310 | zftra = - trc_i(ji,jj,jn) * fmmflx(ji,jj) ! uptake of tracer in the sea ice |
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| 311 | ! ! only used in the levitating sea ice case |
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| 312 | ! tracer flux only : add concentration dilution term in net tracer flux, no F-M in volume flux |
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| 313 | ! tracer and mass fluxes : no concentration dilution term in net tracer flux, F-M term in volume flux |
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| 314 | ztfx = zftra ! net tracer flux |
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| 315 | ! |
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| 316 | zdtra = r1_rho0 * ( ztfx + ( emp(ji,jj) - fmmflx(ji,jj) ) * ptr(ji,jj,1,jn,Kmm) ) |
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| 317 | IF ( zdtra < 0. ) THEN |
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| 318 | zdtra = MAX(zdtra, -ptr(ji,jj,1,jn,Kmm) * e3t(ji,jj,1,Kmm) / rDt_trc ) ! avoid negative concentrations to arise |
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| 319 | ENDIF |
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| 320 | ptr(ji,jj,1,jn,Krhs) = ptr(ji,jj,1,jn,Krhs) + zdtra |
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| 321 | END_2D |
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| 322 | END DO |
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| 323 | ! |
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| 324 | END SELECT |
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| 325 | ! |
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| 326 | ELSE !* non linear free surface (concentration/dilution effect due to volume variation) |
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| 327 | ! |
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| 328 | SELECT CASE ( nn_ice_tr ) |
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| 329 | ! CASE ( -1 ) natural concentration/dilution effect due to volume variation : nothing to do |
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| 330 | ! |
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| 331 | CASE ( 0 ) ! Same concentration in sea ice and in the ocean : correct concentration/dilution effect due to "freezing - melting" |
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| 332 | ! |
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| 333 | DO jn = 1, jptra |
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| 334 | DO_2D( 0, 0, 0, 1 ) |
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| 335 | z1_rho0_e3t = r1_rho0 / e3t(ji,jj,1,Kmm) |
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| 336 | ptr(ji,jj,1,jn,Krhs) = ptr(ji,jj,1,jn,Krhs) - fmmflx(ji,jj) * r1_rho0 * ptr(ji,jj,1,jn,Kmm) |
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| 337 | END_2D |
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| 338 | END DO |
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| 339 | ! |
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| 340 | CASE ( 1 ) ! Specific treatment of sea ice fluxes with an imposed concentration in sea ice |
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| 341 | ! |
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| 342 | DO jn = 1, jptra |
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| 343 | DO_2D( 0, 0, 0, 0 ) |
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| 344 | ! tracer flux at the ice/ocean interface (tracer/m2/s) |
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| 345 | zftra = - trc_i(ji,jj,jn) * fmmflx(ji,jj) ! uptake of tracer in the sea ice |
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| 346 | ! ! only used in the levitating sea ice case |
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| 347 | ! tracer flux only : add concentration dilution term in net tracer flux, no F-M in volume flux |
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| 348 | ! tracer and mass fluxes : no concentration dilution term in net tracer flux, F-M term in volume flux |
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| 349 | ztfx = zftra ! net tracer flux |
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| 350 | ! |
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| 351 | zdtra = r1_rho0 * ( ztfx - fmmflx(ji,jj) * ptr(ji,jj,1,jn,Kmm) ) |
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| 352 | IF ( zdtra < 0. ) THEN |
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| 353 | zdtra = MAX(zdtra, -ptr(ji,jj,1,jn,Kmm) * e3t(ji,jj,1,Kmm) / rDt_trc ) ! avoid negative concentrations to arise |
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| 354 | ENDIF |
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| 355 | ptr(ji,jj,1,jn,Krhs) = ptr(ji,jj,1,jn,Krhs) + zdtra |
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| 356 | END_2D |
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| 357 | END DO |
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| 358 | ! |
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| 359 | END SELECT |
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| 360 | ! |
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| 361 | ENDIF |
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| 362 | ! |
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| 363 | ! |
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| 364 | !!st useless trc_sbc only in the interior even in MLF case CALL lbc_lnk( 'trcsbc', sbc_trc(:,:,:), 'T', 1.0_wp ) |
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| 365 | ! Concentration dilution effect on tracers due to evaporation & precipitation |
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| 366 | DO jn = 1, jptra |
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| 367 | ! |
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| 368 | IF(lwp) WRITE(numout,*) |
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| 369 | IF(lwp) WRITE(numout,*) 'trc_sbc_RK3 : Runge Kutta 3rd order at stage ', kstg, jn |
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| 370 | IF(lwp) WRITE(numout,*) |
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| 371 | ! |
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| 372 | IF( l_trdtrc ) THEN |
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| 373 | ztrtrd(:,:,:) = ptr(:,:,:,jn,Krhs) - ztrtrd(:,:,:) |
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| 374 | CALL trd_tra( kt, Kmm, Krhs, 'TRC', jn, jptra_nsr, ztrtrd ) |
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| 375 | END IF |
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| 376 | ! |
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| 377 | END DO |
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| 378 | ! |
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| 379 | IF( l_trdtrc ) DEALLOCATE( ztrtrd ) |
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| 380 | ! |
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| 381 | END SELECT |
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| 382 | ! |
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| 383 | IF( sn_cfctl%l_prttrc ) THEN |
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| 384 | WRITE(charout, FMT="('sbc ')") ; CALL prt_ctl_info( charout, cdcomp = 'top' ) |
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| 385 | CALL prt_ctl( tab4d_1=ptr(:,:,:,:,Krhs), mask1=tmask, clinfo=ctrcnm, clinfo3='trd' ) |
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| 386 | ENDIF |
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| 387 | ! |
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| 388 | IF( ln_timing ) CALL timing_stop('trc_sbc_RK3') |
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| 389 | ! |
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| 390 | END SUBROUTINE trc_sbc_RK3 |
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| 391 | |
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| 392 | |
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| 393 | #else |
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| 394 | !!---------------------------------------------------------------------- |
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| 395 | !! Dummy module : NO passive tracer |
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| 396 | !!---------------------------------------------------------------------- |
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| 397 | USE par_oce |
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| 398 | USE par_trc |
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| 399 | CONTAINS |
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| 400 | SUBROUTINE trc_sbc ( kt, Kmm, ptr, Krhs ) ! Empty routine |
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| 401 | INTEGER, INTENT(in ) :: kt ! ocean time-step index |
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| 402 | INTEGER, INTENT(in ) :: Kmm, Krhs ! time level indices |
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| 403 | REAL(wp), DIMENSION(jpi,jpj,jpk,jptra,jpt), INTENT(inout) :: ptr ! passive tracers and RHS of tracer equation |
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| 404 | WRITE(*,*) 'trc_sbc: You should not have seen this print! error?', kt |
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| 405 | END SUBROUTINE trc_sbc |
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| 406 | #endif |
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| 407 | |
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| 408 | !!====================================================================== |
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| 409 | END MODULE trcsbc |
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