| [3] | 1 | MODULE trasbc |
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| 2 | !!============================================================================== |
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| 3 | !! *** MODULE trasbc *** |
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| 4 | !! Ocean active tracers: surface boundary condition |
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| 5 | !!============================================================================== |
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| [503] | 6 | !! History : 8.2 ! 98-10 (G. Madec, G. Roullet, M. Imbard) Original code |
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| 7 | !! 8.2 ! 01-02 (D. Ludicone) sea ice and free surface |
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| 8 | !! 8.5 ! 02-06 (G. Madec) F90: Free form and module |
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| [3] | 9 | !!---------------------------------------------------------------------- |
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| [503] | 10 | |
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| 11 | !!---------------------------------------------------------------------- |
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| [3] | 12 | !! tra_sbc : update the tracer trend at ocean surface |
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| 13 | !!---------------------------------------------------------------------- |
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| 14 | USE oce ! ocean dynamics and active tracers |
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| [888] | 15 | USE sbc_oce ! surface boundary condition: ocean |
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| [3] | 16 | USE dom_oce ! ocean space domain variables |
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| 17 | USE phycst ! physical constant |
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| [216] | 18 | USE traqsr ! solar radiation penetration |
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| 19 | USE trdmod ! ocean trends |
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| 20 | USE trdmod_oce ! ocean variables trends |
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| [3] | 21 | USE in_out_manager ! I/O manager |
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| [258] | 22 | USE prtctl ! Print control |
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| [1938] | 23 | USE sbcrnf ! River runoff |
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| 24 | USE sbcmod ! ln_rnf |
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| [3] | 25 | |
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| 26 | IMPLICIT NONE |
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| 27 | PRIVATE |
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| 28 | |
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| [503] | 29 | PUBLIC tra_sbc ! routine called by step.F90 |
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| [3] | 30 | |
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| 31 | !! * Substitutions |
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| 32 | # include "domzgr_substitute.h90" |
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| 33 | # include "vectopt_loop_substitute.h90" |
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| 34 | !!---------------------------------------------------------------------- |
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| [247] | 35 | !! OPA 9.0 , LOCEAN-IPSL (2005) |
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| [888] | 36 | !! $Id$ |
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| [503] | 37 | !! Software governed by the CeCILL licence (modipsl/doc/NEMO_CeCILL.txt) |
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| [3] | 38 | !!---------------------------------------------------------------------- |
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| 39 | |
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| 40 | CONTAINS |
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| 41 | |
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| 42 | SUBROUTINE tra_sbc ( kt ) |
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| 43 | !!---------------------------------------------------------------------- |
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| 44 | !! *** ROUTINE tra_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 | !! (flux through the interface, concentration/dilution effect) |
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| 48 | !! and add it to the general trend of tracer equations. |
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| 49 | !! |
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| 50 | !! ** Method : |
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| [664] | 51 | !! Following Roullet and Madec (2000), the air-sea flux can be divided |
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| 52 | !! into three effects: (1) Fext, external forcing; |
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| 53 | !! (2) Fwi, concentration/dilution effect due to water exchanged |
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| 54 | !! at the surface by evaporation, precipitations and runoff (E-P-R); |
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| 55 | !! (3) Fwe, tracer carried with the water that is exchanged. |
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| 56 | !! |
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| 57 | !! Fext, flux through the air-sea interface for temperature and salt: |
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| [3] | 58 | !! - temperature : heat flux q (w/m2). If penetrative solar |
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| 59 | !! radiation q is only the non solar part of the heat flux, the |
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| 60 | !! solar part is added in traqsr.F routine. |
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| 61 | !! ta = ta + q /(rau0 rcp e3t) for k=1 |
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| 62 | !! - salinity : no salt flux |
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| [664] | 63 | !! |
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| 64 | !! The formulation for Fwb and Fwi vary according to the free |
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| 65 | !! surface formulation (linear or variable volume). |
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| 66 | !! * Linear free surface |
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| 67 | !! The surface freshwater flux modifies the ocean volume |
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| [3] | 68 | !! and thus the concentration of a tracer and the temperature. |
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| 69 | !! First order of the effect of surface freshwater exchange |
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| 70 | !! for salinity, it can be neglected on temperature (especially |
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| [664] | 71 | !! as the temperature of precipitations and runoffs is usually |
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| 72 | !! unknown). |
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| [3] | 73 | !! - temperature : we assume that the temperature of both |
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| 74 | !! precipitations and runoffs is equal to the SST, thus there |
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| 75 | !! is no additional flux since in this case, the concentration |
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| 76 | !! dilution effect is balanced by the net heat flux associated |
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| [664] | 77 | !! to the freshwater exchange (Fwe+Fwi=0): |
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| 78 | !! (Tp P - Te E) + SST (P-E) = 0 when Tp=Te=SST |
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| [3] | 79 | !! - salinity : evaporation, precipitation and runoff |
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| [664] | 80 | !! water has a zero salinity (Fwe=0), thus only Fwi remains: |
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| [3] | 81 | !! sa = sa + emp * sn / e3t for k=1 |
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| 82 | !! where emp, the surface freshwater budget (evaporation minus |
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| 83 | !! precipitation minus runoff) given in kg/m2/s is divided |
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| [1739] | 84 | !! by 1035 kg/m3 (density of ocena water) to obtain m/s. |
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| [664] | 85 | !! Note: even though Fwe does not appear explicitly for |
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| 86 | !! temperature in this routine, the heat carried by the water |
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| 87 | !! exchanged through the surface is part of the total heat flux |
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| 88 | !! forcing and must be taken into account in the global heat |
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| 89 | !! balance). |
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| 90 | !! * nonlinear free surface (variable volume, lk_vvl) |
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| 91 | !! contrary to the linear free surface case, Fwi is properly |
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| 92 | !! taken into account by using the true layer thicknesses to |
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| 93 | !! calculate tracer content and advection. There is no need to |
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| 94 | !! deal with it in this routine. |
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| 95 | !! - temperature: Fwe=SST (P-E+R) is added to Fext. |
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| 96 | !! - salinity: Fwe = 0, there is no surface flux of salt. |
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| [3] | 97 | !! |
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| 98 | !! ** Action : - Update the 1st level of (ta,sa) with the trend associated |
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| 99 | !! with the tracer surface boundary condition |
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| 100 | !! - save the trend it in ttrd ('key_trdtra') |
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| [503] | 101 | !!---------------------------------------------------------------------- |
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| 102 | USE oce, ONLY : ztrdt => ua ! use ua as 3D workspace |
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| 103 | USE oce, ONLY : ztrds => va ! use va as 3D workspace |
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| [3] | 104 | !! |
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| [503] | 105 | INTEGER, INTENT(in) :: kt ! ocean time-step index |
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| 106 | !! |
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| [1938] | 107 | INTEGER :: ji, jj, jk ! dummy loop indices |
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| 108 | REAL(wp) :: zta, zsa ! temporary scalars, adjustment to temperature and salinity |
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| 109 | REAL(wp) :: azta, azsa ! temporary scalars, calculations of automatic change to temp & sal due to vvl (done elsewhere) |
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| 110 | REAL(wp) :: zsrau, zse3t, zdep ! temporary scalars, 1/density, 1/height of box, 1/height of effected water column |
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| 111 | REAL(wp) :: dheat, dsalt ! total change of temperature and salinity |
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| 112 | REAL(wp) :: tot_sal1, tot_tmp1 |
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| [3] | 113 | !!---------------------------------------------------------------------- |
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| 114 | |
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| 115 | IF( kt == nit000 ) THEN |
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| 116 | IF(lwp) WRITE(numout,*) |
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| 117 | IF(lwp) WRITE(numout,*) 'tra_sbc : TRAcer Surface Boundary Condition' |
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| 118 | IF(lwp) WRITE(numout,*) '~~~~~~~ ' |
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| 119 | ENDIF |
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| 120 | |
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| [1739] | 121 | zsrau = 1. / rau0 ! initialization |
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| [457] | 122 | #if defined key_zco |
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| 123 | zse3t = 1. / e3t_0(1) |
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| [3] | 124 | #endif |
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| 125 | |
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| [503] | 126 | IF( l_trdtra ) THEN ! Save ta and sa trends |
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| 127 | ztrdt(:,:,:) = ta(:,:,:) |
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| 128 | ztrds(:,:,:) = sa(:,:,:) |
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| [216] | 129 | ENDIF |
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| 130 | |
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| [3] | 131 | IF( .NOT.ln_traqsr ) qsr(:,:) = 0.e0 ! no solar radiation penetration |
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| 132 | |
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| [1938] | 133 | ! Concentration dillution effect on (t,s) due to evapouration, precipitation and qns, but not river runoff |
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| [3] | 134 | DO jj = 2, jpj |
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| 135 | DO ji = fs_2, fs_jpim1 ! vector opt. |
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| [457] | 136 | #if ! defined key_zco |
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| [3] | 137 | zse3t = 1. / fse3t(ji,jj,1) |
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| 138 | #endif |
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| [592] | 139 | IF( lk_vvl) THEN |
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| [1938] | 140 | zta = ro0cpr * qns(ji,jj) * zse3t & ! temperature : heat flux |
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| 141 | & - emp(ji,jj) * zsrau * tn(ji,jj,1) * zse3t ! & cooling/heating effet of EMP flux |
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| [592] | 142 | zsa = 0.e0 ! No salinity concent./dilut. effect |
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| 143 | ELSE |
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| [1938] | 144 | zta = ro0cpr * qns(ji,jj) * zse3t ! temperature : heat flux |
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| 145 | zsa = emps(ji,jj) * zsrau * sn(ji,jj,1) * zse3t ! salinity : concent./dilut. effect |
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| [592] | 146 | ENDIF |
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| 147 | ta(ji,jj,1) = ta(ji,jj,1) + zta ! add the trend to the general tracer trend |
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| [3] | 148 | sa(ji,jj,1) = sa(ji,jj,1) + zsa |
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| 149 | END DO |
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| 150 | END DO |
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| [216] | 151 | |
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| [1938] | 152 | IF ( ln_rnf ) THEN |
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| 153 | ! Concentration / dilution effect on (t,s) due to river runoff |
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| 154 | DO jj=1,jpj |
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| 155 | DO ji=1,jpi |
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| 156 | rnf_dep(ji,jj)=0 |
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| 157 | DO jk=1,rnf_mod_dep(ji,jj) ! recalculates rnf_dep to be the depth |
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| 158 | rnf_dep(ji,jj)=rnf_dep(ji,jj)+fse3t(ji,jj,jk) ! in metres to the bottom of the relevant grid box |
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| 159 | ENDDO |
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| 160 | zdep = 1. / rnf_dep(ji,jj) |
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| 161 | zse3t= 1. / fse3t(ji,jj,1) |
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| 162 | IF ( rnf_tmp(ji,jj) == -999 ) rnf_tmp(ji,jj)=tn(ji,jj,1) ! if not specified set runoff temp to be sst |
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| 163 | |
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| 164 | IF ( rnf(ji,jj) .gt. 0.0 ) THEN |
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| 165 | |
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| 166 | IF( lk_vvl) THEN |
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| 167 | !!!indirect flux, concentration or dilution effect |
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| 168 | !!!force a dilution effect in all levels; |
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| 169 | dheat=0.0 |
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| 170 | dsalt=0.0 |
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| 171 | DO jk=1, rnf_mod_dep(ji,jj) |
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| 172 | zta = -tn(ji,jj,jk) * rnf(ji,jj) * zsrau * zdep |
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| 173 | zsa = -sn(ji,jj,jk) * rnf(ji,jj) * zsrau * zdep |
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| 174 | ta(ji,jj,jk)=ta(ji,jj,jk)+zta |
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| 175 | sa(ji,jj,jk)=sa(ji,jj,jk)+zsa |
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| 176 | dheat=dheat+zta*fse3t(ji,jj,jk) |
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| 177 | dsalt=dsalt+zsa*fse3t(ji,jj,jk) |
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| 178 | ENDDO |
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| 179 | !!!negate this total change in heat and salt content from top level |
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| 180 | zta=-dheat*zse3t |
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| 181 | zsa=-dsalt*zse3t |
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| 182 | ta(ji,jj,1)=ta(ji,jj,1)+zta |
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| 183 | sa(ji,jj,1)=sa(ji,jj,1)+zsa |
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| 184 | |
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| 185 | !!!direct flux |
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| 186 | zta = rnf_tmp(ji,jj) * rnf(ji,jj) * zsrau * zdep |
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| 187 | zsa = rnf_sal(ji,jj) * rnf(ji,jj) * zsrau * zdep |
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| 188 | |
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| 189 | DO jk=1, rnf_mod_dep(ji,jj) |
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| 190 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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| 191 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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| 192 | ENDDO |
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| 193 | |
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| 194 | ELSE |
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| 195 | DO jk=1, rnf_mod_dep(ji,jj) |
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| 196 | zta = ( rnf_tmp(ji,jj)-tn(ji,jj,jk) ) * rnf(ji,jj) * zsrau * zdep |
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| 197 | zsa = ( rnf_sal(ji,jj)-sn(ji,jj,jk) ) * rnf(ji,jj) * zsrau * zdep |
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| 198 | ta(ji,jj,jk) = ta(ji,jj,jk) + zta |
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| 199 | sa(ji,jj,jk) = sa(ji,jj,jk) + zsa |
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| 200 | ENDDO |
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| 201 | ENDIF |
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| 202 | |
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| 203 | ELSEIF (rnf(ji,jj) .lt. 0.) THEN !! for use in baltic when flow is out of domain, want no change in temp and sal |
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| 204 | |
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| 205 | IF( lk_vvl) THEN |
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| 206 | !calculate automatic adjustment to sal and temp due to dilution/concentraion effect |
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| 207 | azta = -tn(ji,jj,1) * rnf(ji,jj) * zsrau * zse3t |
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| 208 | azsa = -sn(ji,jj,1) * rnf(ji,jj) * zsrau * zse3t |
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| 209 | !!!negate this change in sal and temp |
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| 210 | ta(ji,jj,1)=ta(ji,jj,1)-azta |
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| 211 | sa(ji,jj,1)=sa(ji,jj,1)-azsa |
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| 212 | ENDIF |
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| 213 | |
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| 214 | ENDIF |
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| 215 | |
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| 216 | ENDDO |
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| 217 | ENDDO |
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| 218 | |
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| 219 | ENDIF |
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| 220 | |
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| [503] | 221 | IF( l_trdtra ) THEN ! save the sbc trends for diagnostic |
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| 222 | ztrdt(:,:,:) = ta(:,:,:) - ztrdt(:,:,:) |
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| 223 | ztrds(:,:,:) = sa(:,:,:) - ztrds(:,:,:) |
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| 224 | CALL trd_mod(ztrdt, ztrds, jptra_trd_nsr, 'TRA', kt) |
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| [216] | 225 | ENDIF |
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| [503] | 226 | ! |
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| 227 | IF(ln_ctl) CALL prt_ctl( tab3d_1=ta, clinfo1=' sbc - Ta: ', mask1=tmask, & |
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| 228 | & tab3d_2=sa, clinfo2= ' Sa: ', mask2=tmask, clinfo3='tra' ) |
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| 229 | ! |
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| [3] | 230 | END SUBROUTINE tra_sbc |
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| 231 | |
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| 232 | !!====================================================================== |
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| 233 | END MODULE trasbc |
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