MODULE tranpc !!============================================================================== !! *** MODULE tranpc *** !! Ocean active tracers: non penetrative convective adjustment scheme !!============================================================================== !! History : 1.0 ! 1990-09 (G. Madec) Original code !! ! 1996-01 (G. Madec) statement function for e3 !! NEMO 1.0 ! 2002-06 (G. Madec) free form F90 !! 3.0 ! 2008-06 (G. Madec) applied on ta, sa and called before tranxt in step.F90 !! 3.3 ! 2010-05 (C. Ethe, G. Madec) merge TRC-TRA !! 3.6 ! 2015-05 (L. Brodeau) new algorithm based on local Brunt-Vaisala freq. !!---------------------------------------------------------------------- !!---------------------------------------------------------------------- !! tra_npc : apply the non penetrative convection scheme !!---------------------------------------------------------------------- USE oce ! ocean dynamics and active tracers USE dom_oce ! ocean space and time domain USE phycst ! physical constants USE zdf_oce ! ocean vertical physics USE trd_oce ! ocean active tracer trends USE trdtra ! ocean active tracer trends USE eosbn2 ! equation of state (eos routine) ! USE lbclnk ! lateral boundary conditions (or mpp link) USE in_out_manager ! I/O manager USE lib_mpp ! MPP library USE wrk_nemo ! Memory Allocation USE timing ! Timing IMPLICIT NONE PRIVATE PUBLIC tra_npc ! routine called by step.F90 !! * Substitutions # include "domzgr_substitute.h90" # include "vectopt_loop_substitute.h90" !!---------------------------------------------------------------------- !! NEMO/OPA 3.6 , NEMO Consortium (2014) !! $Id$ !! Software governed by the CeCILL licence (NEMOGCM/NEMO_CeCILL.txt) !!---------------------------------------------------------------------- CONTAINS SUBROUTINE tra_npc( kt ) !!---------------------------------------------------------------------- !! *** ROUTINE tranpc *** !! !! ** Purpose : Non-penetrative convective adjustment scheme. solve !! the static instability of the water column on after fields !! while conserving heat and salt contents. !! !! ** Method : updated algorithm able to deal with non-linear equation of state !! (i.e. static stability computed locally) !! !! ** Action : - (ta,sa) after the application od the npc scheme !! - send the associated trends for on-line diagnostics (l_trdtra=T) !! !! References : Madec, et al., 1991, JPO, 21, 9, 1349-1371. !!---------------------------------------------------------------------- INTEGER, INTENT(in) :: kt ! ocean time-step index ! INTEGER :: ji, jj, jk ! dummy loop indices INTEGER :: inpcc ! number of statically instable water column INTEGER :: jiter, ikbot, ikp, ikup, ikdown, ilayer, ik_low ! local integers LOGICAL :: l_bottom_reached, l_column_treated REAL(wp) :: zta, zalfa, zsum_temp, zsum_alfa, zaw, zdz, zsum_z REAL(wp) :: zsa, zbeta, zsum_sali, zsum_beta, zbw, zrw, z1_r2dt REAL(wp), PARAMETER :: zn2_zero = 1.e-14_wp ! acceptance criteria for neutrality (N2==0) REAL(wp), POINTER, DIMENSION(:) :: zvn2 ! vertical profile of N2 at 1 given point... REAL(wp), POINTER, DIMENSION(:,:) :: zvts ! vertical profile of T and S at 1 given point... REAL(wp), POINTER, DIMENSION(:,:) :: zvab ! vertical profile of alpha and beta REAL(wp), POINTER, DIMENSION(:,:,:) :: zn2 ! N^2 REAL(wp), POINTER, DIMENSION(:,:,:,:) :: zab ! alpha and beta REAL(wp), POINTER, DIMENSION(:,:,:) :: ztrdt, ztrds ! 3D workspace ! LOGICAL, PARAMETER :: l_LB_debug = .FALSE. ! set to true if you want to follow what is INTEGER :: ilc1, jlc1, klc1, nncpu ! actually happening in a water column at point "ilc1, jlc1" LOGICAL :: lp_monitor_point = .FALSE. ! in CPU domain "nncpu" !!---------------------------------------------------------------------- ! IF( nn_timing == 1 ) CALL timing_start('tra_npc') ! IF( MOD( kt, nn_npc ) == 0 ) THEN ! CALL wrk_alloc( jpi, jpj, jpk, zn2 ) ! N2 CALL wrk_alloc( jpi, jpj, jpk, 2, zab ) ! Alpha and Beta CALL wrk_alloc( jpk, 2, zvts, zvab ) ! 1D column vector at point ji,jj CALL wrk_alloc( jpk, zvn2 ) ! 1D column vector at point ji,jj IF( l_trdtra ) THEN !* Save initial after fields CALL wrk_alloc( jpi, jpj, jpk, ztrdt, ztrds ) ztrdt(:,:,:) = tsa(:,:,:,jp_tem) ztrds(:,:,:) = tsa(:,:,:,jp_sal) ENDIF IF( l_LB_debug ) THEN ! Location of 1 known convection site to follow what's happening in the water column ilc1 = 45 ; jlc1 = 3 ; ! ORCA2 4x4, Antarctic coast, more than 2 unstable portions in the water column... nncpu = 1 ; ! the CPU domain contains the convection spot klc1 = mbkt(ilc1,jlc1) ! bottom of the ocean for debug point... ENDIF CALL eos_rab( tsa, zab ) ! after alpha and beta (given on T-points) CALL bn2 ( tsa, zab, zn2 ) ! after Brunt-Vaisala (given on W-points) inpcc = 0 DO jj = 2, jpjm1 ! interior column only DO ji = fs_2, fs_jpim1 ! IF( tmask(ji,jj,2) == 1 ) THEN ! At least 2 ocean points ! ! consider one ocean column zvts(:,jp_tem) = tsa(ji,jj,:,jp_tem) ! temperature zvts(:,jp_sal) = tsa(ji,jj,:,jp_sal) ! salinity zvab(:,jp_tem) = zab(ji,jj,:,jp_tem) ! Alpha zvab(:,jp_sal) = zab(ji,jj,:,jp_sal) ! Beta zvn2(:) = zn2(ji,jj,:) ! N^2 IF( l_LB_debug ) THEN !LB debug: lp_monitor_point = .FALSE. IF( ( ji == ilc1 ).AND.( jj == jlc1 ) ) lp_monitor_point = .TRUE. ! writing only if on CPU domain where conv region is: lp_monitor_point = (narea == nncpu).AND.lp_monitor_point ENDIF !LB debug end ikbot = mbkt(ji,jj) ! ikbot: ocean bottom T-level ikp = 1 ! because N2 is irrelevant at the surface level (will start at ikp=2) ilayer = 0 jiter = 0 l_column_treated = .FALSE. DO WHILE ( .NOT. l_column_treated ) ! jiter = jiter + 1 IF( jiter >= 400 ) EXIT l_bottom_reached = .FALSE. DO WHILE ( .NOT. l_bottom_reached ) ikp = ikp + 1 !! Testing level ikp for instability !! ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~ IF( zvn2(ikp) < -zn2_zero ) THEN ! Instability found! ilayer = ilayer + 1 ! yet another instable portion of the water column found.... IF( lp_monitor_point ) THEN WRITE(numout,*) IF( ilayer == 1 .AND. jiter == 1 ) THEN ! first time a column is spoted with an instability WRITE(numout,*) WRITE(numout,*) 'Time step = ',kt,' !!!' ENDIF WRITE(numout,*) ' * Iteration #',jiter,': found instable portion #',ilayer, & & ' in column! Starting at ikp =', ikp WRITE(numout,*) ' *** N2 for point (i,j) = ',ji,' , ',jj DO jk = 1, klc1 WRITE(numout,*) jk, zvn2(jk) END DO WRITE(numout,*) ENDIF IF( jiter == 1 ) inpcc = inpcc + 1 IF( lp_monitor_point ) WRITE(numout, *) 'Negative N2 at ikp =',ikp,' for layer #', ilayer !! ikup is the uppermost point where mixing will start: ikup = ikp - 1 ! ikup is always "at most at ikp-1", less if neutral levels overlying !! If the points above ikp-1 have N2 == 0 they must also be mixed: IF( ikp > 2 ) THEN DO jk = ikp-1, 2, -1 IF( ABS(zvn2(jk)) < zn2_zero ) THEN ikup = ikup - 1 ! 1 more upper level has N2=0 and must be added for the mixing ELSE EXIT ENDIF END DO ENDIF IF( ikup < 1 ) CALL ctl_stop( 'tra_npc : PROBLEM #1') zsum_temp = 0._wp zsum_sali = 0._wp zsum_alfa = 0._wp zsum_beta = 0._wp zsum_z = 0._wp DO jk = ikup, ikbot ! Inside the instable (and overlying neutral) portion of the column ! zdz = fse3t(ji,jj,jk) zsum_temp = zsum_temp + zvts(jk,jp_tem)*zdz zsum_sali = zsum_sali + zvts(jk,jp_sal)*zdz zsum_alfa = zsum_alfa + zvab(jk,jp_tem)*zdz zsum_beta = zsum_beta + zvab(jk,jp_sal)*zdz zsum_z = zsum_z + zdz ! IF( jk == ikbot ) EXIT ! avoid array-index overshoot in case ikbot = jpk, cause we're calling jk+1 next line !! EXIT when we have reached the last layer that is instable (N2<0) or neutral (N2=0): IF( zvn2(jk+1) > zn2_zero ) EXIT END DO ikdown = jk ! for the current unstable layer, ikdown is the deepest point with a negative or neutral N2 IF( ikup == ikdown ) CALL ctl_stop( 'tra_npc : PROBLEM #2') ! Mixing Temperature, salinity, alpha and beta from ikup to ikdown included: zta = zsum_temp/zsum_z zsa = zsum_sali/zsum_z zalfa = zsum_alfa/zsum_z zbeta = zsum_beta/zsum_z IF( lp_monitor_point ) THEN WRITE(numout,*) 'MIXED T, S, alfa and beta between ikup =',ikup, & & ' and ikdown =',ikdown,', in layer #',ilayer WRITE(numout,*) ' => Mean temp. in that portion =', zta WRITE(numout,*) ' => Mean sali. in that portion =', zsa WRITE(numout,*) ' => Mean Alfa in that portion =', zalfa WRITE(numout,*) ' => Mean Beta in that portion =', zbeta ENDIF !! Homogenaizing the temperature, salinity, alpha and beta in this portion of the column DO jk = ikup, ikdown zvts(jk,jp_tem) = zta zvts(jk,jp_sal) = zsa zvab(jk,jp_tem) = zalfa zvab(jk,jp_sal) = zbeta END DO !! Updating N2 in the relvant portion of the water column !! Temperature, Salinity, Alpha and Beta have been homogenized in the unstable portion !! => Need to re-compute N2! will use Alpha and Beta! ikup = MAX(2,ikup) ! ikup can never be 1 ! ik_low = MIN(ikdown+1,ikbot) ! we must go 1 point deeper than ikdown! DO jk = ikup, ik_low ! we must go 1 point deeper than ikdown! !! Interpolating alfa and beta at W point: zrw = (fsdepw(ji,jj,jk ) - fsdept(ji,jj,jk)) & & / (fsdept(ji,jj,jk-1) - fsdept(ji,jj,jk)) zaw = zvab(jk,jp_tem) * (1._wp - zrw) + zvab(jk-1,jp_tem) * zrw zbw = zvab(jk,jp_sal) * (1._wp - zrw) + zvab(jk-1,jp_sal) * zrw !! N2 at W point, doing exactly as in eosbn2.F90: zvn2(jk) = grav*( zaw * ( zvts(jk-1,jp_tem) - zvts(jk,jp_tem) ) & & - zbw * ( zvts(jk-1,jp_sal) - zvts(jk,jp_sal) ) ) & & / fse3w(ji,jj,jk) * tmask(ji,jj,jk) !! OR, faster => just considering the vertical gradient of density !! as only the signa maters... !zvn2(jk) = ( zaw * ( zvts(jk-1,jp_tem) - zvts(jk,jp_tem) ) & ! & - zbw * ( zvts(jk-1,jp_sal) - zvts(jk,jp_sal) ) ) END DO ikp = MIN(ikdown+1,ikbot) ENDIF !IF( zvn2(ikp) < 0. ) IF( ikp == ikbot ) l_bottom_reached = .TRUE. ! END DO ! DO WHILE ( .NOT. l_bottom_reached ) IF( ikp /= ikbot ) CALL ctl_stop( 'tra_npc : PROBLEM #3') ! ******* At this stage ikp == ikbot ! ******* IF( ilayer > 0 ) THEN !! least an unstable layer has been found ! IF( lp_monitor_point ) THEN WRITE(numout,*) WRITE(numout,*) 'After ',jiter,' iteration(s), we neutralized ',ilayer,' instable layer(s)' WRITE(numout,*) ' ==> N2 at i,j=',ji,',',jj,' now looks like this:' DO jk = 1, klc1 WRITE(numout,*) jk, zvn2(jk) END DO WRITE(numout,*) ENDIF ! ikp = 1 ! starting again at the surface for the next iteration ilayer = 0 ENDIF ! IF( ikp >= ikbot ) l_column_treated = .TRUE. ! END DO ! DO WHILE ( .NOT. l_column_treated ) !! Updating tsa: tsa(ji,jj,:,jp_tem) = zvts(:,jp_tem) tsa(ji,jj,:,jp_sal) = zvts(:,jp_sal) !! LB: Potentially some other global variable beside theta and S can be treated here !! like BGC tracers. IF( lp_monitor_point ) WRITE(numout,*) ENDIF ! IF( tmask(ji,jj,3) == 1 ) THEN END DO ! ji END DO ! jj ! IF( l_trdtra ) THEN ! send the Non penetrative mixing trends for diagnostic z1_r2dt = 1._wp / (2._wp * rdt) ztrdt(:,:,:) = ( tsa(:,:,:,jp_tem) - ztrdt(:,:,:) ) * z1_r2dt ztrds(:,:,:) = ( tsa(:,:,:,jp_sal) - ztrds(:,:,:) ) * z1_r2dt CALL trd_tra( kt, 'TRA', jp_tem, jptra_npc, ztrdt ) CALL trd_tra( kt, 'TRA', jp_sal, jptra_npc, ztrds ) CALL wrk_dealloc( jpi, jpj, jpk, ztrdt, ztrds ) ENDIF ! CALL lbc_lnk( tsa(:,:,:,jp_tem), 'T', 1. ) ; CALL lbc_lnk( tsa(:,:,:,jp_sal), 'T', 1. ) ! IF( lwp .AND. l_LB_debug ) THEN WRITE(numout,*) 'Exiting tra_npc , kt = ',kt,', => numb. of statically instable water-columns: ', inpcc WRITE(numout,*) ENDIF ! CALL wrk_dealloc(jpi, jpj, jpk, zn2 ) CALL wrk_dealloc(jpi, jpj, jpk, 2, zab ) CALL wrk_dealloc(jpk, zvn2 ) CALL wrk_dealloc(jpk, 2, zvts, zvab ) ! ENDIF ! IF( MOD( kt, nn_npc ) == 0 ) THEN ! IF( nn_timing == 1 ) CALL timing_stop('tra_npc') ! END SUBROUTINE tra_npc !!====================================================================== END MODULE tranpc