Changeset 13497 for NEMO/trunk/src/OCE/DYN
- Timestamp:
- 2020-09-21T14:37:46+02:00 (4 years ago)
- Location:
- NEMO/trunk/src/OCE/DYN
- Files:
-
- 14 edited
-
divhor.F90 (modified) (1 diff)
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dynadv_cen2.F90 (modified) (5 diffs)
-
dynadv_ubs.F90 (modified) (5 diffs)
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dynkeg.F90 (modified) (1 diff)
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dynldf_iso.F90 (modified) (2 diffs)
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dynldf_lap_blp.F90 (modified) (1 diff)
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dynspg.F90 (modified) (4 diffs)
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dynspg_exp.F90 (modified) (1 diff)
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dynspg_ts.F90 (modified) (4 diffs)
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dynvor.F90 (modified) (1 diff)
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dynzad.F90 (modified) (5 diffs)
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dynzdf.F90 (modified) (4 diffs)
-
sshwzv.F90 (modified) (2 diffs)
-
wet_dry.F90 (modified) (1 diff)
Legend:
- Unmodified
- Added
- Removed
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NEMO/trunk/src/OCE/DYN/divhor.F90
r13295 r13497 77 77 ENDIF 78 78 ! 79 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) 79 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) !== Horizontal divergence ==! 80 80 hdiv(ji,jj,jk) = ( e2u(ji ,jj) * e3u(ji ,jj,jk,Kmm) * uu(ji ,jj,jk,Kmm) & 81 81 & - e2u(ji-1,jj) * e3u(ji-1,jj,jk,Kmm) * uu(ji-1,jj,jk,Kmm) & -
NEMO/trunk/src/OCE/DYN/dynadv_cen2.F90
r13295 r13497 72 72 zfu(:,:,jk) = 0.25_wp * e2u(:,:) * e3u(:,:,jk,Kmm) * puu(:,:,jk,Kmm) 73 73 zfv(:,:,jk) = 0.25_wp * e1v(:,:) * e3v(:,:,jk,Kmm) * pvv(:,:,jk,Kmm) 74 DO_2D( 1, 0, 1, 0 ) 74 DO_2D( 1, 0, 1, 0 ) ! horizontal momentum fluxes (at T- and F-point) 75 75 zfu_t(ji+1,jj ,jk) = ( zfu(ji,jj,jk) + zfu(ji+1,jj,jk) ) * ( puu(ji,jj,jk,Kmm) + puu(ji+1,jj ,jk,Kmm) ) 76 76 zfv_f(ji ,jj ,jk) = ( zfv(ji,jj,jk) + zfv(ji+1,jj,jk) ) * ( puu(ji,jj,jk,Kmm) + puu(ji ,jj+1,jk,Kmm) ) … … 78 78 zfv_t(ji ,jj+1,jk) = ( zfv(ji,jj,jk) + zfv(ji,jj+1,jk) ) * ( pvv(ji,jj,jk,Kmm) + pvv(ji ,jj+1,jk,Kmm) ) 79 79 END_2D 80 DO_2D( 0, 0, 0, 0 ) 80 DO_2D( 0, 0, 0, 0 ) ! divergence of horizontal momentum fluxes 81 81 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) - ( zfu_t(ji+1,jj,jk) - zfu_t(ji,jj ,jk) & 82 82 & + zfv_f(ji ,jj,jk) - zfv_f(ji,jj-1,jk) ) * r1_e1e2u(ji,jj) & … … 98 98 ! !== Vertical advection ==! 99 99 ! 100 DO_2D( 0, 0, 0, 0 ) 100 DO_2D( 0, 0, 0, 0 ) ! surface/bottom advective fluxes set to zero 101 101 zfu_uw(ji,jj,jpk) = 0._wp ; zfv_vw(ji,jj,jpk) = 0._wp 102 102 zfu_uw(ji,jj, 1 ) = 0._wp ; zfv_vw(ji,jj, 1 ) = 0._wp … … 109 109 ENDIF 110 110 DO jk = 2, jpkm1 ! interior advective fluxes 111 DO_2D( 0, 1, 0, 1 ) 111 DO_2D( 0, 1, 0, 1 ) ! 1/4 * Vertical transport 112 112 zfw(ji,jj,jk) = 0.25_wp * e1e2t(ji,jj) * ww(ji,jj,jk) 113 113 END_2D … … 117 117 END_2D 118 118 END DO 119 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) 119 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) ! divergence of vertical momentum flux divergence 120 120 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) - ( zfu_uw(ji,jj,jk) - zfu_uw(ji,jj,jk+1) ) * r1_e1e2u(ji,jj) & 121 121 & / e3u(ji,jj,jk,Kmm) -
NEMO/trunk/src/OCE/DYN/dynadv_ubs.F90
r13295 r13497 108 108 zfv(:,:,jk) = e1v(:,:) * e3v(:,:,jk,Kmm) * pvv(:,:,jk,Kmm) 109 109 ! 110 DO_2D( 0, 0, 0, 0 ) 110 DO_2D( 0, 0, 0, 0 ) ! laplacian 111 111 zlu_uu(ji,jj,jk,1) = ( puu (ji+1,jj ,jk,Kbb) - 2.*puu (ji,jj,jk,Kbb) + puu (ji-1,jj ,jk,Kbb) ) * umask(ji,jj,jk) 112 112 zlv_vv(ji,jj,jk,1) = ( pvv (ji ,jj+1,jk,Kbb) - 2.*pvv (ji,jj,jk,Kbb) + pvv (ji ,jj-1,jk,Kbb) ) * vmask(ji,jj,jk) … … 136 136 zfv(:,:,jk) = 0.25_wp * e1v(:,:) * e3v(:,:,jk,Kmm) * pvv(:,:,jk,Kmm) 137 137 ! 138 DO_2D( 1, 0, 1, 0 ) 138 DO_2D( 1, 0, 1, 0 ) ! horizontal momentum fluxes at T- and F-point 139 139 zui = ( puu(ji,jj,jk,Kmm) + puu(ji+1,jj ,jk,Kmm) ) 140 140 zvj = ( pvv(ji,jj,jk,Kmm) + pvv(ji ,jj+1,jk,Kmm) ) … … 168 168 & * ( pvv(ji,jj,jk,Kmm) + pvv(ji+1,jj ,jk,Kmm) - gamma1 * zl_v ) 169 169 END_2D 170 DO_2D( 0, 0, 0, 0 ) 170 DO_2D( 0, 0, 0, 0 ) ! divergence of horizontal momentum fluxes 171 171 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) - ( zfu_t(ji+1,jj,jk) - zfu_t(ji,jj ,jk) & 172 172 & + zfv_f(ji ,jj,jk) - zfv_f(ji,jj-1,jk) ) * r1_e1e2u(ji,jj) & … … 187 187 ! ! Vertical advection ! 188 188 ! ! ==================== ! 189 DO_2D( 0, 0, 0, 0 ) 189 DO_2D( 0, 0, 0, 0 ) ! surface/bottom advective fluxes set to zero 190 190 zfu_uw(ji,jj,jpk) = 0._wp 191 191 zfv_vw(ji,jj,jpk) = 0._wp … … 208 208 END_2D 209 209 END DO 210 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) 210 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) ! divergence of vertical momentum flux divergence 211 211 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) - ( zfu_uw(ji,jj,jk) - zfu_uw(ji,jj,jk+1) ) * r1_e1e2u(ji,jj) & 212 212 & / e3u(ji,jj,jk,Kmm) -
NEMO/trunk/src/OCE/DYN/dynkeg.F90
r13295 r13497 125 125 END SELECT 126 126 ! 127 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) 127 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) !== grad( KE ) added to the general momentum trends ==! 128 128 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) - ( zhke(ji+1,jj ,jk) - zhke(ji,jj,jk) ) / e1u(ji,jj) 129 129 pvv(ji,jj,jk,Krhs) = pvv(ji,jj,jk,Krhs) - ( zhke(ji ,jj+1,jk) - zhke(ji,jj,jk) ) / e2v(ji,jj) -
NEMO/trunk/src/OCE/DYN/dynldf_iso.F90
r13295 r13497 128 128 IF( ln_dynldf_hor .AND. ln_traldf_iso ) THEN 129 129 ! 130 DO_3D( 0, 0, 0, 0, 1, jpk ) 130 DO_3D( 0, 0, 0, 0, 1, jpk ) ! set the slopes of iso-level 131 131 uslp (ji,jj,jk) = - ( gdept(ji+1,jj,jk,Kbb) - gdept(ji ,jj ,jk,Kbb) ) * r1_e1u(ji,jj) * umask(ji,jj,jk) 132 132 vslp (ji,jj,jk) = - ( gdept(ji,jj+1,jk,Kbb) - gdept(ji ,jj ,jk,Kbb) ) * r1_e2v(ji,jj) * vmask(ji,jj,jk) … … 268 268 ! Second derivative (divergence) and add to the general trend 269 269 ! ----------------------------------------------------------- 270 DO_2D( 0, 0, 0, 0 ) 270 DO_2D( 0, 0, 0, 0 ) !!gm Question vectop possible??? !!bug 271 271 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) + ( ziut(ji+1,jj) - ziut(ji,jj ) & 272 272 & + zjuf(ji ,jj) - zjuf(ji,jj-1) ) * r1_e1e2u(ji,jj) & -
NEMO/trunk/src/OCE/DYN/dynldf_lap_blp.F90
r13295 r13497 84 84 END_2D 85 85 ! 86 DO_2D( 0, 0, 0, 0 ) 86 DO_2D( 0, 0, 0, 0 ) ! - curl( curl) + grad( div ) 87 87 pu_rhs(ji,jj,jk) = pu_rhs(ji,jj,jk) + zsign * umask(ji,jj,jk) * ( & ! * by umask is mandatory for dyn_ldf_blp use 88 88 & - ( zcur(ji ,jj) - zcur(ji,jj-1) ) * r1_e2u(ji,jj) / e3u(ji,jj,jk,Kmm) & -
NEMO/trunk/src/OCE/DYN/dynspg.F90
r13295 r13497 102 102 IF( ln_apr_dyn .AND. .NOT.ln_dynspg_ts ) THEN !== Atmospheric pressure gradient (added later in time-split case) ==! 103 103 zg_2 = grav * 0.5 104 DO_2D( 0, 0, 0, 0 ) 104 DO_2D( 0, 0, 0, 0 ) ! gradient of Patm using inverse barometer ssh 105 105 spgu(ji,jj) = spgu(ji,jj) + zg_2 * ( ssh_ib (ji+1,jj) - ssh_ib (ji,jj) & 106 106 & + ssh_ibb(ji+1,jj) - ssh_ibb(ji,jj) ) * r1_e1u(ji,jj) … … 117 117 CALL upd_tide(zt0step, Kmm) 118 118 ! 119 DO_2D( 0, 0, 0, 0 ) 119 DO_2D( 0, 0, 0, 0 ) ! add tide potential forcing 120 120 spgu(ji,jj) = spgu(ji,jj) + grav * ( pot_astro(ji+1,jj) - pot_astro(ji,jj) ) * r1_e1u(ji,jj) 121 121 spgv(ji,jj) = spgv(ji,jj) + grav * ( pot_astro(ji,jj+1) - pot_astro(ji,jj) ) * r1_e2v(ji,jj) … … 124 124 IF (ln_scal_load) THEN 125 125 zld = rn_scal_load * grav 126 DO_2D( 0, 0, 0, 0 ) 126 DO_2D( 0, 0, 0, 0 ) ! add scalar approximation for load potential 127 127 spgu(ji,jj) = spgu(ji,jj) + zld * ( pssh(ji+1,jj,Kmm) - pssh(ji,jj,Kmm) ) * r1_e1u(ji,jj) 128 128 spgv(ji,jj) = spgv(ji,jj) + zld * ( pssh(ji,jj+1,Kmm) - pssh(ji,jj,Kmm) ) * r1_e2v(ji,jj) … … 143 143 ENDIF 144 144 ! 145 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) 145 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) !== Add all terms to the general trend 146 146 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) + spgu(ji,jj) 147 147 pvv(ji,jj,jk,Krhs) = pvv(ji,jj,jk,Krhs) + spgv(ji,jj) -
NEMO/trunk/src/OCE/DYN/dynspg_exp.F90
r13295 r13497 74 74 IF( ln_linssh ) THEN !* linear free surface : add the surface pressure gradient trend 75 75 ! 76 DO_2D( 0, 0, 0, 0 ) 76 DO_2D( 0, 0, 0, 0 ) ! now surface pressure gradient 77 77 spgu(ji,jj) = - grav * ( ssh(ji+1,jj,Kmm) - ssh(ji,jj,Kmm) ) * r1_e1u(ji,jj) 78 78 spgv(ji,jj) = - grav * ( ssh(ji,jj+1,Kmm) - ssh(ji,jj,Kmm) ) * r1_e2v(ji,jj) 79 79 END_2D 80 80 ! 81 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) 81 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) ! Add it to the general trend 82 82 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) + spgu(ji,jj) 83 83 pvv(ji,jj,jk,Krhs) = pvv(ji,jj,jk,Krhs) + spgv(ji,jj) -
NEMO/trunk/src/OCE/DYN/dynspg_ts.F90
r13472 r13497 279 279 ENDIF 280 280 ! 281 DO_2D( 0, 0, 0, 0 ) 281 DO_2D( 0, 0, 0, 0 ) ! Remove coriolis term (and possibly spg) from barotropic trend 282 282 zu_frc(ji,jj) = zu_frc(ji,jj) - zu_trd(ji,jj) * ssumask(ji,jj) 283 283 zv_frc(ji,jj) = zv_frc(ji,jj) - zv_trd(ji,jj) * ssvmask(ji,jj) … … 475 475 ! 476 476 ! ! ocean u- and v-depth at mid-step (separate DO-loops remove the need of a lbc_lnk) 477 DO_2D( 1, 1, 1, 0 ) 477 DO_2D( 1, 1, 1, 0 ) ! not jpi-column 478 478 zhup2_e(ji,jj) = hu_0(ji,jj) + r1_2 * r1_e1e2u(ji,jj) & 479 479 & * ( e1e2t(ji ,jj) * zsshp2_e(ji ,jj) & 480 480 & + e1e2t(ji+1,jj) * zsshp2_e(ji+1,jj) ) * ssumask(ji,jj) 481 481 END_2D 482 DO_2D( 1, 0, 1, 1 ) 482 DO_2D( 1, 0, 1, 1 ) ! not jpj-row 483 483 zhvp2_e(ji,jj) = hv_0(ji,jj) + r1_2 * r1_e1e2v(ji,jj) & 484 484 & * ( e1e2t(ji,jj ) * zsshp2_e(ji,jj ) & … … 1308 1308 !!---------------------------------------------------------------------- 1309 1309 ! 1310 DO_2D( 1, 1, 1, 0 ) 1310 DO_2D( 1, 1, 1, 0 ) ! not jpi-column 1311 1311 IF ( phU(ji,jj) > 0._wp ) THEN ; pUmsk(ji,jj) = pTmsk(ji ,jj) 1312 1312 ELSE ; pUmsk(ji,jj) = pTmsk(ji+1,jj) … … 1316 1316 END_2D 1317 1317 ! 1318 DO_2D( 1, 0, 1, 1 ) 1318 DO_2D( 1, 0, 1, 1 ) ! not jpj-row 1319 1319 IF ( phV(ji,jj) > 0._wp ) THEN ; pVmsk(ji,jj) = pTmsk(ji,jj ) 1320 1320 ELSE ; pVmsk(ji,jj) = pTmsk(ji,jj+1) -
NEMO/trunk/src/OCE/DYN/dynvor.F90
r13295 r13497 246 246 CASE ( np_CRV ) !* Coriolis + relative vorticity 247 247 DO jk = 1, jpkm1 ! Horizontal slab 248 DO_2D( 1, 0, 1, 0 ) 248 DO_2D( 1, 0, 1, 0 ) ! relative vorticity 249 249 zwz(ji,jj,jk) = ( e2v(ji+1,jj) * pv(ji+1,jj,jk) - e2v(ji,jj) * pv(ji,jj,jk) & 250 250 & - e1u(ji,jj+1) * pu(ji,jj+1,jk) + e1u(ji,jj) * pu(ji,jj,jk) ) * r1_e1e2f(ji,jj) -
NEMO/trunk/src/OCE/DYN/dynzad.F90
r13295 r13497 71 71 ENDIF 72 72 73 IF( l_trddyn ) THEN ! Save puu(:,:,:,Krhs) and pvv(:,:,:,Krhs) trends73 IF( l_trddyn ) THEN ! Save puu(:,:,:,Krhs) and pvv(:,:,:,Krhs) trends 74 74 ALLOCATE( ztrdu(jpi,jpj,jpk) , ztrdv(jpi,jpj,jpk) ) 75 75 ztrdu(:,:,:) = puu(:,:,:,Krhs) … … 77 77 ENDIF 78 78 79 DO jk = 2, jpkm1 ! Vertical momentum advection at level w and u- and v- vertical80 DO_2D( 0, 1, 0, 1 ) 79 DO jk = 2, jpkm1 ! Vertical momentum advection at level w and u- and v- vertical 80 DO_2D( 0, 1, 0, 1 ) ! vertical fluxes 81 81 zww(ji,jj) = 0.25_wp * e1e2t(ji,jj) * ww(ji,jj,jk) 82 82 END_2D 83 DO_2D( 0, 0, 0, 0 ) 83 DO_2D( 0, 0, 0, 0 ) ! vertical momentum advection at w-point 84 84 zwuw(ji,jj,jk) = ( zww(ji+1,jj ) + zww(ji,jj) ) * ( puu(ji,jj,jk-1,Kmm) - puu(ji,jj,jk,Kmm) ) 85 85 zwvw(ji,jj,jk) = ( zww(ji ,jj+1) + zww(ji,jj) ) * ( pvv(ji,jj,jk-1,Kmm) - pvv(ji,jj,jk,Kmm) ) … … 95 95 END_2D 96 96 ! 97 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) 97 DO_3D( 0, 0, 0, 0, 1, jpkm1 ) ! Vertical momentum advection at u- and v-points 98 98 puu(ji,jj,jk,Krhs) = puu(ji,jj,jk,Krhs) - ( zwuw(ji,jj,jk) + zwuw(ji,jj,jk+1) ) * r1_e1e2u(ji,jj) & 99 99 & / e3u(ji,jj,jk,Kmm) … … 102 102 END_3D 103 103 104 IF( l_trddyn ) THEN ! save the vertical advection trends for diagnostic104 IF( l_trddyn ) THEN ! save the vertical advection trends for diagnostic 105 105 ztrdu(:,:,:) = puu(:,:,:,Krhs) - ztrdu(:,:,:) 106 106 ztrdv(:,:,:) = pvv(:,:,:,Krhs) - ztrdv(:,:,:) … … 108 108 DEALLOCATE( ztrdu, ztrdv ) 109 109 ENDIF 110 ! ! Control print110 ! ! Control print 111 111 IF(sn_cfctl%l_prtctl) CALL prt_ctl( tab3d_1=puu(:,:,:,Krhs), clinfo1=' zad - Ua: ', mask1=umask, & 112 112 & tab3d_2=pvv(:,:,:,Krhs), clinfo2= ' Va: ', mask2=vmask, clinfo3='dyn' ) -
NEMO/trunk/src/OCE/DYN/dynzdf.F90
r13472 r13497 131 131 pvv(ji,jj,jk,Kaa) = ( pvv(ji,jj,jk,Kaa) - vv_b(ji,jj,Kaa) ) * vmask(ji,jj,jk) 132 132 END_3D 133 DO_2D( 0, 0, 0, 0 ) 133 DO_2D( 0, 0, 0, 0 ) ! Add bottom/top stress due to barotropic component only 134 134 iku = mbku(ji,jj) ! ocean bottom level at u- and v-points 135 135 ikv = mbkv(ji,jj) ! (deepest ocean u- and v-points) … … 190 190 END_3D 191 191 END SELECT 192 DO_2D( 0, 0, 0, 0 ) 192 DO_2D( 0, 0, 0, 0 ) !* Surface boundary conditions 193 193 zwi(ji,jj,1) = 0._wp 194 194 ze3ua = ( 1._wp - r_vvl ) * e3u(ji,jj,1,Kmm) & … … 227 227 END_3D 228 228 END SELECT 229 DO_2D( 0, 0, 0, 0 ) 229 DO_2D( 0, 0, 0, 0 ) !* Surface boundary conditions 230 230 zwi(ji,jj,1) = 0._wp 231 231 zwd(ji,jj,1) = 1._wp - zws(ji,jj,1) … … 366 366 END_3D 367 367 END SELECT 368 DO_2D( 0, 0, 0, 0 ) 368 DO_2D( 0, 0, 0, 0 ) !* Surface boundary conditions 369 369 zwi(ji,jj,1) = 0._wp 370 370 zwd(ji,jj,1) = 1._wp - zws(ji,jj,1) -
NEMO/trunk/src/OCE/DYN/sshwzv.F90
r13295 r13497 203 203 ELSE !== Quasi-Eulerian vertical coordinate ==! ('key_qco') 204 204 ! !==========================================! 205 DO jk = jpkm1, 1, -1 ! integrate from the bottom the hor. divergence205 DO jk = jpkm1, 1, -1 ! integrate from the bottom the hor. divergence 206 206 pww(:,:,jk) = pww(:,:,jk+1) - ( e3t(:,:,jk,Kmm) * hdiv(:,:,jk) & 207 207 & + r1_Dt * ( e3t(:,:,jk,Kaa) & … … 393 393 ! 394 394 IF( MAXVAL( Cu_adv(:,:,:) ) > Cu_min ) THEN ! Quick check if any breaches anywhere 395 DO_3DS( 1, 1, 1, 1, jpkm1, 2, -1 ) 395 DO_3DS( 1, 1, 1, 1, jpkm1, 2, -1 ) ! or scan Courant criterion and partition ! w where necessary 396 396 ! 397 397 zCu = MAX( Cu_adv(ji,jj,jk) , Cu_adv(ji,jj,jk-1) ) -
NEMO/trunk/src/OCE/DYN/wet_dry.F90
r13295 r13497 307 307 zwdlmtv(:,:) = 1._wp 308 308 ! 309 DO_2D( 0, 1, 0, 1 ) 309 DO_2D( 0, 1, 0, 1 ) ! Horizontal Flux in u and v direction 310 310 ! 311 311 IF( tmask(ji, jj, 1 ) < 0.5_wp) CYCLE ! we don't care about land cells
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