Changeset 11277 for branches/UKMO/AMM15_v3_6_STABLE_package_collate/NEMOGCM/NEMO/OPA_SRC/DYN/dynspg_ts.F90
- Timestamp:
- 2019-07-17T15:29:15+02:00 (5 years ago)
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branches/UKMO/AMM15_v3_6_STABLE_package_collate/NEMOGCM/NEMO/OPA_SRC/DYN/dynspg_ts.F90
r10268 r11277 11 11 !! 3.5 ! 2013-07 (J. Chanut) Switch to Forward-backward time stepping 12 12 !! 3.6 ! 2013-11 (A. Coward) Update for z-tilde compatibility 13 !! - ! 2016-12 (G. Madec, E. Clementi) update for Stoke-Drift divergence 13 14 !!--------------------------------------------------------------------- 14 15 #if defined key_dynspg_ts || defined key_esopa … … 31 32 USE sbctide ! tides 32 33 USE updtide ! tide potential 34 USE sbcwave ! surface wave 35 ! 33 36 USE lib_mpp ! distributed memory computing library 34 37 USE lbclnk ! ocean lateral boundary conditions (or mpp link) … … 333 336 END DO 334 337 END DO 338 339 !!gm Question here when removing the Vertically integrated trends, we remove the vertically integrated NL trends on momentum.... 340 !!gm Is it correct to do so ? I think so... 341 342 335 343 ! !* barotropic Coriolis trends (vorticity scheme dependent) 336 344 ! ! -------------------------------------------------------- … … 475 483 ! 476 484 ! ----------------------------------------------------------------------- 477 ! Phase 2 : Integration of the barotropic equations 485 ! Phase 2 : Integration of the barotropic equations 478 486 ! ----------------------------------------------------------------------- 479 487 ! 480 488 ! ! ==================== ! 481 489 ! ! Initialisations ! 482 ! ! ==================== ! 490 ! ! ==================== ! 483 491 ! Initialize barotropic variables: 484 492 IF( ll_init )THEN … … 489 497 ub_e (:,:) = 0._wp 490 498 vb_e (:,:) = 0._wp 499 ENDIF 500 ! 501 ! Moved here to allow merging with other branch 502 IF( ln_sdw ) THEN ! Stokes drift divergence added if necessary 503 zssh_frc(:,:) = zssh_frc(:,:) + div_sd(:,:) 491 504 ENDIF 492 505 !
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