Changeset 10473 for branches/UKMO/AMM15_v3_6_STABLE_package_collate_coupling/NEMOGCM/NEMO/OPA_SRC/DYN/dynspg_ts.F90
- Timestamp:
- 2019-01-08T18:02:36+01:00 (5 years ago)
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branches/UKMO/AMM15_v3_6_STABLE_package_collate_coupling/NEMOGCM/NEMO/OPA_SRC/DYN/dynspg_ts.F90
r10268 r10473 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 ! ! -------------------------------------------------------- … … 462 470 & + fwfisf(:,:) + fwfisf_b(:,:) ) 463 471 ENDIF 472 ! 473 IF( ln_sdw ) THEN ! Stokes drift divergence added if necessary 474 zssh_frc(:,:) = zssh_frc(:,:) + div_sd(:,:) 475 ENDIF 476 ! 464 477 #if defined key_asminc 465 478 ! ! Include the IAU weighted SSH increment
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