- Timestamp:
- 2013-11-22T13:12:59+01:00 (10 years ago)
- File:
-
- 1 edited
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branches/2013/dev_MERGE_2013/NEMOGCM/NEMO/OPA_SRC/step.F90
r4312 r4313 112 112 ! Note that the computation of vertical velocity above, hence "after" sea level 113 113 ! is necessary to compute momentum advection for the rhs of barotropic loop: 114 CALL eos ( tsn, rhd, rhop ) ! now in situ density for hpg computation114 CALL eos ( tsn, rhd, rhop, fsdept_n(:,:,:) ) ! now in situ density for hpg computation 115 115 IF( ln_zps ) CALL zps_hde( kstp, jpts, tsn, gtsu, gtsv, & ! zps: now hor. derivative 116 116 & rhd, gru , grv ) ! of t, s, rd at the last ocean level
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