- Timestamp:
- 2012-11-27T15:42:24+01:00 (11 years ago)
- File:
-
- 1 edited
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branches/2012/dev_MERGE_2012/NEMOGCM/NEMO/TOP_SRC/TRP/trcsbc.F90
r3625 r3680 50 50 !! tra = tra + emp * trn / e3t for k=1 51 51 !! where emp, the surface freshwater budget (evaporation minus 52 !! precipitation minus runoff) given in kg/m2/s is divided52 !! precipitation ) given in kg/m2/s is divided 53 53 !! by 1035 kg/m3 (density of ocean water) to obtain m/s. 54 54 !! … … 79 79 ENDIF 80 80 81 ! Coupling online : river runoff is added to the horizontal divergence (hdivn) in the subroutine sbc_rnf_div 82 ! one only consider the concentration/dilution effect due to evaporation minus precipitation + freezing/melting of sea-ice 81 83 82 IF( lk_offline ) THEN ! sfx in dynamical files contains sfx - rnf 83 zsfx(:,:) = sfx(:,:) 84 ELSE ! Concentration dilution effect on tracer due to evaporation, precipitation, and river runoff 85 IF( lk_vvl ) THEN ! volume variable 86 zsfx(:,:) = sfx(:,:) - emp(:,:) 87 !!ch zsfx(:,:) = 0. 88 ELSE ! linear free surface 89 IF( ln_rnf ) THEN ; zsfx(:,:) = sfx(:,:) - rnf(:,:) ! E-P-R 90 ELSE ; zsfx(:,:) = sfx(:,:) 91 ENDIF 92 ENDIF 93 ENDIF 84 IF( .NOT. lk_offline .AND. lk_vvl ) THEN ! online coupling + volume variable 85 zemps(:,:) = sfx(:,:) - emp(:,:) 86 ELSE 87 zemps(:,:) = emp(:,:) 88 ENDIF 94 89 95 90 ! 0. initialization
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