- Timestamp:
- 2019-12-05T18:41:39+01:00 (4 years ago)
- File:
-
- 1 edited
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NEMO/branches/2019/UKMO_MERGE_2019/src/OCE/TRA/traisf.F90
r12068 r12077 10 10 !! tra_isf : update the tracer trend at ocean surface 11 11 !!---------------------------------------------------------------------- 12 USE oce ! ocean dynamics and active tracers 13 USE dom_oce ! ocean space domain variables 14 USE phycst ! physical constant 15 USE eosbn2 ! Equation Of State 16 USE isf ! Ice shelf variable 17 USE isfutils ! 18 ! 19 USE in_out_manager ! I/O manager 20 USE iom ! xIOS server 21 USE timing ! Timing 12 USE isf_oce ! Ice shelf variables 13 USE dom_oce , ONLY : e3t, r1_e1e2t ! ocean space domain variables 14 USE isfutils, ONLY : debug ! debug option 15 USE timing , ONLY : timing_start, timing_stop ! Timing 16 USE in_out_manager ! I/O manager 22 17 23 18 IMPLICIT NONE … … 65 60 IF ( ln_isfcpl ) THEN 66 61 ! 62 ! Dynamical stability at start up after change in under ice shelf cavity geometry is achieve by correcting the divergence. 63 ! This is achieved by applying a volume flux in order to keep the horizontal divergence after remapping 64 ! the same as at the end of the latest time step. So correction need to be apply at nit000 (euler time step) and 65 ! half of it at nit000+1 (leap frog time step). 66 ! in accordance to this, the heat content flux due to injected water need to be added in the temperature and salt trend 67 ! at time step nit000 and nit000+1 67 68 IF ( kt == nit000 ) CALL tra_isf_cpl(Kmm, risfcpl_tsc , pts(:,:,:,:,Krhs)) 68 69 IF ( kt == nit000+1) CALL tra_isf_cpl(Kmm, risfcpl_tsc*0.5_wp, pts(:,:,:,:,Krhs))
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