Changeset 12062 for NEMO/branches/2019/ENHANCE-02_ISF_nemo/src/OCE/TRA
- Timestamp:
- 2019-12-05T10:57:46+01:00 (4 years ago)
- File:
-
- 1 edited
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NEMO/branches/2019/ENHANCE-02_ISF_nemo/src/OCE/TRA/traisf.F90
r11987 r12062 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 isf_oce ! Ice shelf variable 15 USE phycst ! physical constant 16 USE eosbn2 ! Equation Of State 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 oce , ONLY : tsa ! ocean dynamics and active tracers 14 USE dom_oce , ONLY : e3t_n, r1_e1e2t ! ocean space domain variables 15 USE isfutils, ONLY : debug ! debug option 16 USE timing , ONLY : timing_start, timing_stop ! Timing 17 USE in_out_manager ! I/O manager 22 18 23 19 IMPLICIT NONE … … 63 59 IF ( ln_isfcpl ) THEN 64 60 ! 61 ! Dynamical stability at start up after change in under ice shelf cavity geometry is achieve by correcting the divergence. 62 ! This is achieved by applying a volume flux in order to keep the horizontal divergence after remapping 63 ! the same as at the end of the latest time step. So correction need to be apply at nit000 (euler time step) and 64 ! half of it at nit000+1 (leap frog time step). 65 ! in accordance to this, the heat content flux due to injected water need to be added in the temperature and salt trend 66 ! at time step nit000 and nit000+1 65 67 IF ( kt == nit000 ) CALL tra_isf_cpl(risfcpl_tsc , tsa) 66 68 IF ( kt == nit000+1) CALL tra_isf_cpl(risfcpl_tsc*0.5_wp, tsa)
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