- Timestamp:
- 2020-04-20T18:53:13+02:00 (4 years ago)
- File:
-
- 1 edited
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NEMO/branches/2020/dev_r12377_KERNEL-06_techene_e3/src/TOP/TRP/trcsbc.F90
r12724 r12779 30 30 !! * Substitutions 31 31 # include "do_loop_substitute.h90" 32 # include "domzgr_substitute.h90" 32 33 !!---------------------------------------------------------------------- 33 34 !! NEMO/TOP 4.0 , NEMO Consortium (2018) … … 49 50 !! The surface freshwater flux modify the ocean volume 50 51 !! and thus the concentration of a tracer as : 51 !! tr(Krhs) = tr(Krhs) + emp * tr(Kmm) / e3t for k=152 !! tr(Krhs) = tr(Krhs) + emp * tr(Kmm) / e3t_ for k=1 52 53 !! where emp, the surface freshwater budget (evaporation minus 53 54 !! precipitation ) given in kg/m2/s is divided
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