- Timestamp:
- 2020-11-26T17:47:20+01:00 (4 years ago)
- Location:
- NEMO/branches/2020/dev_r12985_TOP-04_IMMERSE_BGC_interface
- Files:
-
- 4 edited
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NEMO/branches/2020/dev_r12985_TOP-04_IMMERSE_BGC_interface
- Property svn:externals
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old new 3 3 ^/utils/build/mk@HEAD mk 4 4 ^/utils/tools@HEAD tools 5 ^/vendors/AGRIF/dev @HEADext/AGRIF5 ^/vendors/AGRIF/dev_r12970_AGRIF_CMEMS ext/AGRIF 6 6 ^/vendors/FCM@HEAD ext/FCM 7 7 ^/vendors/IOIPSL@HEAD ext/IOIPSL 8 8 9 9 # SETTE 10 ^/utils/CI/sette@1 2931sette10 ^/utils/CI/sette@13559 sette
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- Property svn:externals
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NEMO/branches/2020/dev_r12985_TOP-04_IMMERSE_BGC_interface/doc/latex/NEMO/subfiles/chap_SBC.tex
r12377 r13892 832 832 Solid precipitation & snow & $Kg.m^{-2}.s^{-1}$ & T \\ 833 833 \hline 834 Mean sea-level pressure & slp & $ hPa$ & T \\834 Mean sea-level pressure & slp & $Pa$ & T \\ 835 835 \hline 836 836 \end{tabular} -
NEMO/branches/2020/dev_r12985_TOP-04_IMMERSE_BGC_interface/doc/latex/NEMO/subfiles/chap_TRA.tex
r11693 r13892 1229 1229 In the computer code, a density anomaly, $d_a = \rho / \rho_o - 1$, is computed, 1230 1230 with $\rho_o$ a reference density. 1231 Called \textit{r au0} in the code,1231 Called \textit{rho0} in the code, 1232 1232 $\rho_o$ is set in \mdl{phycst} to a value of \texttt{1,026} $Kg/m^3$. 1233 1233 This is a sensible choice for the reference density used in a Boussinesq ocean climate model, -
NEMO/branches/2020/dev_r12985_TOP-04_IMMERSE_BGC_interface/doc/latex/NEMO/subfiles/chap_ZDF.tex
r11693 r13892 1160 1160 \] 1161 1161 When \np[=.true.]{ln_lin}{ln\_lin}, the value of $r$ used is \np{rn_Uc0}{rn\_Uc0}*\np{rn_Cd0}{rn\_Cd0}. 1162 Setting \np[=.true.]{ln_ OFF}{ln\_OFF} (and \forcode{ln_lin=.true.}) is equivalent to setting $r=0$ and leads to a free-slip boundary condition.1162 Setting \np[=.true.]{ln_drg_OFF}{ln\_OFF} (and \forcode{ln_lin=.true.}) is equivalent to setting $r=0$ and leads to a free-slip boundary condition. 1163 1163 1164 1164 These values are assigned in \mdl{zdfdrg}.
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