- Timestamp:
- 2016-03-18T14:56:37+01:00 (8 years ago)
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branches/2015/nemo_v3_6_STABLE/DOC/TexFiles/Chapters/Chap_SBC.tex
r6350 r6396 948 948 \namdisplay{namsbc_isf} 949 949 %-------------------------------------------------------------------------------------------------------- 950 Namelist variable in \ngn{namsbc}, \np{nn\_isf}, controls the ice shelf representation used. 950 Namelist variable in \ngn{namsbc}, \np{nn\_isf}, controls the ice shelf representation used (Fig. \ref{Fig_SBC_isf}): 951 952 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 953 \begin{figure}[!h] \begin{center} 954 \includegraphics[width=0.8\textwidth]{./TexFiles/Figures/Fig_SBC_isf.pdf} 955 \caption{ \label{Fig_SBC_isf} 956 Schematic for all the options available trough \np{nn\_isf}.} 957 \end{center} \end{figure} 958 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 959 951 960 \begin{description} 961 \item[\np{nn\_isf}~=~0] 962 The ice shelf routines are not used. The ice shelf melting is not computed or prescribed, the cavity have to be closed. 963 If needed, the ice shelf melting should be added to the runoff or the precipitation file. 964 952 965 \item[\np{nn\_isf}~=~1] 953 966 The ice shelf cavity is represented. The fwf and heat flux are computed. Two different bulk formula are available: … … 1002 1015 $\bullet$ \np{nn\_isf}~=~1 and \np{nn\_isf}~=~2 compute a melt rate based on the water mass properties, ocean velocities and depth. 1003 1016 This flux is thus highly dependent of the model resolution (horizontal and vertical), realism of the water masses onto the shelf ...\\ 1004 1005 1017 1006 1018 $\bullet$ \np{nn\_isf}~=~3 and \np{nn\_isf}~=~4 read the melt rate from a file. You have total control of the fwf forcing.
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