Changeset 13950
- Timestamp:
- 2020-12-01T18:33:58+01:00 (4 years ago)
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NEMO/branches/2020/ticket2377/doc/latex/NEMO/subfiles/chap_SBC.tex
r12377 r13950 18 18 Release & Author(s) & Modifications \\ 19 19 \hline 20 {\em next} & {\em S. M\" uller} & {\em Revision of \autoref{subsec:SBC_fwb}}\\ 20 21 {\em 4.0} & {\em ...} & {\em ...} \\ 21 22 {\em 3.6} & {\em ...} & {\em ...} \\ … … 1795 1796 \label{subsec:SBC_fwb} 1796 1797 1797 For global ocean simulation, it can be useful to introduce a control of the mean sea level in order to 1798 prevent unrealistic drift of the sea surface height due to inaccuracy in the freshwater fluxes. 1799 In \NEMO, two way of controlling the freshwater budget are proposed: 1798 \begin{listing} 1799 \nlst{namsbc_fwb} 1800 \caption{\forcode{&namsbc_fwb}} 1801 \label{lst:namsbc_fwb} 1802 \end{listing} 1803 1804 For global ocean simulations, it can be useful to introduce a control of the 1805 mean sea level in order to prevent unrealistic drifting of the sea surface 1806 height due to unbalanced freshwater fluxes. In \NEMO, two options for 1807 controlling the freshwater budget are proposed. 1800 1808 1801 1809 \begin{description} 1802 \item [{\np[=0]{nn_fwb}{nn\_fwb}} ] no control at all.1803 The mean sea level isfree to drift, and will certainly do so.1804 \item [{\np[=1]{nn_fwb}{nn\_fwb}} ] global mean \textit{emp}set to zero at each model time step.1810 \item [{\np[=0]{nn_fwb}{nn\_fwb}}:] No control at all; the mean sea level is 1811 free to drift, and will certainly do so. 1812 \item [{\np[=1]{nn_fwb}{nn\_fwb}}:] The global mean \textit{emp} is set to zero at each model time step. 1805 1813 %GS: comment below still relevant ? 1806 1814 %Note that with a sea-ice model, this technique only controls the mean sea level with linear free surface and no mass flux between ocean and ice (as it is implemented in the current ice-ocean coupling). 1807 \item [{\np[=2]{nn_fwb}{nn\_fwb}}] freshwater budget is adjusted from the previous year annual mean budget which 1808 is read in the \textit{EMPave\_old.dat} file. 1809 As the model uses the Boussinesq approximation, the annual mean fresh water budget is simply evaluated from 1810 the change in the mean sea level at January the first and saved in the \textit{EMPav.dat} file. 1815 \item [{\np[=2]{nn_fwb}{nn\_fwb}}:] \textit{emp} is adjusted by adding a 1816 spatially uniform, annual-mean freshwater flux that balances the freshwater 1817 budget at the end of the previous year; as the model uses the Boussinesq 1818 approximation, the freshwater budget can be evaluated from the change in the 1819 mean sea level and in the ice and snow mass after the end of each simulation 1820 year; at the start of the model run, an initial adjustment flux can be set 1821 using parameter \np{rn_rwb0}{rn\_fwb0} in namelist \nam{sbc_fwb}{sbc\_fwb}. 1811 1822 \end{description} 1812 1823
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