Changeset 14130 for NEMO/trunk/doc/latex/NEMO
- Timestamp:
- 2020-12-08T11:48:58+01:00 (2 years ago)
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- 1 edited
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
r14116 r14130 16 16 Release & Author(s) & Modifications \\ 17 17 \hline 18 {\em next} & {\em Simon M{\" u}ller} & {\em Update of \autoref{sec:SBC_TDE} }\\[2mm]18 {\em next} & {\em Simon M{\" u}ller} & {\em Update of \autoref{sec:SBC_TDE}; revision of \autoref{subsec:SBC_fwb}}\\[2mm] 19 19 {\em 4.0} & {\em ...} & {\em ...} \\ 20 20 {\em 3.6} & {\em ...} & {\em ...} \\ … … 1777 1777 \label{subsec:SBC_fwb} 1778 1778 1779 For global ocean simulation, it can be useful to introduce a control of the mean sea level in order to 1780 prevent unrealistic drift of the sea surface height due to inaccuracy in the freshwater fluxes. 1781 In \NEMO, two way of controlling the freshwater budget are proposed: 1779 \begin{listing} 1780 \nlst{namsbc_fwb} 1781 \caption{\forcode{&namsbc_fwb}} 1782 \label{lst:namsbc_fwb} 1783 \end{listing} 1784 1785 For global ocean simulations, it can be useful to introduce a control of the 1786 mean sea level in order to prevent unrealistic drifting of the sea surface 1787 height due to unbalanced freshwater fluxes. In \NEMO, two options for 1788 controlling the freshwater budget are proposed. 1782 1789 1783 1790 \begin{description} 1784 \item [{\np[=0]{nn_fwb}{nn\_fwb}} ] no control at all.1785 The mean sea level isfree to drift, and will certainly do so.1786 \item [{\np[=1]{nn_fwb}{nn\_fwb}} ] global mean \textit{emp}set to zero at each model time step.1791 \item [{\np[=0]{nn_fwb}{nn\_fwb}}:] No control at all; the mean sea level is 1792 free to drift, and will certainly do so. 1793 \item [{\np[=1]{nn_fwb}{nn\_fwb}}:] The global mean \textit{emp} is set to zero at each model time step. 1787 1794 %GS: comment below still relevant ? 1788 1795 %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). 1789 \item [{\np[=2]{nn_fwb}{nn\_fwb}}] freshwater budget is adjusted from the previous year annual mean budget which 1790 is read in the \textit{EMPave\_old.dat} file. 1791 As the model uses the Boussinesq approximation, the annual mean fresh water budget is simply evaluated from 1792 the change in the mean sea level at January the first and saved in the \textit{EMPav.dat} file. 1796 \item [{\np[=2]{nn_fwb}{nn\_fwb}}:] \textit{emp} is adjusted by adding a 1797 spatially uniform, annual-mean freshwater flux that balances the freshwater 1798 budget at the end of the previous year; as the model uses the Boussinesq 1799 approximation, the freshwater budget can be evaluated from the change in the 1800 mean sea level and in the ice and snow mass after the end of each simulation 1801 year; at the start of the model run, an initial adjustment flux can be set 1802 using parameter \np{rn_rwb0}{rn\_fwb0} in namelist \nam{sbc_fwb}{sbc\_fwb}. 1793 1803 \end{description} 1794 1804
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