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Changeset 13950 for NEMO/branches – NEMO

Changeset 13950 for NEMO/branches


Ignore:
Timestamp:
2020-12-01T18:33:58+01:00 (3 years ago)
Author:
smueller
Message:

Update of the documentation subsection on the freshwater-budget adjustment mechanism (ticket #2377)

File:
1 edited

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  • NEMO/branches/2020/ticket2377/doc/latex/NEMO/subfiles/chap_SBC.tex

    r12377 r13950  
    1818    Release & Author(s) & Modifications \\ 
    1919    \hline 
     20    {\em  next} & {\em S. M\" uller} & {\em Revision of \autoref{subsec:SBC_fwb}}\\ 
    2021    {\em   4.0} & {\em ...} & {\em ...} \\ 
    2122    {\em   3.6} & {\em ...} & {\em ...} \\ 
     
    17951796\label{subsec:SBC_fwb} 
    17961797 
    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 
     1804For global ocean simulations, it can be useful to introduce a control of the 
     1805mean sea level in order to prevent unrealistic drifting of the sea surface 
     1806height due to unbalanced freshwater fluxes. In \NEMO, two options for 
     1807controlling the freshwater budget are proposed. 
    18001808 
    18011809\begin{description} 
    1802 \item [{\np[=0]{nn_fwb}{nn\_fwb}}] no control at all. 
    1803   The mean sea level is free 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. 
    18051813  %GS: comment below still relevant ? 
    18061814  %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}. 
    18111822\end{description} 
    18121823 
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