Ignore:
Timestamp:
2019-07-17T15:08:21+02:00 (15 months ago)
Author:
mdrudi
Message:

revision of CMIP specific diagnostics in chap_DIA.tex in NEMO doc

File:
1 edited

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  • NEMO/trunk/doc/latex/NEMO/subfiles/chap_DIA.tex

    r11218 r11276  
    1515%       Old Model Output  
    1616% ================================================================ 
    17 \section{Old model output (default)} 
     17\section{Model output} 
    1818\label{sec:DIA_io_old} 
    1919 
     
    14941494\textbf{Note that} in the current version (v3.6), many changes has been introduced but not fully tested. 
    14951495In particular, options associated with \np{ln\_dyn\_mxl}, \np{ln\_vor\_trd}, and \np{ln\_tra\_mxl} are not working, 
    1496 and none of the options have been tested with variable volume (\ie \key{vvl} defined). 
     1496and none of the options have been tested with variable volume (\ie \np{ln\_linssh}\forcode{ = .true.}). 
    14971497 
    14981498% ------------------------------------------------------------------------------------------------------------- 
     
    19301930   
    19311931Third, the discretisation of \autoref{eq:steric_Bq} depends on the type of free surface which is considered. 
    1932 In the non linear free surface case, \ie \key{vvl} defined, it is given by 
     1932In the non linear free surface case, \ie \np{ln\_linssh}\forcode{ = .true.}, it is given by 
    19331933 
    19341934\[ 
     
    19691969where $S_o$ and $p_o$ are the initial salinity and pressure, respectively. 
    19701970 
    1971 Both steric and thermosteric sea level are computed in \mdl{diaar5} which needs the \key{diaar5} defined to 
    1972 be called. 
     1971Both steric and thermosteric sea level are computed in \mdl{diaar5}. 
    19731972 
    19741973% ------------------------------------------------------------------------------------------------------------- 
    19751974%       Other Diagnostics 
    19761975% ------------------------------------------------------------------------------------------------------------- 
    1977 \section[Other diagnostics (\texttt{\textbf{key\_diahth}}, \texttt{\textbf{key\_diaar5}})] 
    1978 {Other diagnostics (\protect\key{diahth}, \protect\key{diaar5})} 
     1976\section[Other diagnostics] 
     1977{Other diagnostics} 
    19791978\label{sec:DIA_diag_others} 
    19801979 
     
    19951994- the depth of the thermocline (maximum of the vertical temperature gradient) (\mdl{diahth}) 
    19961995 
    1997 % ----------------------------------------------------------- 
    1998 %     Poleward heat and salt transports 
    1999 % ----------------------------------------------------------- 
    2000  
    2001 \subsection[Poleward heat and salt transports (\textit{diaptr.F90})] 
    2002 {Poleward heat and salt transports (\protect\mdl{diaptr})} 
    2003  
    2004 %------------------------------------------namptr----------------------------------------- 
    2005  
    2006 \nlst{namptr}  
    2007 %----------------------------------------------------------------------------------------- 
    2008  
    2009 The poleward heat and salt transports, their advective and diffusive component, 
    2010 and the meriodional stream function can be computed on-line in \mdl{diaptr} \np{ln\_diaptr} to true 
    2011 (see the \textit{\ngn{namptr} } namelist below). 
    2012 When \np{ln\_subbas}\forcode{ = .true.}, transports and stream function are computed for the Atlantic, Indian, 
    2013 Pacific and Indo-Pacific Oceans (defined north of 30\deg{S}) as well as for the World Ocean. 
    2014 The sub-basin decomposition requires an input file (\ifile{subbasins}) which contains three 2D mask arrays, 
    2015 the Indo-Pacific mask been deduced from the sum of the Indian and Pacific mask (\autoref{fig:mask_subasins}). 
    20161996 
    20171997%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
     
    20342014%       CMIP specific diagnostics  
    20352015% ----------------------------------------------------------- 
    2036 \subsection[CMIP specific diagnostics (\textit{diaar5.F90})] 
     2016\subsection[CMIP specific diagnostics (\textit{diaar5.F90}, \textit{diaptr.F90})] 
    20372017{CMIP specific diagnostics (\protect\mdl{diaar5})} 
    20382018 
    2039 A series of diagnostics has been added in the \mdl{diaar5}. 
    2040 They corresponds to outputs that are required for AR5 simulations (CMIP5) 
     2019A series of diagnostics has been added in the \mdl{diaar5} and \mdl{diaptr}. 
     2020In \mdl{diaar5} they correspond to outputs that are required for AR5 simulations (CMIP5) 
    20412021(see also \autoref{sec:DIA_steric} for one of them). 
    2042 Activating those outputs requires to define the \key{diaar5} CPP key. 
     2022The module \mdl{diaar5} is active when one of the following outputs is required : global total volume (voltot), global mean ssh (sshtot), global total mass (masstot), global mean temperature (temptot), global mean ssh steric (sshsteric), global mean ssh thermosteric (sshthster), global mean salinity (saltot), sea water pressure at sea floor (botpres), dynamic sea surface height (sshdyn). 
     2023 
     2024In \mdl{diaptr} when \np{ln\_diaptr}\forcode{ = .true.}  
     2025(see the \textit{\ngn{namptr} } namelist below) can be computed on-line the poleward heat and salt transports, their advective and diffusive component, and the meriodional stream function . 
     2026When \np{ln\_subbas}\forcode{ = .true.}, transports and stream function are computed for the Atlantic, Indian, 
     2027Pacific and Indo-Pacific Oceans (defined north of 30\deg{S}) as well as for the World Ocean. 
     2028The sub-basin decomposition requires an input file (\ifile{subbasins}) which contains three 2D mask arrays, 
     2029the Indo-Pacific mask been deduced from the sum of the Indian and Pacific mask (\autoref{fig:mask_subasins}). 
     2030 
     2031%------------------------------------------namptr----------------------------------------- 
     2032 
     2033\nlst{namptr}  
     2034%----------------------------------------------------------------------------------------- 
    20432035 
    20442036% ----------------------------------------------------------- 
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