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Changeset 3037 for branches – NEMO

Changeset 3037 for branches


Ignore:
Timestamp:
2011-11-03T12:28:28+01:00 (12 years ago)
Author:
cetlod
Message:

branch 2011/dev_LOCEAN_2011: update documentation

Location:
branches/2011/dev_LOCEAN_2011/DOC/TexFiles
Files:
1 added
2 deleted
3 edited

Legend:

Unmodified
Added
Removed
  • branches/2011/dev_LOCEAN_2011/DOC/TexFiles/Chapters/Chap_DOM.tex

    r2376 r3037  
    832832\gmcomment{   \colorbox{yellow}{Add one word on tricky trick !} mbathy in further modified in zdfbfr{\ldots}.  } 
    833833%%% 
     834 
     835% ================================================================ 
     836% Domain: Initial State (dtatsd & istate) 
     837% ================================================================ 
     838\section  [Domain: Initial State (\textit{istate & dtatsd})] 
     839      {Domain: Initial State \small{(\mdl{istate & dtatsd} modules)} } 
     840\label{DTA_tsd} 
     841%-----------------------------------------namtsd------------------------------------------- 
     842\namdisplay{namtsd}  
     843%------------------------------------------------------------------------------------------ 
     844 
     845By default, we assume that the velocity field is set to zero at the start.  
     846The initialisation of temperature and salinity fields is controlled by the namelist parameter (\np{ln\_tsd_init}) 
     847\begin{description} 
     848\item[ln{\_}tsd_init = .true.]  use of climatologies that can be given on the model grid itself or  
     849on their native input data grid. In the latter case, the data will be interpolated on-the-fly both in the  
     850horizontal and the vertical to the model grid (see \S~\ref{SBC_iof}).  
     851The computation is done in the \mdl{dtatsd} module. 
     852\item[ln{\_}tsd_init = .false.] use salinity constant value of 35.5 psu and an analytical profile of temperature,  
     853see subroutine \rou{istate\_t\_s} (called from \mdl{istate} module). 
  • branches/2011/dev_LOCEAN_2011/DOC/TexFiles/Chapters/Chap_TRA.tex

    r2541 r3037  
    10531053%--------------------------------------------namtra_dmp------------------------------------------------- 
    10541054\namdisplay{namtra_dmp} 
    1055 \namdisplay{namdta_tem} 
    1056 \namdisplay{namdta_sal} 
    10571055%-------------------------------------------------------------------------------------------------------------- 
    10581056 
     
    10671065where $\gamma$ is the inverse of a time scale, and $T_o$ and $S_o$  
    10681066are given temperature and salinity fields (usually a climatology).  
    1069 The restoring term is added when \key{tradmp} is defined.  
    1070 It also requires that both \key{dtatem} and \key{dtasal} are defined  
    1071 and fill in \textit{namdta\_tem} and \textit{namdta\_sal namelists}  
     1067The restoring term is added when the namelist parameter \np{ln\_tradmp} is set to true.  
     1068It also requires that both \np{ln\_tsd_init} and \np{ln\_tsd_tradmp} are set to true 
     1069and fill in \textit{namtsd} namelist}  
    10721070($i.e.$ that $T_o$ and $S_o$ are read using \mdl{fldread},  
    10731071see \S\ref{SBC_fldread}). The restoring coefficient $\gamma$ is  
  • branches/2011/dev_LOCEAN_2011/DOC/TexFiles/Namelist/namtra_dmp

    r2540 r3037  
    11!----------------------------------------------------------------------- 
    2 &namtra_dmp    !   tracer: T & S newtonian damping                      ('key_tradmp') 
     2&namtra_dmp    !   tracer: T & S newtonian damping 
    33!----------------------------------------------------------------------- 
     4   ln_tradmp   =  .true.   !  add a damping termn (T) or not (F) 
    45   nn_hdmp     =   -1      !  horizontal shape =-1, damping in Med and Red Seas only 
    56                           !                   =XX, damping poleward of XX degrees (XX>0) 
    67                           !                      + F(distance-to-coast) + Red and Med Seas 
    7    nn_zdmp     =    1      !  vertical   shape =0    damping throughout the water column 
     8   nn_zdmp     =    0      !  vertical   shape =0    damping throughout the water column 
    89                           !                   =1 no damping in the mixing layer (kz  criteria) 
    910                           !                   =2 no damping in the mixed  layer (rho crieria) 
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