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Changeset 11599 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex – NEMO

Ignore:
Timestamp:
2019-09-25T22:19:45+02:00 (5 years ago)
Author:
nicolasmartin
Message:

Cosmetic cleaning

File:
1 edited

Legend:

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

    r11598 r11599  
    135135 
    136136%\colorbox{yellow}{Miss: } 
    137 % 
    138137%A extensive description of all namsbc namelist (parameter that have to be 
    139138%created!) 
    140 % 
    141139%Especially the \np{nn_fsbc}{nn\_fsbc}, the \mdl{sbc\_oce} module (fluxes + mean sst sss ssu 
    142140%ssv) \ie\ information required by flux computation or sea-ice 
    143 % 
    144141%\mdl{sbc\_oce} containt the definition in memory of the 7 fields (6+runoff), add 
    145142%a word on runoff: included in surface bc or add as lateral obc{\ldots}. 
    146 % 
    147143%Sbcmod manage the ``providing'' (fourniture) to the ocean the 7 fields 
    148 % 
    149144%Fluxes update only each nf\_sbc time step (namsbc) explain relation 
    150145%between nf\_sbc and nf\_ice, do we define nf\_blk??? ? only one 
    151146%nf\_sbc 
    152 % 
    153147%Explain here all the namlist namsbc variable{\ldots}. 
    154 % 
    155148% explain : use or not of surface currents 
    156 % 
    157149%\colorbox{yellow}{End Miss } 
    158150 
     
    889881 
    890882%\gmcomment{  word doc of runoffs: 
    891 % 
    892883%In the current \NEMO\ setup river runoff is added to emp fluxes, these are then applied at just the sea surface as a volume change (in the variable volume case this is a literal volume change, and in the linear free surface case the free surface is moved) and a salt flux due to the concentration/dilution effect.  There is also an option to increase vertical mixing near river mouths; this gives the effect of having a 3d river.  All river runoff and emp fluxes are assumed to be fresh water (zero salinity) and at the same temperature as the sea surface. 
    893884%Our aim was to code the option to specify the temperature and salinity of river runoff, (as well as the amount), along with the depth that the river water will affect.  This would make it possible to model low salinity outflow, such as the Baltic, and would allow the ocean temperature to be affected by river runoff. 
     
    13131304\subsection[Diurnal cycle (\textit{sbcdcy.F90})]{Diurnal cycle (\protect\mdl{sbcdcy})} 
    13141305\label{subsec:SBC_dcy} 
    1315 % 
    13161306 
    13171307\begin{figure}[!t] 
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