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Changeset 10406 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex – NEMO

Ignore:
Timestamp:
2018-12-18T11:25:09+01:00 (5 years ago)
Author:
nicolasmartin
Message:

Edition of math environments

Location:
NEMO/trunk/doc/latex
Files:
4 edited

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  • NEMO/trunk/doc/latex

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

    r10405 r10406  
    1919\begin{itemize} 
    2020\item 
    21   the two components of the surface ocean stress $\left( {\tau _u \;,\;\tau _v} \right)$ 
     21  the two components of the surface ocean stress $\left( {\tau_u \;,\;\tau_v} \right)$ 
    2222\item 
    2323  the incoming solar and non solar heat fluxes $\left( {Q_{ns} \;,\;Q_{sr} } \right)$ 
     
    391391The symbolic algorithm used to calculate values on the model grid is now: 
    392392 
    393 \begin{equation*} \begin{split} 
     393\[ \begin{split} 
    394394f_{m}(i,j) =  f_{m}(i,j) +& \sum_{k=1}^{4} {wgt(k)f(idx(src(k)))}      
    395395              +   \sum_{k=5}^{8} {wgt(k)\left.\frac{\partial f}{\partial i}\right| _{idx(src(k))} }    \\ 
     
    397397              +   \sum_{k=13}^{16} {wgt(k)\left.\frac{\partial ^2 f}{\partial i \partial j}\right| _{idx(src(k))} } 
    398398\end{split} 
    399 \end{equation*} 
     399\] 
    400400The gradients here are taken with respect to the horizontal indices and not distances since 
    401401the spatial dependency has been absorbed into the weights. 
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