Changeset 10406 for NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
- Timestamp:
- 2018-12-18T11:25:09+01:00 (5 years ago)
- Location:
- NEMO/trunk/doc/latex
- Files:
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- 4 edited
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NEMO/trunk/doc/latex
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NEMO/trunk/doc/latex/NEMO
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NEMO/trunk/doc/latex/NEMO/subfiles
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NEMO/trunk/doc/latex/NEMO/subfiles/chap_SBC.tex
r10405 r10406 19 19 \begin{itemize} 20 20 \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 $\left( {\tau_u \;,\;\tau_v} \right)$ 22 22 \item 23 23 the incoming solar and non solar heat fluxes $\left( {Q_{ns} \;,\;Q_{sr} } \right)$ … … 391 391 The symbolic algorithm used to calculate values on the model grid is now: 392 392 393 \ begin{equation*}\begin{split}393 \[ \begin{split} 394 394 f_{m}(i,j) = f_{m}(i,j) +& \sum_{k=1}^{4} {wgt(k)f(idx(src(k)))} 395 395 + \sum_{k=5}^{8} {wgt(k)\left.\frac{\partial f}{\partial i}\right| _{idx(src(k))} } \\ … … 397 397 + \sum_{k=13}^{16} {wgt(k)\left.\frac{\partial ^2 f}{\partial i \partial j}\right| _{idx(src(k))} } 398 398 \end{split} 399 \ end{equation*}399 \] 400 400 The gradients here are taken with respect to the horizontal indices and not distances since 401 401 the spatial dependency has been absorbed into the weights.
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