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chap_DIU.tex

Timestamp:

2018-12-18T11:25:09+01:00 (5 years ago)

Author:

nicolasmartin

Message:

Edition of math environments

Use LaTeX shortanted syntax for unnumbered equations (\[ ... \])
Replace deprecated eqnarray with align environment (reference http://en.wikibooks.org/w/index.php?title=LaTeX/Advanced_Mathematics&#Other_environments)
Remove some space before indices

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NEMO/trunk/doc/latex

Files:

Property svn:ignore

Property svn:ignore

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-                      r10354
+                      r10406
 The warm layer is calculated using the model of \citet{Takaya_al_JGR10} (TAKAYA10 model hereafter).
 This is a simple flux based model that is defined by the equations
 \begin{eqnarray}
+\begin{align}
 \frac{\partial{\Delta T_{\rm{wl}}}}{\partial{t}}&=&\frac{Q(\nu+1)}{D_T\rho_w c_p
 \nu}-\frac{(\nu+1)ku^*_{w}f(L_a)\Delta T}{D_T\Phi\!\left(\frac{D_T}{L}\right)} \mbox{,}
 \label{eq:ecmwf1} \\
 L&=&\frac{\rho_w c_p u^{*^3}_{w}}{\kappa g \alpha_w Q }\mbox{,}\label{eq:ecmwf2}
 \end{eqnarray}
+\end{align}
 where $\Delta T_{\rm{wl}}$ is the temperature difference between the top of the warm layer and the depth $D_T=3$\,m at which there is assumed to be no diurnal signal.
 In equation (\autoref{eq:ecmwf1}) $\alpha_w=2\times10^{-4}$ is the thermal expansion coefficient of water,

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