Changeset 6997 for trunk/DOC/TexFiles/Chapters/Chap_LDF.tex
- Timestamp:
- 2016-10-05T16:26:13+02:00 (8 years ago)
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trunk/DOC/TexFiles/Chapters/Chap_LDF.tex
r6289 r6997 1 \documentclass[NEMO_book]{subfiles} 2 \begin{document} 1 3 2 4 % ================================================================ … … 228 230 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 229 231 \begin{figure}[!ht] \begin{center} 230 \includegraphics[width=0.70\textwidth]{ ./TexFiles/Figures/Fig_LDF_ZDF1.pdf}232 \includegraphics[width=0.70\textwidth]{Fig_LDF_ZDF1} 231 233 \caption { \label{Fig_LDF_ZDF1} 232 234 averaging procedure for isopycnal slope computation.} … … 256 258 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 257 259 \begin{figure}[!ht] \begin{center} 258 \includegraphics[width=0.70\textwidth]{ ./TexFiles/Figures/Fig_eiv_slp.pdf}260 \includegraphics[width=0.70\textwidth]{Fig_eiv_slp} 259 261 \caption { \label{Fig_eiv_slp} 260 262 Vertical profile of the slope used for lateral mixing in the mixed layer : … … 298 300 diffusion along model level surfaces, i.e. using the shear computed along 299 301 the model levels and with no additional friction at the ocean bottom (see 300 {\S\ref{LBC_coast}).302 \S\ref{LBC_coast}). 301 303 302 304 … … 425 427 values are $0$). However, the technique used to compute the isopycnal 426 428 slopes is intended to get rid of such a background diffusion, since it introduces 427 spurious diapycnal diffusion (see {\S\ref{LDF_slp}).429 spurious diapycnal diffusion (see \S\ref{LDF_slp}). 428 430 429 431 (4) when an eddy induced advection term is used (\key{traldf\_eiv}), $A^{eiv}$, … … 499 501 500 502 501 503 \end{document}
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