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branches/2015/nemo_v3_6_STABLE/DOC/TexFiles/Chapters/Chap_ZDF.tex
r6322 r6992 1 %\documentclass[NEMO_book]{subfiles} 2 %\begin{document} 1 3 % ================================================================ 2 4 % Chapter Vertical Ocean Physics (ZDF) … … 233 235 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 234 236 \begin{figure}[!t] \begin{center} 235 \includegraphics[width=1.00\textwidth]{ ./TexFiles/Figures/Fig_mixing_length.pdf}237 \includegraphics[width=1.00\textwidth]{Fig_mixing_length} 236 238 \caption{ \label{Fig_mixing_length} 237 239 Illustration of the mixing length computation. } … … 407 409 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 408 410 \begin{figure}[!t] \begin{center} 409 \includegraphics[width=1.00\textwidth]{ ./TexFiles/Figures/Fig_ZDF_TKE_time_scheme.pdf}411 \includegraphics[width=1.00\textwidth]{Fig_ZDF_TKE_time_scheme} 410 412 \caption{ \label{Fig_TKE_time_scheme} 411 413 Illustration of the TKE time integration and its links to the momentum and tracer time integration. } … … 586 588 value near physical boundaries (logarithmic boundary layer law). $C_{\mu}$ and $C_{\mu'}$ 587 589 are calculated from stability function proposed by \citet{Galperin_al_JAS88}, or by \citet{Kantha_Clayson_1994} 588 or one of the two functions suggested by \citet{Canuto_2001} (\np{nn\_stab\_func} = 0, 1, 2 or 3, resp. }).590 or one of the two functions suggested by \citet{Canuto_2001} (\np{nn\_stab\_func} = 0, 1, 2 or 3, resp.). 589 591 The value of $C_{0\mu}$ depends of the choice of the stability function. 590 592 … … 658 660 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 659 661 \begin{figure}[!htb] \begin{center} 660 \includegraphics[width=0.90\textwidth]{ ./TexFiles/Figures/Fig_npc.pdf}662 \includegraphics[width=0.90\textwidth]{Fig_npc} 661 663 \caption{ \label{Fig_npc} 662 664 Example of an unstable density profile treated by the non penetrative … … 814 816 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 815 817 \begin{figure}[!t] \begin{center} 816 \includegraphics[width=0.99\textwidth]{ ./TexFiles/Figures/Fig_zdfddm.pdf}818 \includegraphics[width=0.99\textwidth]{Fig_zdfddm} 817 819 \caption{ \label{Fig_zdfddm} 818 820 From \citet{Merryfield1999} : (a) Diapycnal diffusivities $A_f^{vT}$ … … 1143 1145 baroclinic and barotropic components which is appropriate when using either the 1144 1146 explicit or filtered surface pressure gradient algorithms (\key{dynspg\_exp} or 1145 {\key{dynspg\_flt}). Extra attention is required, however, when using1147 \key{dynspg\_flt}). Extra attention is required, however, when using 1146 1148 split-explicit time stepping (\key{dynspg\_ts}). In this case the free surface 1147 1149 equation is solved with a small time step \np{rn\_rdt}/\np{nn\_baro}, while the three … … 1258 1260 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 1259 1261 \begin{figure}[!t] \begin{center} 1260 \includegraphics[width=0.90\textwidth]{ ./TexFiles/Figures/Fig_ZDF_M2_K1_tmx.pdf}1262 \includegraphics[width=0.90\textwidth]{Fig_ZDF_M2_K1_tmx} 1261 1263 \caption{ \label{Fig_ZDF_M2_K1_tmx} 1262 1264 (a) M2 and (b) K1 internal wave drag energy from \citet{Carrere_Lyard_GRL03} ($W/m^2$). } … … 1369 1371 1370 1372 1373 %\end{document}
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