Changeset 6997 for trunk/DOC/TexFiles/Chapters/Chap_ZDF.tex
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- 2016-10-05T16:26:13+02:00 (7 years ago)
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trunk/DOC/TexFiles/Chapters/Chap_ZDF.tex
r6497 r6997 1 \documentclass[NEMO_book]{subfiles} 2 \begin{document} 1 3 % ================================================================ 2 4 % Chapter Vertical Ocean Physics (ZDF) … … 234 236 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 235 237 \begin{figure}[!t] \begin{center} 236 \includegraphics[width=1.00\textwidth]{ ./TexFiles/Figures/Fig_mixing_length.pdf}238 \includegraphics[width=1.00\textwidth]{Fig_mixing_length} 237 239 \caption{ \label{Fig_mixing_length} 238 240 Illustration of the mixing length computation. } … … 408 410 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 409 411 \begin{figure}[!t] \begin{center} 410 \includegraphics[width=1.00\textwidth]{ ./TexFiles/Figures/Fig_ZDF_TKE_time_scheme.pdf}412 \includegraphics[width=1.00\textwidth]{Fig_ZDF_TKE_time_scheme} 411 413 \caption{ \label{Fig_TKE_time_scheme} 412 414 Illustration of the TKE time integration and its links to the momentum and tracer time integration. } … … 587 589 value near physical boundaries (logarithmic boundary layer law). $C_{\mu}$ and $C_{\mu'}$ 588 590 are calculated from stability function proposed by \citet{Galperin_al_JAS88}, or by \citet{Kantha_Clayson_1994} 589 or one of the two functions suggested by \citet{Canuto_2001} (\np{nn\_stab\_func} = 0, 1, 2 or 3, resp. }).591 or one of the two functions suggested by \citet{Canuto_2001} (\np{nn\_stab\_func} = 0, 1, 2 or 3, resp.). 590 592 The value of $C_{0\mu}$ depends of the choice of the stability function. 591 593 … … 643 645 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 644 646 \begin{figure}[!htb] \begin{center} 645 \includegraphics[width=0.90\textwidth]{ ./TexFiles/Figures/Fig_npc.pdf}647 \includegraphics[width=0.90\textwidth]{Fig_npc} 646 648 \caption{ \label{Fig_npc} 647 649 Example of an unstable density profile treated by the non penetrative … … 799 801 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 800 802 \begin{figure}[!t] \begin{center} 801 \includegraphics[width=0.99\textwidth]{ ./TexFiles/Figures/Fig_zdfddm.pdf}803 \includegraphics[width=0.99\textwidth]{Fig_zdfddm} 802 804 \caption{ \label{Fig_zdfddm} 803 805 From \citet{Merryfield1999} : (a) Diapycnal diffusivities $A_f^{vT}$ … … 1129 1131 baroclinic and barotropic components which is appropriate when using either the 1130 1132 explicit or filtered surface pressure gradient algorithms (\key{dynspg\_exp} or 1131 {\key{dynspg\_flt}). Extra attention is required, however, when using1133 \key{dynspg\_flt}). Extra attention is required, however, when using 1132 1134 split-explicit time stepping (\key{dynspg\_ts}). In this case the free surface 1133 1135 equation is solved with a small time step \np{rn\_rdt}/\np{nn\_baro}, while the three … … 1244 1246 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 1245 1247 \begin{figure}[!t] \begin{center} 1246 \includegraphics[width=0.90\textwidth]{ ./TexFiles/Figures/Fig_ZDF_M2_K1_tmx.pdf}1248 \includegraphics[width=0.90\textwidth]{Fig_ZDF_M2_K1_tmx} 1247 1249 \caption{ \label{Fig_ZDF_M2_K1_tmx} 1248 1250 (a) M2 and (b) K1 internal wave drag energy from \citet{Carrere_Lyard_GRL03} ($W/m^2$). } … … 1355 1357 1356 1358 1359 \end{document}
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