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Changeset 6992 for branches/2015/nemo_v3_6_STABLE/DOC/TexFiles/Chapters/Chap_ZDF.tex – NEMO

Ignore:
Timestamp:
2016-10-05T14:07:19+02:00 (8 years ago)
Author:
nicolasmartin
Message:

Global reorganisation of DOC directory to ensure the export of NEMO Reference Manual both in PDF & HTML

  • Move 'Figures' and 'Namelists' from ./TexFiles? to the root, create 'Styles' directory in ./TexFiles? with corresponding files and generate EPS version of all figures
  • Fix LaTex? typos, add the possibility to compile each chapter separately with 'subfiles' package and clean the main LaTeX file by creating 'Preamble.tex' & 'Top_Matter.tex' in ./TexFiles?
  • Provide LaTeX2HTML.sh script for producing HTML output (LaTeX2HTML tool needed with patch)
  • Remove PDF files from versionned files
File:
1 edited

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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} 
    13% ================================================================ 
    24% Chapter  Vertical Ocean Physics (ZDF) 
     
    233235%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    234236\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} 
    236238\caption{ \label{Fig_mixing_length}  
    237239Illustration of the mixing length computation. } 
     
    407409%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    408410\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} 
    410412\caption{ \label{Fig_TKE_time_scheme}  
    411413Illustration of the TKE time integration and its links to the momentum and tracer time integration. } 
     
    586588value near physical boundaries (logarithmic boundary layer law). $C_{\mu}$ and $C_{\mu'}$  
    587589are 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.}).  
     590or one of the two functions suggested by \citet{Canuto_2001}  (\np{nn\_stab\_func} = 0, 1, 2 or 3, resp.).  
    589591The value of $C_{0\mu}$ depends of the choice of the stability function. 
    590592 
     
    658660%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    659661\begin{figure}[!htb]    \begin{center} 
    660 \includegraphics[width=0.90\textwidth]{./TexFiles/Figures/Fig_npc.pdf} 
     662\includegraphics[width=0.90\textwidth]{Fig_npc} 
    661663\caption{  \label{Fig_npc}  
    662664Example of an unstable density profile treated by the non penetrative  
     
    814816%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    815817\begin{figure}[!t]   \begin{center} 
    816 \includegraphics[width=0.99\textwidth]{./TexFiles/Figures/Fig_zdfddm.pdf} 
     818\includegraphics[width=0.99\textwidth]{Fig_zdfddm} 
    817819\caption{  \label{Fig_zdfddm} 
    818820From \citet{Merryfield1999} : (a) Diapycnal diffusivities $A_f^{vT}$  
     
    11431145baroclinic and barotropic components which is appropriate when using either the 
    11441146explicit or filtered surface pressure gradient algorithms (\key{dynspg\_exp} or  
    1145 {\key{dynspg\_flt}). Extra attention is required, however, when using  
     1147\key{dynspg\_flt}). Extra attention is required, however, when using  
    11461148split-explicit time stepping (\key{dynspg\_ts}). In this case the free surface  
    11471149equation is solved with a small time step \np{rn\_rdt}/\np{nn\_baro}, while the three  
     
    12581260%>>>>>>>>>>>>>>>>>>>>>>>>>>>> 
    12591261\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} 
    12611263\caption{  \label{Fig_ZDF_M2_K1_tmx}  
    12621264(a) M2 and (b) K1 internal wave drag energy from \citet{Carrere_Lyard_GRL03} ($W/m^2$). } 
     
    13691371 
    13701372 
     1373%\end{document} 
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