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- 2016-10-05T14:07:19+02:00 (7 years ago)
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branches/2015/nemo_v3_6_STABLE/DOC/TexFiles/Chapters/Chap_DYN.tex
r6396 r6992 1 %\documentclass[NEMO_book]{subfiles} 2 %\begin{document} 1 3 % ================================================================ 2 4 % Chapter ——— Ocean Dynamics (DYN) … … 293 295 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>>> 294 296 \begin{figure}[!ht] \begin{center} 295 \includegraphics[width=0.70\textwidth]{ ./TexFiles/Figures/Fig_DYN_een_triad.pdf}297 \includegraphics[width=0.70\textwidth]{Fig_DYN_een_triad} 296 298 \caption{ \label{Fig_DYN_een_triad} 297 299 Triads used in the energy and enstrophy conserving scheme (een) for … … 660 662 $\bullet$ The main hypothesis to compute the ice shelf load is that the ice shelf is in isostatic equilibrium. 661 663 The top pressure is computed integrating a reference density profile (prescribed as density of a water at 34.4 662 PSU and -1.9$ \degresC$) from the sea surface to the ice shelf base, which corresponds to the load of the water664 PSU and -1.9$^{\circ}C$) from the sea surface to the ice shelf base, which corresponds to the load of the water 663 665 column in which the ice shelf is floatting. This top pressure is constant over time. A detailed description of 664 666 this method is described in \citet{Losch2008}.\\ … … 827 829 %> > > > > > > > > > > > > > > > > > > > > > > > > > > > 828 830 \begin{figure}[!t] \begin{center} 829 \includegraphics[width=0.7\textwidth]{ ./TexFiles/Figures/Fig_DYN_dynspg_ts.pdf}831 \includegraphics[width=0.7\textwidth]{Fig_DYN_dynspg_ts} 830 832 \caption{ \label{Fig_DYN_dynspg_ts} 831 833 Schematic of the split-explicit time stepping scheme for the external … … 1332 1334 1333 1335 % ================================================================ 1336 %\end{document}
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