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branches/nemo_v3_3_beta/DOC/TexFiles/Chapters/Chap_TRA.tex
r2349 r2376 90 90 the continuity equation which is used to calculate the vertical velocity. 91 91 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 92 \begin{figure}[!t] \label{Fig_adv_scheme}\begin{center}92 \begin{figure}[!t] \begin{center} 93 93 \includegraphics[width=0.9\textwidth]{./TexFiles/Figures/Fig_adv_scheme.pdf} 94 \caption{Schematic representation of some ways used to evaluate the tracer value 94 \caption{ \label{Fig_adv_scheme} 95 Schematic representation of some ways used to evaluate the tracer value 95 96 at $u$-point and the amount of tracer exchanged between two neighbouring grid 96 97 points. Upsteam biased scheme (ups): the upstream value is used and the black … … 836 837 837 838 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 838 \begin{figure}[!t] \label{Fig_traqsr_irradiance}\begin{center}839 \begin{figure}[!t] \begin{center} 839 840 \includegraphics[width=1.0\textwidth]{./TexFiles/Figures/Fig_TRA_Irradiance.pdf} 840 \caption{Penetration profile of the downward solar irradiance 841 calculated by four models. Two waveband chlorophyll-independent formulation (blue), 842 a chlorophyll-dependent monochromatic formulation (green), 4 waveband RGB formulation (red), 841 \caption{ \label{Fig_traqsr_irradiance} 842 Penetration profile of the downward solar irradiance calculated by four models. 843 Two waveband chlorophyll-independent formulation (blue), a chlorophyll-dependent 844 monochromatic formulation (green), 4 waveband RGB formulation (red), 843 845 61 waveband Morel (1988) formulation (black) for a chlorophyll concentration of 844 846 (a) Chl=0.05 mg/m$^3$ and (b) Chl=0.5 mg/m$^3$. From \citet{Lengaigne_al_CD07}.} … … 856 858 %-------------------------------------------------------------------------------------------------------------- 857 859 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 858 \begin{figure}[!t] \label{Fig_geothermal}\begin{center}860 \begin{figure}[!t] \begin{center} 859 861 \includegraphics[width=1.0\textwidth]{./TexFiles/Figures/Fig_TRA_geoth.pdf} 860 \caption{Geothermal Heat flux (in $mW.m^{-2}$) used by \cite{Emile-Geay_Madec_OS09}. 862 \caption{ \label{Fig_geothermal} 863 Geothermal Heat flux (in $mW.m^{-2}$) used by \cite{Emile-Geay_Madec_OS09}. 861 864 It is inferred from the age of the sea floor and the formulae of \citet{Stein_Stein_Nat92}.} 862 865 \end{center} \end{figure} … … 963 966 964 967 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 965 \begin{figure}[!t] \label{Fig_bbl}\begin{center}968 \begin{figure}[!t] \begin{center} 966 969 \includegraphics[width=0.7\textwidth]{./TexFiles/Figures/Fig_BBL_adv.pdf} 967 \caption{Advective/diffusive Bottom Boundary Layer. The BBL parameterisation is 970 \caption{ \label{Fig_bbl} 971 Advective/diffusive Bottom Boundary Layer. The BBL parameterisation is 968 972 activated when $\rho^i_{kup}$ is larger than $\rho^{i+1}_{kdnw}$. 969 973 Red arrows indicate the additional overturning circulation due to the advective BBL. … … 1316 1320 1317 1321 %>>>>>>>>>>>>>>>>>>>>>>>>>>>> 1318 \begin{figure}[!p] \label{Fig_Partial_step_scheme}\begin{center}1322 \begin{figure}[!p] \begin{center} 1319 1323 \includegraphics[width=0.9\textwidth]{./TexFiles/Figures/Partial_step_scheme.pdf} 1320 \caption{ Discretisation of the horizontal difference and average of tracers in the $z$-partial step coordinate (\np{ln\_zps}=true) in the case $( e3w_k^{i+1} - e3w_k^i )>0$. A linear interpolation is used to estimate $\widetilde{T}_k^{i+1}$, the tracer value at the depth of the shallower tracer point of the two adjacent bottom $T$-points. The horizontal difference is then given by: $\delta _{i+1/2} T_k= \widetilde{T}_k^{\,i+1} -T_k^{\,i}$ and the average by: $\overline{T}_k^{\,i+1/2}= ( \widetilde{T}_k^{\,i+1/2} - T_k^{\,i} ) / 2$. } 1324 \caption{ \label{Fig_Partial_step_scheme} 1325 Discretisation of the horizontal difference and average of tracers in the $z$-partial 1326 step coordinate (\np{ln\_zps}=true) in the case $( e3w_k^{i+1} - e3w_k^i )>0$. 1327 A linear interpolation is used to estimate $\widetilde{T}_k^{i+1}$, the tracer value 1328 at the depth of the shallower tracer point of the two adjacent bottom $T$-points. 1329 The horizontal difference is then given by: $\delta _{i+1/2} T_k= \widetilde{T}_k^{\,i+1} -T_k^{\,i}$ 1330 and the average by: $\overline{T}_k^{\,i+1/2}= ( \widetilde{T}_k^{\,i+1/2} - T_k^{\,i} ) / 2$. } 1321 1331 \end{center} \end{figure} 1322 1332 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>
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