Changeset 11524
 Timestamp:
 20190910T16:09:48+02:00 (22 months ago)
 Location:
 NEMO/trunk/doc/latex
 Files:

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NEMO/trunk/doc/latex/NEMO/subfiles/chap_TRA.tex
r11459 r11524 139 139 two quantities that are not correlated \citep{roullet.madec_JGR00, griffies.pacanowski.ea_MWR01, campin.adcroft.ea_OM04}. 140 140 141 The velocity field that appears in (\autoref{eq:tra_adv} is 141 The velocity field that appears in (\autoref{eq:tra_adv} is 142 142 the centred (\textit{now}) \textit{effective} ocean velocity, \ie\ the \textit{eulerian} velocity 143 143 (see \autoref{chap:DYN}) plus the eddy induced velocity (\textit{eiv}) and/or … … 471 471 \item[\np{ln\_traldf\_lap}\forcode{ = .true.}:] 472 472 a laplacian operator is selected. 473 This harmonic operator takes the following expression: $\math pzc{L}(T) = \nabla \cdot A_{ht} \; \nabla T $,473 This harmonic operator takes the following expression: $\mathcal{L}(T) = \nabla \cdot A_{ht} \; \nabla T $, 474 474 where the gradient operates along the selected direction (see \autoref{subsec:TRA_ldf_dir}), 475 475 and $A_{ht}$ is the eddy diffusivity coefficient expressed in $m^2/s$ (see \autoref{chap:LDF}). … … 477 477 a bilaplacian operator is selected. 478 478 This biharmonic operator takes the following expression: 479 $\math pzc{B} =  \mathpzc{L}(\mathpzc{L}(T)) =  \nabla \cdot b \nabla (\nabla \cdot b \nabla T)$479 $\mathcal{B} =  \mathcal{L}(\mathcal{L}(T)) =  \nabla \cdot b \nabla (\nabla \cdot b \nabla T)$ 480 480 where the gradient operats along the selected direction, 481 481 and $b^2 = B_{ht}$ is the eddy diffusivity coefficient expressed in $m^4/s$ (see \autoref{chap:LDF}). … … 534 534 where zero diffusive fluxes is assumed across solid boundaries, 535 535 first (and third in bilaplacian case) horizontal tracer derivative are masked. 536 It is implemented in the \rou{tra\_ldf\_lap} subroutine found in the \mdl{traldf\_lap\_blp} }module.536 It is implemented in the \rou{tra\_ldf\_lap} subroutine found in the \mdl{traldf\_lap\_blp} module. 537 537 The module also contains \rou{tra\_ldf\_blp}, the subroutine calling twice \rou{tra\_ldf\_lap} in order to 538 538 compute the isolevel bilaplacian operator. … … 1217 1217 density in the World Ocean varies by no more than 2$\%$ from that value \citep{gill_bk82}. 1218 1218 1219 Options which control the EOS used are defined through the \n gn{nameos} namelist variables.1219 Options which control the EOS used are defined through the \nam{eos} namelist variables. 1220 1220 1221 1221 \begin{description} 
NEMO/trunk/doc/latex/global/document.tex
r11515 r11524 11 11 12 12 %% Document layout 13 \documentclass[ fontsize = 10pt,13 \documentclass[draft, fontsize = 10pt, 14 14 twoside = semi, abstract = on, 15 15 open = right]{scrreprt}
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