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Changeset 6289 for trunk/DOC/TexFiles/Chapters/Chap_LDF.tex – NEMO

Ignore:
Timestamp:
2016-02-05T00:47:05+01:00 (8 years ago)
Author:
gm
Message:

#1673 DOC of the trunk - Update, see associated wiki page for description

File:
1 edited

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  • trunk/DOC/TexFiles/Chapters/Chap_LDF.tex

    r6140 r6289  
    6969 r_{1u} &= \frac{e_{3u}}{ \left( e_{1u}\;\overline{\overline{e_{3w}}}^{\,i+1/2,\,k} \right)} 
    7070           \;\delta_{i+1/2}[z_t]  
    71       &\approx \frac{1}{e_{1u}}\; \delta_{i+1/2}[z_t]  
     71      &\approx \frac{1}{e_{1u}}\; \delta_{i+1/2}[z_t] \ \ \ 
    7272\\ 
    7373 r_{2v} &= \frac{e_{3v}}{\left( e_{2v}\;\overline{\overline{e_{3w}}}^{\,j+1/2,\,k} \right)}  
    7474           \;\delta_{j+1/2} [z_t]  
    75       &\approx \frac{1}{e_{2v}}\; \delta_{j+1/2}[z_t]  
     75      &\approx \frac{1}{e_{2v}}\; \delta_{j+1/2}[z_t] \ \ \ 
    7676\\ 
    7777 r_{1w} &= \frac{1}{e_{1w}}\;\overline{\overline{\delta_{i+1/2}[z_t]}}^{\,i,\,k+1/2} 
     
    448448\label{LDF_eiv} 
    449449 
     450%%gm  from Triad appendix  : to be incorporated.... 
     451\gmcomment{ 
     452Values of iso-neutral diffusivity and GM coefficient are set as 
     453described in \S\ref{LDF_coef}. If none of the keys \key{traldf\_cNd}, 
     454N=1,2,3 is set (the default), spatially constant iso-neutral $A_l$ and 
     455GM diffusivity $A_e$ are directly set by \np{rn\_aeih\_0} and 
     456\np{rn\_aeiv\_0}. If 2D-varying coefficients are set with 
     457\key{traldf\_c2d} then $A_l$ is reduced in proportion with horizontal 
     458scale factor according to \eqref{Eq_title} \footnote{Except in global ORCA 
     459  $0.5^{\circ}$ runs with \key{traldf\_eiv}, where 
     460  $A_l$ is set like $A_e$ but with a minimum vale of 
     461  $100\;\mathrm{m}^2\;\mathrm{s}^{-1}$}. In idealised setups with 
     462\key{traldf\_c2d}, $A_e$ is reduced similarly, but if \key{traldf\_eiv} 
     463is set in the global configurations with \key{traldf\_c2d}, a horizontally varying $A_e$ is 
     464instead set from the Held-Larichev parameterisation\footnote{In this 
     465  case, $A_e$ at low latitudes $|\theta|<20^{\circ}$ is further 
     466  reduced by a factor $|f/f_{20}|$, where $f_{20}$ is the value of $f$ 
     467  at $20^{\circ}$~N} (\mdl{ldfeiv}) and \np{rn\_aeiv\_0} is ignored 
     468unless it is zero. 
     469} 
     470 
    450471When Gent and McWilliams [1990] diffusion is used (\key{traldf\_eiv} defined),  
    451472an eddy induced tracer advection term is added, the formulation of which  
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