Changeset 6497 for trunk/DOC/TexFiles/Chapters/Chap_DOM.tex
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- 2016-04-27T09:33:46+02:00 (8 years ago)
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trunk/DOC/TexFiles/Chapters/Chap_DOM.tex
r6320 r6497 486 486 The last choice in terms of vertical coordinate concerns the presence (or not) in the model domain 487 487 of ocean cavities beneath ice shelves. Setting \np{ln\_isfcav} to true allows to manage ocean cavities, 488 otherwise they are filled in. 488 otherwise they are filled in. This option is currently only available in $z$- or $zps$-coordinate, 489 and partial step are also applied at the ocean/ice shelf interface. 489 490 490 491 Contrary to the horizontal grid, the vertical grid is computed in the code and no … … 772 773 \end{equation} 773 774 774 where $s_{min}$ is the depth at which the s-coordinate stretching starts and775 allows a z-coordinate to placed on top of the stretched coordinate,776 and zis the depth (negative down from the asea surface).775 where $s_{min}$ is the depth at which the $s$-coordinate stretching starts and 776 allows a $z$-coordinate to placed on top of the stretched coordinate, 777 and $z$ is the depth (negative down from the asea surface). 777 778 778 779 \begin{equation} … … 886 887 that do not communicate with another ocean point at the same level are eliminated. 887 888 888 In case of ice shelf cavities, as for the representation of bathymetry, a 2D integer array, misfdep, is created. 889 misfdep defines the level of the first wet $t$-point (ie below the ice-shelf/ocean interface). All the cells between $k=1$ and $misfdep(i,j)-1$ are masked. 890 By default, $misfdep(:,:)=1$ and no cells are masked. 891 Modifications of the model bathymetry and ice shelf draft into 889 As for the representation of bathymetry, a 2D integer array, misfdep, is created. 890 misfdep defines the level of the first wet $t$-point. All the cells between $k=1$ and $misfdep(i,j)-1$ are masked. 891 By default, misfdep(:,:)=1 and no cells are masked. 892 893 In case of ice shelf cavities, modifications of the model bathymetry and ice shelf draft into 892 894 the cavities are performed in the \textit{zgr\_isf} routine. The compatibility between ice shelf draft and bathymetry is checked. 893 895 All the locations where the isf cavity is thinnest than \np{rn\_isfhmin} meters are grounded ($i.e.$ masked). … … 903 905 vmask(i,j,k) &= \; tmask(i,j,k) \ * \ tmask(i,j+1,k) \\ 904 906 fmask(i,j,k) &= \; tmask(i,j,k) \ * \ tmask(i+1,j,k) \\ 905 &\ \ \, * tmask(i,j,k) \ * \ tmask(i+1,j,k) \\907 & \ \ \, * tmask(i,j,k) \ * \ tmask(i+1,j,k) \\ 906 908 wmask(i,j,k) &= \; tmask(i,j,k) \ * \ tmask(i,j,k-1) \text{ with } wmask(i,j,1) = tmask(i,j,1) 907 909 \end{align*} 908 910 909 Note, wmask is now defined. It allows, in case of ice shelves, 910 to deal with the top boundary (ice shelf/ocean interface) exactly in the same way as for the bottom boundary. 911 Note that, without ice shelves cavities, masks at $t-$ and $w-$points are identical with 912 the numerical indexing used (\S~\ref{DOM_Num_Index}). Nevertheless, $wmask$ are required 913 with oceean cavities to deal with the top boundary (ice shelf/ocean interface) 914 exactly in the same way as for the bottom boundary. 911 915 912 916 The specification of closed lateral boundaries requires that at least the first and last … … 916 920 (and so too the mask arrays) (see \S~\ref{LBC_jperio}). 917 921 918 %%%919 \gmcomment{ \colorbox{yellow}{Add one word on tricky trick !} mbathy in further modified in zdfbfr{\ldots}. }920 %%%921 922 922 923 % ================================================================
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