Changeset 2274

Timestamp:

2010-10-15T10:41:19+02:00 (14 years ago)

Author:

gm

Message:

ticket:#658 add the Griffies operator documentation from DEV_r1924_nocs_latphys branche

Location:

branches/DEV_r1826_DOC/DOC/TexFiles

Files:

• Biblio/Biblio.bib (modified) (1 diff)
• Chapters/Chap_DOM.tex (modified) (1 diff)
• Chapters/Chap_STP.tex (modified) (1 diff)
• Chapters/Chap_TRA.tex (modified) (1 diff)

branches/DEV_r1826_DOC/DOC/TexFiles/Biblio/Biblio.bib

@@ -96 +96 @@
 @ARTICLE{Adcroft_Campin_OM04,
   author = {A. Adcroft and J.-M. Campin},
-  title = {Re-scaled height coordinates for accurate representation of free-surface
-   flows in ocean circulation models},
+  title = {Re-scaled height coordinates for accurate representation of free-surface flows in ocean circulation models},
   journal = OM,
-  year = {2004},
   volume = {7},
-  owner = {gm},
-  timestamp = {2008.01.27}
+  year = {2004}
 }
 
 @ARTICLE{Arakawa1966,
   author = {A. Arakawa},
-  title = {Computational design for long term numerical integration of the equations
-   of fluid motion, two-dimensional incompressible flow, Part. I.},
+  title = {Computational design for long term numerical integration of the equations of fluid motion, two-dimensional incompressible flow, Part. I.},
   journal = JCP,
   year = {1966},
   volume = {I},
-  pages = {119--149},
-  owner = {gm},
-  timestamp = {2007.08.04}
+  pages = {119--149}
 }
 

branches/DEV_r1826_DOC/DOC/TexFiles/Chapters/Chap_DOM.tex

@@ -528 +528 @@
 C-Pre-Processor (CPP) key. To improve the code readability while providing this 
 flexibility, the vertical coordinate and scale factors are defined as functions of 
-$(i,j,k)$ with "fs" as prefix (examples: \textit{fsdeptht, fse3t,} etc) that can be either 
+$(i,j,k)$ with "fs" as prefix (examples: \textit{fsdept, fse3t,} etc) that can be either 
 three-dimensional arrays, or a one dimensional array when \key{zco} is defined. 
 These functions are defined in the file \hf{domzgr\_substitute} of the DOM directory. 

branches/DEV_r1826_DOC/DOC/TexFiles/Chapters/Chap_STP.tex

@@ -290 +290 @@
 \caption{Illustration of forcing integration methods. 
 (top) ''Traditional'' formulation : the forcing is defined at the same time as the variable 
-on which it is applied (integer value of the time step index) and it is applied over a $2\rdt$ period. 
-(bottom)  modified formulation : the forcing is defined in the mid of the time (integer and a half 
-value of the time step index) and the mean of two successive forcing ($n-1/2$, $n+1/2$).
+to which it is applied (integer value of the time step index) and it is applied over a $2\rdt$ period. 
+(bottom)  modified formulation : the forcing is defined in the middle of the time (integer and a half 
+value of the time step index) and the mean of two successive forcing values ($n-1/2$, $n+1/2$).
 is applied over a $2\rdt$ period.}
 \end{center}   \end{figure}
 %>>>>>>>>>>>>>>>>>>>>>>>>>>>>
-
-\sgacomment{two methods in caption sound the same ==> gm:  I try to change this, but I'm not happy with the result}
 
 % -------------------------------------------------------------------------------------------------------------

branches/DEV_r1826_DOC/DOC/TexFiles/Chapters/Chap_TRA.tex

@@ -543 +543 @@
 background horizontal diffusion \citep{Guilyardi_al_CD01}. An alternative scheme 
 developed by \cite{Griffies_al_JPO98} which preserves both tracer and its variance 
-is also available in \NEMO (\np{ln\_traldf_grif}=true).
+is also available in \NEMO (\np{ln\_traldf\_grif}=true). A complete description of 
+the algorithm is given in App.\ref{Apdx_Griffies}.
 
 Note that in the partial step $z$-coordinate (\np{ln\_zps}=true), the horizontal