Changeset 14644 for NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final/doc/latex/NEMO/subfiles/chap_DOM.tex
- Timestamp:
- 2021-03-26T15:33:49+01:00 (3 years ago)
- Location:
- NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final
- Files:
-
- 3 edited
Legend:
- Unmodified
- Added
- Removed
-
NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final
- Property svn:externals
-
old new 9 9 10 10 # SETTE 11 ^/utils/CI/sette _wave@13990sette11 ^/utils/CI/sette@14244 sette
-
- Property svn:externals
-
NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final/doc/latex/NEMO/subfiles
- Property svn:ignore
-
old new 1 *.aux 2 *.bbl 3 *.blg 4 *.fdb* 5 *.fls 6 *.idx 7 *.ilg 1 8 *.ind 2 *.ilg 9 *.lo* 10 *.out 11 *.pdf 12 *.pyg 13 *.tdo 14 *.toc 15 *.xdv 16 cache*
-
- Property svn:ignore
-
NEMO/branches/2020/dev_r14116_HPC-04_mcastril_Mixed_Precision_implementation_final/doc/latex/NEMO/subfiles/chap_DOM.tex
r11693 r14644 14 14 % - domclo: closed sea and lakes.... 15 15 % management of closea sea area: specific to global cfg, both forced and coupled 16 17 \thispagestyle{plain}18 16 19 17 \chaptertoc … … 368 366 \label{subsec:DOM_size} 369 367 370 The total size of the computational domain is set by the parameters \ jp{jpiglo}, \jp{jpjglo} and371 \ jp{jpkglo} for the $i$, $j$ and $k$ directions, respectively.368 The total size of the computational domain is set by the parameters \texttt{jpiglo}, \texttt{jpjglo} and 369 \texttt{jpkglo} for the $i$, $j$ and $k$ directions, respectively. 372 370 Note, that the variables \texttt{jpi} and \texttt{jpj} refer to 373 371 the size of each processor subdomain when the code is run in parallel using domain decomposition … … 379 377 in which case \np{cn_cfg}{cn\_cfg} and \np{nn_cfg}{nn\_cfg} are set from these values accordingly). 380 378 381 The global lateral boundary condition type is selected from 8 options using parameter \jp{jperio}.379 The global lateral boundary condition type is selected from 8 options using parameters \texttt{l\_Iperio}, \texttt{l\_Jperio}, \texttt{l\_NFold} and \texttt{c\_NFtype}. 382 380 See \autoref{sec:LBC_jperio} for details on the available options and 383 the corresponding values for \ jp{jperio}.381 the corresponding values for \texttt{l\_Iperio}, \texttt{l\_Jperio}, \texttt{l\_NFold} and \texttt{c\_NFtype}. 384 382 385 383 %% ================================================================================================= … … 396 394 397 395 \begin{clines} 398 int jpiglo, jpjglo, jpkglo /* global domain sizes */ 399 int jperio /* lateral global domain b.c. */ 400 double glamt, glamu, glamv, glamf /* geographic longitude (t,u,v and f points respectively) */ 401 double gphit, gphiu, gphiv, gphif /* geographic latitude */ 402 double e1t, e1u, e1v, e1f /* horizontal scale factors */ 403 double e2t, e2u, e2v, e2f /* horizontal scale factors */ 396 integer Ni0glo, NjOglo, jpkglo /* global domain sizes (without MPI halos) */ 397 logical l\_Iperio, l\_Jperio /* lateral global domain b.c.: i- j-periodicity */ 398 logical l\_NFold /* lateral global domain b.c.: North Pole folding */ 399 char(1) c\_NFtype /* type of North pole Folding: T or F point */ 400 real glamt, glamu, glamv, glamf /* geographic longitude (t,u,v and f points respectively) */ 401 real gphit, gphiu, gphiv, gphif /* geographic latitude */ 402 real e1t, e1u, e1v, e1f /* horizontal scale factors */ 403 real e2t, e2u, e2v, e2f /* horizontal scale factors */ 404 404 \end{clines} 405 405 … … 465 465 \begin{enumerate} 466 466 \item the bathymetry given in meters; 467 \item the number of levels of the model (\ jp{jpk});467 \item the number of levels of the model (\texttt{jpk}); 468 468 \item the analytical transformation $z(i,j,k)$ and the vertical scale factors 469 469 (derivatives of the transformation); and … … 575 575 every gridcell in the model regardless of the choice of vertical coordinate. 576 576 With constant z-levels, e3 metrics will be uniform across each horizontal level. 577 In the partial step case each e3 at the \ jp{bottom\_level}578 (and, possibly, \ jp{top\_level} if ice cavities are present)577 In the partial step case each e3 at the \texttt{bottom\_level} 578 (and, possibly, \texttt{top\_level} if ice cavities are present) 579 579 may vary from its horizontal neighbours. 580 580 And, in s-coordinates, variations can occur throughout the water column. … … 585 585 those arising from a flat sea surface with zero elevation. 586 586 587 The \ jp{bottom\_level} and \jp{top\_level} 2D arrays define588 the \ jp{bottom\_level} and top wet levels in each grid column.589 Without ice cavities, \ jp{top\_level} is essentially a land mask (0 on land; 1 everywhere else).590 With ice cavities, \ jp{top\_level} determines the first wet point below the overlying ice shelf.587 The \texttt{bottom\_level} and \texttt{top\_level} 2D arrays define 588 the \texttt{bottom\_level} and top wet levels in each grid column. 589 Without ice cavities, \texttt{top\_level} is essentially a land mask (0 on land; 1 everywhere else). 590 With ice cavities, \texttt{top\_level} determines the first wet point below the overlying ice shelf. 591 591 592 592 %% ================================================================================================= … … 594 594 \label{subsec:DOM_msk} 595 595 596 From \ jp{top\_level} and \jp{bottom\_level} fields, the mask fields are defined as follows:596 From \texttt{top\_level} and \texttt{bottom\_level} fields, the mask fields are defined as follows: 597 597 \begin{align*} 598 598 tmask(i,j,k) &=
Note: See TracChangeset
for help on using the changeset viewer.