Changeset 11582 for NEMO/trunk/doc/latex/NEMO/subfiles/apdx_DOMAINcfg.tex
- Timestamp:
- 2019-09-20T11:44:31+02:00 (5 years ago)
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NEMO/trunk/doc/latex/NEMO/subfiles/apdx_DOMAINcfg.tex
r11578 r11582 1 1 \documentclass[../main/NEMO_manual]{subfiles} 2 3 \onlyinsubfile{\makeindex} 2 4 3 5 \begin{document} … … 55 57 56 58 \begin{description} 57 \item[ \np{jphgr_mesh}{jphgr\_mesh}=0] The most general curvilinear orthogonal grids.59 \item[{\np{jphgr_mesh}{jphgr\_mesh}=0}] The most general curvilinear orthogonal grids. 58 60 The coordinates and their first derivatives with respect to $i$ and $j$ are provided 59 61 in a input file (\ifile{coordinates}), read in \rou{hgr\_read} subroutine of the domhgr module. 60 62 This is now the only option available within \NEMO\ itself from v4.0 onwards. 61 \item[ \np{jphgr_mesh}{jphgr\_mesh}=1 to 5] A few simple analytical grids are provided (see below).63 \item[{\np{jphgr_mesh}{jphgr\_mesh}=1 to 5}] A few simple analytical grids are provided (see below). 62 64 For other analytical grids, the \mdl{domhgr} module (\texttt{DOMAINcfg} variant) must be 63 65 modified by the user. In most cases, modifying the \mdl{usrdef\_hgr} module of \NEMO\ is … … 136 138 137 139 It is possible to define a simple regular vertical grid by giving zero stretching 138 (\np {ppacr}{ppacr}\forcode{ = 0}). In that case, the parameters \jp{jpk} (number of $w$-levels)140 (\np[=0]{ppacr}{ppacr}). In that case, the parameters \jp{jpk} (number of $w$-levels) 139 141 and \np{pphmax}{pphmax} (total ocean depth in meters) fully define the grid. 140 142 … … 152 154 top and bottom with a smooth hyperbolic tangent transition in between (\autoref{fig:DOMCFG_zgr}). 153 155 154 A double hyperbolic tangent version (\np {ldbletanh}{ldbletanh}\forcode{ = .true.}) is also available156 A double hyperbolic tangent version (\np[=.true.]{ldbletanh}{ldbletanh}) is also available 155 157 which permits finer control and is used, typically, to obtain a well resolved upper ocean 156 158 without compromising on resolution at depth using a moderate number of levels. … … 170 172 \end{gather} 171 173 172 If the ice shelf cavities are opened (\np {ln_isfcav}{ln\_isfcav}\forcode{ = .true.}), the definition174 If the ice shelf cavities are opened (\np[=.true.]{ln_isfcav}{ln\_isfcav}), the definition 173 175 of $z_0$ is the same. However, definition of $e_3^0$ at $t$- and $w$-points is 174 176 respectively changed to: … … 314 316 \np{nn_bathy}{nn\_bathy} (found in \nam{dom}{dom} namelist (\texttt{DOMAINCFG} variant) ): 315 317 \begin{description} 316 \item[ \np{nn_bathy}{nn\_bathy}\forcode{ = 0}]:318 \item[{\np[=0]{nn_bathy}{nn\_bathy}}]: 317 319 a flat-bottom domain is defined. 318 320 The total depth $z_w (jpk)$ is given by the coordinate transformation. 319 321 The domain can either be a closed basin or a periodic channel depending on the parameter \np{jperio}{jperio}. 320 \item[ \np{nn_bathy}{nn\_bathy}\forcode{ = -1}]:322 \item[{\np[=-1]{nn_bathy}{nn\_bathy}}]: 321 323 a domain with a bump of topography one third of the domain width at the central latitude. 322 324 This is meant for the "EEL-R5" configuration, a periodic or open boundary channel with a seamount. 323 \item[ \np{nn_bathy}{nn\_bathy}\forcode{ = 1}]:325 \item[{\np[=1]{nn_bathy}{nn\_bathy}}]: 324 326 read a bathymetry and ice shelf draft (if needed). 325 327 The \ifile{bathy\_meter} file (Netcdf format) provides the ocean depth (positive, in meters) at … … 332 334 The \ifile{isfdraft\_meter} file (Netcdf format) provides the ice shelf draft (positive, in meters) at 333 335 each grid point of the model grid. 334 This file is only needed if \np {ln_isfcav}{ln\_isfcav}\forcode{ = .true.}.336 This file is only needed if \np[=.true.]{ln_isfcav}{ln\_isfcav}. 335 337 Defining the ice shelf draft will also define the ice shelf edge and the grounding line position. 336 338 \end{description} … … 412 414 %-------------------------------------------------------------------------------------------------------------- 413 415 Options are defined in \nam{zgr_sco}{zgr\_sco} (\texttt{DOMAINcfg} only). 414 In $s$-coordinate (\np {ln_sco}{ln\_sco}\forcode{ = .true.}), the depth and thickness of the model levels are defined from416 In $s$-coordinate (\np[=.true.]{ln_sco}{ln\_sco}), the depth and thickness of the model levels are defined from 415 417 the product of a depth field and either a stretching function or its derivative, respectively: 416 418 … … 435 437 436 438 The original default \NEMO\ s-coordinate stretching is available if neither of the other options are specified as true 437 (\np {ln_s_SH94}{ln\_s\_SH94}\forcode{ = .false.} and \np{ln_s_SF12}{ln\_s\_SF12}\forcode{ = .false.}).439 (\np[=.false.]{ln_s_SH94}{ln\_s\_SH94} and \np[=.false.]{ln_s_SF12}{ln\_s\_SF12}). 438 440 This uses a depth independent $\tanh$ function for the stretching \citep{madec.delecluse.ea_JPO96}: 439 441 … … 455 457 456 458 A stretching function, 457 modified from the commonly used \citet{song.haidvogel_JCP94} stretching (\np {ln_s_SH94}{ln\_s\_SH94}\forcode{ = .true.}),459 modified from the commonly used \citet{song.haidvogel_JCP94} stretching (\np[=.true.]{ln_s_SH94}{ln\_s\_SH94}), 458 460 is also available and is more commonly used for shelf seas modelling: 459 461 … … 558 560 This option is described in the Report by Levier \textit{et al.} (2007), available on the \NEMO\ web site. 559 561 560 \ biblio561 562 \ pindex562 \onlyinsubfile{\bibliography{../main/bibliography}} 563 564 \onlyinsubfile{\printindex} 563 565 564 566 \end{document}
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