Changeset 14789 for NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU/doc/latex/NEMO/subfiles/apdx_DOMAINcfg.tex
- Timestamp:
- 2021-05-05T13:18:04+02:00 (3 years ago)
- Location:
- NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU
- Files:
-
- 3 edited
Legend:
- Unmodified
- Added
- Removed
-
NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU
- Property svn:externals
-
old new 3 3 ^/utils/build/mk@HEAD mk 4 4 ^/utils/tools@HEAD tools 5 ^/vendors/AGRIF/dev _r12970_AGRIF_CMEMSext/AGRIF5 ^/vendors/AGRIF/dev@HEAD ext/AGRIF 6 6 ^/vendors/FCM@HEAD ext/FCM 7 7 ^/vendors/IOIPSL@HEAD ext/IOIPSL 8 ^/vendors/PPR@HEAD ext/PPR 8 9 9 10 # SETTE 10 ^/utils/CI/sette@1 3559sette11 ^/utils/CI/sette@14244 sette
-
- Property svn:externals
-
NEMO/branches/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU/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/2021/dev_r13747_HPC-11_mcastril_HPDAonline_DiagGPU/doc/latex/NEMO/subfiles/apdx_DOMAINcfg.tex
r11693 r14789 6 6 \label{apdx:DOMCFG} 7 7 8 % {\em 4.0} & {\em Andrew Coward} & {\em Created at v4.0 from materials removed from chap\_DOM that are still relevant to the \forcode{DOMAINcfg} tool and which illustrate and explain the choices to be made by the user when setting up new domains } \\9 10 \thispagestyle{plain}11 12 8 \chaptertoc 13 9 … … 16 12 {\footnotesize 17 13 \begin{tabularx}{\textwidth}{l||X|X} 18 Release & Author(s) & Modifications\\19 \hline 20 {\em 4.0} & {\em ...} & {\em ...} \\21 {\em 3.6} & {\em ...} & {\em ...} \\22 {\em 3.4} & {\em ...} & {\em ...} \\23 {\em <=3.4} & {\em ...} & {\em ...}14 Release & Author(s) & Modifications \\ 15 \hline 16 {\em next} & {\em Pierre Mathiot} & {\em Add ice shelf and closed sea option description } \\ 17 {\em 4.0} & {\em Andrew Coward} & {\em Creation from materials removed from \autoref{chap:DOM} 18 that are still relevant to the DOMAINcfg tool 19 when setting up new domains } 24 20 \end{tabularx} 25 21 } … … 46 42 47 43 \begin{listing} 48 \nlst{namdom_domcfg} 44 \begin{forlines} 45 !----------------------------------------------------------------------- 46 &namdom ! space and time domain (bathymetry, mesh, timestep) 47 !----------------------------------------------------------------------- 48 nn_bathy = 1 ! compute analyticaly (=0) or read (=1) the bathymetry file 49 ! or compute (2) from external bathymetry 50 nn_interp = 1 ! type of interpolation (nn_bathy =2) 51 cn_topo = 'bathymetry_ORCA12_V3.3.nc' ! external topo file (nn_bathy =2) 52 cn_bath = 'Bathymetry' ! topo name in file (nn_bathy =2) 53 cn_lon = 'nav_lon' ! lon name in file (nn_bathy =2) 54 cn_lat = 'nav_lat' ! lat name in file (nn_bathy =2) 55 rn_scale = 1 56 rn_bathy = 0. ! value of the bathymetry. if (=0) bottom flat at jpkm1 57 jphgr_msh = 0 ! type of horizontal mesh 58 ppglam0 = 999999.0 ! longitude of first raw and column T-point (jphgr_msh = 1) 59 ppgphi0 = 999999.0 ! latitude of first raw and column T-point (jphgr_msh = 1) 60 ppe1_deg = 999999.0 ! zonal grid-spacing (degrees) 61 ppe2_deg = 999999.0 ! meridional grid-spacing (degrees) 62 ppe1_m = 999999.0 ! zonal grid-spacing (degrees) 63 ppe2_m = 999999.0 ! meridional grid-spacing (degrees) 64 ppsur = -4762.96143546300 ! ORCA r4, r2 and r05 coefficients 65 ppa0 = 255.58049070440 ! (default coefficients) 66 ppa1 = 245.58132232490 ! 67 ppkth = 21.43336197938 ! 68 ppacr = 3.0 ! 69 ppdzmin = 999999. ! Minimum vertical spacing 70 pphmax = 999999. ! Maximum depth 71 ldbletanh = .FALSE. ! Use/do not use double tanf function for vertical coordinates 72 ppa2 = 999999. ! Double tanh function parameters 73 ppkth2 = 999999. ! 74 ppacr2 = 999999. ! 75 / 76 \end{forlines} 49 77 \caption{\forcode{&namdom_domcfg}} 50 78 \label{lst:namdom_domcfg} … … 58 86 \item [{\np{jphgr_mesh}{jphgr\_mesh}=0}] The most general curvilinear orthogonal grids. 59 87 The coordinates and their first derivatives with respect to $i$ and $j$ are provided 60 in a input file (\ ifile{coordinates}), read in \rou{hgr\_read} subroutine of the domhgr module.88 in a input file (\textit{coordinates.nc}), read in \rou{hgr\_read} subroutine of the domhgr module. 61 89 This is now the only option available within \NEMO\ itself from v4.0 onwards. 62 90 \item [{\np{jphgr_mesh}{jphgr\_mesh}=1 to 5}] A few simple analytical grids are provided (see below). … … 123 151 The reference coordinate transformation $z_0(k)$ defines the arrays $gdept_0$ and 124 152 $gdepw_0$ for $t$- and $w$-points, respectively. See \autoref{sec:DOMCFG_sco} for the 125 S-coordinate options. As indicated on \autoref{fig:DOM_index_vert} \ jp{jpk} is the number of126 $w$-levels. $gdepw_0(1)$ is the ocean surface. There are at most \ jp{jpk}-1 $t$-points153 S-coordinate options. As indicated on \autoref{fig:DOM_index_vert} \texttt{jpk} is the number of 154 $w$-levels. $gdepw_0(1)$ is the ocean surface. There are at most \texttt{jpk}-1 $t$-points 127 155 inside the ocean, the additional $t$-point at $jk = jpk$ is below the sea floor and is not 128 156 used. The vertical location of $w$- and $t$-levels is defined from the analytic … … 134 162 135 163 It is possible to define a simple regular vertical grid by giving zero stretching 136 (\np[=0]{ppacr}{ppacr}). In that case, the parameters \ jp{jpk} (number of $w$-levels)164 (\np[=0]{ppacr}{ppacr}). In that case, the parameters \texttt{jpk} (number of $w$-levels) 137 165 and \np{pphmax}{pphmax} (total ocean depth in meters) fully define the grid. 138 166 … … 146 174 \end{gather} 147 175 148 where $k = 1$ to \ jp{jpk} for $w$-levels and $k = 1$ to $k = 1$ for $t-$levels. Such an176 where $k = 1$ to \texttt{jpk} for $w$-levels and $k = 1$ to $k = 1$ for $t-$levels. Such an 149 177 expression allows us to define a nearly uniform vertical location of levels at the ocean 150 178 top and bottom with a smooth hyperbolic tangent transition in between (\autoref{fig:DOMCFG_zgr}). … … 194 222 \end{equation} 195 223 196 With the choice of the stretching $h_{cr} = 3$ and the number of levels \ jp{jpk}~$= 31$,224 With the choice of the stretching $h_{cr} = 3$ and the number of levels \texttt{jpk}~$= 31$, 197 225 the four coefficients $h_{sur}$, $h_0$, $h_1$, and $h_{th}$ in 198 226 \autoref{eq:DOMCFG_zgr_ana_2} have been determined such that \autoref{eq:DOMCFG_zgr_coef} … … 212 240 Values from $3$ to $10$ are usual. 213 241 \item \np{ppkth}{ppkth}~$= h_{th}$: is approximately the model level at which maximum stretching occurs 214 (nondimensional, usually of order 1/2 or 2/3 of \ jp{jpk})242 (nondimensional, usually of order 1/2 or 2/3 of \texttt{jpk}) 215 243 \item \np{ppdzmin}{ppdzmin}: minimum thickness for the top layer (in meters). 216 244 \item \np{pphmax}{pphmax}: total depth of the ocean (meters). … … 218 246 219 247 As an example, for the $45$ layers used in the DRAKKAR configuration those parameters are: 220 \ jp{jpk}~$= 46$, \np{ppacr}{ppacr}~$= 9$, \np{ppkth}{ppkth}~$= 23.563$, \np{ppdzmin}{ppdzmin}~$= 6~m$,248 \texttt{jpk}~$= 46$, \np{ppacr}{ppacr}~$= 9$, \np{ppkth}{ppkth}~$= 23.563$, \np{ppdzmin}{ppdzmin}~$= 6~m$, 221 249 \np{pphmax}{pphmax}~$= 5750~m$. 222 250 … … 313 341 This is meant for the "EEL-R5" configuration, a periodic or open boundary channel with a seamount. 314 342 \item [{\np[=1]{nn_bathy}{nn\_bathy}}]: read a bathymetry and ice shelf draft (if needed). 315 The \ ifile{bathy\_meter} file (Netcdf format) provides the ocean depth (positive, in meters) at343 The \textit{bathy\_meter.nc} file (Netcdf format) provides the ocean depth (positive, in meters) at 316 344 each grid point of the model grid. 317 345 The bathymetry is usually built by interpolating a standard bathymetry product (\eg\ ETOPO2) onto … … 319 347 Defining the bathymetry also defines the coastline: where the bathymetry is zero, 320 348 no wet levels are defined (all levels are masked). 321 322 The \ifile{isfdraft\_meter} file (Netcdf format) provides the ice shelf draft (positive, in meters) at323 each grid point of the model grid.324 This file is only needed if \np[=.true.]{ln_isfcav}{ln\_isfcav}.325 Defining the ice shelf draft will also define the ice shelf edge and the grounding line position.326 349 \end{description} 327 350 … … 363 386 bathymetry varies by less than one level thickness from one grid point to the next). The 364 387 reference layer thicknesses $e_{3t}^0$ have been defined in the absence of bathymetry. 365 With partial steps, layers from 1 to \ jp{jpk}-2can have a thickness smaller than388 With partial steps, layers from 1 to \texttt{jpk-2} can have a thickness smaller than 366 389 $e_{3t}(jk)$. 367 390 368 The model deepest layer (\ jp{jpk}-1) is allowed to have either a smaller or larger391 The model deepest layer (\texttt{jpk-1}) is allowed to have either a smaller or larger 369 392 thickness than $e_{3t}(jpk)$: the maximum thickness allowed is $2*e_{3t}(jpk - 1)$. 370 393 … … 383 406 \subsubsection[$S$-coordinate (\forcode{ln_sco})]{$S$-coordinate (\protect\np{ln_sco}{ln\_sco})} 384 407 \label{sec:DOMCFG_sco} 408 385 409 \begin{listing} 386 \nlst{namzgr_sco_domcfg}387 410 \caption{\forcode{&namzgr_sco_domcfg}} 388 411 \label{lst:namzgr_sco_domcfg} 412 \begin{forlines} 413 !----------------------------------------------------------------------- 414 &namzgr_sco ! s-coordinate or hybrid z-s-coordinate (default: OFF) 415 !----------------------------------------------------------------------- 416 ln_s_sh94 = .false. ! Song & Haidvogel 1994 hybrid S-sigma (T)| 417 ln_s_sf12 = .false. ! Siddorn & Furner 2012 hybrid S-z-sigma (T)| if both are false the NEMO tanh stretching is applied 418 ln_sigcrit = .false. ! use sigma coordinates below critical depth (T) or Z coordinates (F) for Siddorn & Furner stretch 419 ! stretching coefficients for all functions 420 rn_sbot_min = 10.0 ! minimum depth of s-bottom surface (>0) (m) 421 rn_sbot_max = 7000.0 ! maximum depth of s-bottom surface (= ocean depth) (>0) (m) 422 rn_hc = 150.0 ! critical depth for transition to stretched coordinates 423 !!!!!!! Envelop bathymetry 424 rn_rmax = 0.3 ! maximum cut-off r-value allowed (0<r_max<1) 425 !!!!!!! SH94 stretching coefficients (ln_s_sh94 = .true.) 426 rn_theta = 6.0 ! surface control parameter (0<=theta<=20) 427 rn_bb = 0.8 ! stretching with SH94 s-sigma 428 !!!!!!! SF12 stretching coefficient (ln_s_sf12 = .true.) 429 rn_alpha = 4.4 ! stretching with SF12 s-sigma 430 rn_efold = 0.0 ! efold length scale for transition to stretched coord 431 rn_zs = 1.0 ! depth of surface grid box 432 ! bottom cell depth (Zb) is a linear function of water depth Zb = H*a + b 433 rn_zb_a = 0.024 ! bathymetry scaling factor for calculating Zb 434 rn_zb_b = -0.2 ! offset for calculating Zb 435 !!!!!!!! Other stretching (not SH94 or SF12) [also uses rn_theta above] 436 rn_thetb = 1.0 ! bottom control parameter (0<=thetb<= 1) 437 / 438 \end{forlines} 389 439 \end{listing} 390 Options are defined in \nam{zgr_sco}{zgr\_sco} (\texttt{DOMAINcfg} only). 440 441 Options are defined in \forcode{&zgr_sco} (\texttt{DOMAINcfg} only). 391 442 In $s$-coordinate (\np[=.true.]{ln_sco}{ln\_sco}), the depth and thickness of the model levels are defined from 392 443 the product of a depth field and either a stretching function or its derivative, respectively: … … 530 581 This option is described in the Report by Levier \textit{et al.} (2007), available on the \NEMO\ web site. 531 582 583 \section{Ice shelf cavity definition} 584 \label{subsec:zgrisf} 585 586 If the under ice shelf seas are opened (\np{ln_isfcav}{ln\_isfcav}), the depth of the ice shelf/ocean interface has to be include in 587 the \textit{isfdraft\_meter} file (Netcdf format). This file need to include the \textit{isf\_draft} variable. 588 A positive value will mean ice shelf/ocean or ice shelf bedrock interface below the reference 0m ssh. 589 The exact shape of the ice shelf cavity (grounding line position and minimum thickness of the water column under an ice shelf, ...) can be specify in \nam{zgr_isf}{zgr\_isf}. 590 591 \begin{listing} 592 \caption{\forcode{&namzgr_isf}} 593 \label{lst:namzgr_isf} 594 \begin{forlines} 595 !----------------------------------------------------------------------- 596 &namzgr_isf ! isf cavity geometry definition (default: OFF) 597 !----------------------------------------------------------------------- 598 rn_isfdep_min = 10. ! minimum isf draft tickness (if lower, isf draft set to this value) 599 rn_glhw_min = 1.e-3 ! minimum water column thickness to define the grounding line 600 rn_isfhw_min = 10 ! minimum water column thickness in the cavity once the grounding line defined. 601 ln_isfchannel = .false. ! remove channel (based on 2d mask build from isfdraft-bathy) 602 ln_isfconnect = .false. ! force connection under the ice shelf (based on 2d mask build from isfdraft-bathy) 603 nn_kisfmax = 999 ! limiter in level on the previous condition. (if change larger than this number, get back to value before we enforce the connection) 604 rn_zisfmax = 7000. ! limiter in m on the previous condition. (if change larger than this number, get back to value before we enforce the connection) 605 ln_isfcheminey = .false. ! close cheminey 606 ln_isfsubgl = .false. ! remove subglacial lake created by the remapping process 607 rn_isfsubgllon = 0.0 ! longitude of the seed to determine the open ocean 608 rn_isfsubgllat = 0.0 ! latitude of the seed to determine the open ocean 609 / 610 \end{forlines} 611 \end{listing} 612 613 The options available to define the shape of the under ice shelf cavities are listed in \nam{zgr_isf}{zgr\_isf} (\texttt{DOMAINcfg} only, \autoref{lst:namzgr_isf}). 614 615 \subsection{Model ice shelf draft definition} 616 \label{subsec:zgrisf_isfd} 617 618 First of all, the tool make sure, the ice shelf draft ($h_{isf}$) is sensible and compatible with the bathymetry. 619 There are 3 compulsory steps to achieve this: 620 621 \begin{description} 622 \item{\np{rn_isfdep_min}{rn\_isfdep\_min}:} this is the minimum ice shelf draft. This is to make sure there is no ridiculous thin ice shelf. If \np{rn_isfdep_min}{rn\_isfdep\_min} is smaller than the surface level, \np{rn_isfdep_min}{rn\_isfdep\_min} is set to $e3t\_1d(1)$. 623 Where $h_{isf} < MAX(e3t\_1d(1),rn\_isfdep\_min)$, $h_{isf}$ is set to \np{rn_isfdep_min}{rn\_isfdep\_min}. 624 625 \item{\np{rn_glhw_min}{rn\_glhw\_min}:} This parameter is used to define the grounding line position. 626 Where the difference between the bathymetry and the ice shelf draft is smaller than \np{rn_glhw_min}{rn\_glhw\_min}, the cell are grounded (ie masked). 627 This step is needed to take into account possible small mismatch between ice shelf draft value and bathymetry value (sources are coming from different grid, different data processes, rounding error, ...). 628 629 \item{\np{rn_isfhw_min}{rn\_isfhw\_min}:} This parameter is the minimum water column thickness in the cavity. 630 Where the water column thickness is lower than \np{rn_isfhw_min}{rn\_isfhw\_min}, the ice shelf draft is adjusted to match this criterion. 631 If for any reason, this adjustement break the minimum ice shelf draft allowed (\np{rn_isfdep_min}{rn\_isfdep\_min}), the cell is masked. 632 \end{description} 633 634 Once all these adjustements are made, if the water column thickness contains one cell wide channels, these channels can be closed using \np{ln_isfchannel}{ln\_isfchannel}. 635 636 \subsection{Model top level definition} 637 After the definition of the ice shelf draft, the tool defines the top level. 638 The compulsory criterion is that the water column needs at least 2 wet cells in the water column at U- and V-points. 639 To do so, if there one cell wide water column, the tools adjust the ice shelf draft to fillful the requierement.\\ 640 641 The process is the following: 642 \begin{description} 643 \item{step 1:} The top level is defined in the same way as the bottom level is defined. 644 \item{step 2:} The isolated grid point in the bathymetry are filled (as it is done in a domain without ice shelf) 645 \item{step 3:} The tools make sure, the top level is above or equal to the bottom level 646 \item{step 4:} If the water column at a U- or V- point is one wet cell wide, the ice shelf draft is adjusted. So the actual top cell become fully open and the new 647 top cell thickness is set to the minimum cell thickness allowed (following the same logic as for the bottom partial cell). This step is iterated 4 times to ensure the condition is fullfill along the 4 sides of the cell. 648 \end{description} 649 650 In case of steep slope and shallow water column, it likely that 2 cells are disconnected (bathymetry above its neigbourging ice shelf draft). 651 The option \np{ln_isfconnect}{ln\_isfconnect} allow the tool to force the connection between these 2 cells. 652 Some limiters in meter or levels on the digging allowed by the tool are available (respectively, \np{rn_zisfmax}{rn\_zisfmax} or \np{rn_kisfmax}{rn\_kisfmax}). 653 This will prevent the formation of subglacial lakes at the expense of long vertical pipe to connect cells at very different levels. 654 655 \subsection{Subglacial lakes} 656 Despite careful setting of your ice shelf draft and bathymetry input file as well as setting described in \autoref{subsec:zgrisf_isfd}, some situation are unavoidable. 657 For exemple if you setup your ice shelf draft and bathymetry to do ocean/ice sheet coupling, 658 you may decide to fill the whole antarctic with a bathymetry and an ice shelf draft value (ice/bedrock interface depth when grounded). 659 If you do so, the subglacial lakes will show up (Vostock for example). An other possibility is with coarse vertical resolution, some ice shelves could be cut in 2 parts: 660 one connected to the main ocean and an other one closed which can be considered as a subglacial sea be the model.\\ 661 662 The namelist option \np{ln_isfsubgl}{ln\_isfsubgl} allow you to remove theses subglacial lakes. 663 This may be useful for esthetical reason or for stability reasons: 664 665 \begin{description} 666 \item $\bullet$ In a subglacial lakes, in case of very weak circulation (often the case), the only heat flux is the conductive heat flux through the ice sheet. 667 This will lead to constant freezing until water reaches -20C. 668 This is one of the defitiency of the 3 equation melt formulation (for details on this formulation, see: \autoref{sec:isf}). 669 \item $\bullet$ In case of coupling with an ice sheet model, 670 the ssh in the subglacial lakes and the main ocean could be very different (ssh initial adjustement for example), 671 and so if for any reason both a connected at some point, the model is likely to fall over.\\ 672 \end{description} 673 674 \section{Closed sea definition} 675 \label{sec:clocfg} 676 677 \begin{listing} 678 \caption{\forcode{&namclo}} 679 \label{lst:namdom_clo} 680 \begin{forlines} 681 !----------------------------------------------------------------------- 682 &namclo ! (closed sea : need ln_domclo = .true. in namcfg) 683 !----------------------------------------------------------------------- 684 rn_lon_opnsea = -2.0 ! longitude seed of open ocean 685 rn_lat_opnsea = -2.0 ! latitude seed of open ocean 686 nn_closea = 8 ! number of closed seas ( = 0; only the open_sea mask will be computed) 687 ! name ! lon_src ! lat_src ! lon_trg ! lat_trg ! river mouth area ! net evap/precip correction scheme ! radius tgt ! id trg 688 ! ! (degree)! (degree)! (degree)! (degree)! local/coast/global ! (glo/rnf/emp) ! (m) ! 689 ! North American lakes 690 sn_lake(1) = 'superior' , -86.57 , 47.30 , -66.49 , 50.45 , 'local' , 'rnf' , 550000.0 , 2 691 sn_lake(2) = 'michigan' , -87.06 , 42.74 , -66.49 , 50.45 , 'local' , 'rnf' , 550000.0 , 2 692 sn_lake(3) = 'huron' , -82.51 , 44.74 , -66.49 , 50.45 , 'local' , 'rnf' , 550000.0 , 2 693 sn_lake(4) = 'erie' , -81.13 , 42.25 , -66.49 , 50.45 , 'local' , 'rnf' , 550000.0 , 2 694 sn_lake(5) = 'ontario' , -77.72 , 43.62 , -66.49 , 50.45 , 'local' , 'rnf' , 550000.0 , 2 695 ! African Lake 696 sn_lake(6) = 'victoria' , 32.93 , -1.08 , 30.44 , 31.37 , 'coast' , 'emp' , 100000.0 , 3 697 ! Asian Lakes 698 sn_lake(7) = 'caspian' , 50.0 , 44.0 , 0.0 , 0.0 , 'global' , 'glo' , 0.0 , 1 699 sn_lake(8) = 'aral' , 60.0 , 45.0 , 0.0 , 0.0 , 'global' , 'glo' , 0.0 , 1 700 / 701 \end{forlines} 702 \end{listing} 703 704 The options available to define the closed seas and how closed sea net fresh water input will be redistributed by NEMO are listed in \nam{dom_clo}{dom\_clo} (\texttt{DOMAINcfg} only). 705 The individual definition of each closed sea is managed by \np{sn_lake}{sn\_lake}. In this fields the user needs to define:\\ 706 \begin{description} 707 \item $\bullet$ the name of the closed sea (print output purposes). 708 \item $\bullet$ the seed location to define the area of the closed sea (if seed on land because not present in this configuration, this closed sea will be ignored).\\ 709 \item $\bullet$ the seed location for the target area. 710 \item $\bullet$ the type of target area ('local','coast' or 'global'). See point 6 for definition of these cases. 711 \item $\bullet$ the type of redistribution scheme for the net fresh water flux over the closed sea (as a runoff in a target area, as emp in a target area, as emp globally). For the runoff case, if the net fwf is negative, it will be redistribut globally. 712 \item $\bullet$ the radius of the target area (not used for the 'global' case). So the target defined by a 'local' target area of a radius of 100km, for example, correspond to all the wet points within this radius. The coastal case will return only the coastal point within the specifid radius. 713 \item $\bullet$ the target id. This target id is used to group multiple lakes into the same river ouflow (Great Lakes for example). 714 \end{description} 715 716 The closed sea module defines a number of masks in the \textit{domain\_cfg} output: 717 \begin{description} 718 \item[\textit{mask\_opensea}:] a mask of the main ocean without all the closed seas closed. This mask is defined by a flood filling algorithm with an initial seed (localisation defined by \np{rn_lon_opnsea}{rn\_lon\_opnsea} and \np{rn_lat_opnsea}{rn\_lat\_opnsea}). 719 \item[\textit{mask\_csglo}, \textit{mask\_csrnf}, \textit{mask\_csemp}:] a mask of all the closed seas defined in the namelist by \np{sn_lake}{sn\_lake} for each redistribution scheme. The total number of defined closed seas has to be defined in \np{nn_closea}{nn\_closea}. 720 \item[\textit{mask\_csgrpglo}, \textit{mask\_csgrprnf}, \textit{mask\_csgrpemp}:] a mask of all the closed seas and targets grouped by target id for each type of redistribution scheme. 721 \item[\textit{mask\_csundef}:] a mask of all the closed sea not defined in \np{sn_lake}{sn\_lake}. This will allows NEMO to mask them if needed or to inform the user of potential minor issues in its bathymetry. 722 \end{description} 723 532 724 \subinc{\input{../../global/epilogue}} 533 725
Note: See TracChangeset
for help on using the changeset viewer.