Changeset 11123 for NEMO/trunk/doc/latex/NEMO/subfiles/introduction.tex
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- 2019-06-17T14:22:27+02:00 (5 years ago)
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- NEMO/trunk/doc/latex/NEMO/subfiles
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NEMO/trunk/doc/latex/NEMO/subfiles/introduction.tex
r10544 r11123 27 27 28 28 The ocean component of \NEMO has been developed from the legacy of the OPA model, release 8.2, 29 described in \citet{ Madec1998}.29 described in \citet{madec.delecluse.ea_NPM98}. 30 30 This model has been used for a wide range of applications, both regional or global, as a forced ocean model and 31 31 as a model coupled with the sea-ice and/or the atmosphere. … … 67 67 Within the \NEMO system the ocean model is interactively coupled with a sea ice model (SI$^3$) and 68 68 a biogeochemistry model (PISCES). 69 Interactive coupling to Atmospheric models is possible via the OASIS coupler \citep{OASIS2006}.69 Interactive coupling to Atmospheric models is possible via the \href{https://portal.enes.org/oasis}{OASIS coupler}. 70 70 Two-way nesting is also available through an interface to the AGRIF package 71 (Adaptative Grid Refinement in \fortran) \citep{ Debreu_al_CG2008}.71 (Adaptative Grid Refinement in \fortran) \citep{debreu.vouland.ea_CG08}. 72 72 % Needs to be reviewed 73 73 %The interface code for coupling to an alternative sea ice model (CICE, \citet{Hunke2008}) has now been upgraded so … … 83 83 The lateral Laplacian and biharmonic viscosity and diffusion can be rotated following 84 84 a geopotential or neutral direction. 85 There is an optional eddy induced velocity \citep{ Gent1990} with a space and time variable coefficient86 \citet{ Treguier1997}.85 There is an optional eddy induced velocity \citep{gent.mcwilliams_JPO90} with a space and time variable coefficient 86 \citet{treguier.held.ea_JPO97}. 87 87 The model has vertical harmonic viscosity and diffusion with a space and time variable coefficient, 88 with options to compute the coefficients with \citet{ Blanke1993}, \citet{Pacanowski_Philander_JPO81}, or89 \citet{ Umlauf_Burchard_JMS03} mixing schemes.88 with options to compute the coefficients with \citet{blanke.delecluse_JPO93}, \citet{pacanowski.philander_JPO81}, or 89 \citet{umlauf.burchard_JMR03} mixing schemes. 90 90 91 91 %%gm To be put somewhere else .... … … 213 213 NEMO/OPA, like all research tools, is in perpetual evolution. 214 214 The present document describes the OPA version include in the release 3.4 of NEMO. 215 This release differs significantly from version 8, documented in \citet{ Madec1998}. \\215 This release differs significantly from version 8, documented in \citet{madec.delecluse.ea_NPM98}. \\ 216 216 217 217 The main modifications from OPA v8 and NEMO/OPA v3.2 are : … … 222 222 \item 223 223 introduction of partial step representation of bottom topography 224 \citep{ Barnier_al_OD06, Le_Sommer_al_OM09, Penduff_al_OS07};224 \citep{barnier.madec.ea_OD06, le-sommer.penduff.ea_OM09, penduff.le-sommer.ea_OS07}; 225 225 \item 226 226 partial reactivation of a terrain-following vertical coordinate ($s$- and hybrid $s$-$z$) with … … 242 242 additional advection schemes for tracers; 243 243 \item 244 implementation of the AGRIF package (Adaptative Grid Refinement in \fortran) \citep{ Debreu_al_CG2008};244 implementation of the AGRIF package (Adaptative Grid Refinement in \fortran) \citep{debreu.vouland.ea_CG08}; 245 245 \item 246 246 online diagnostics : tracers trend in the mixed layer and vorticity balance; … … 255 255 RGB light penetration and optional use of ocean color 256 256 \item 257 major changes in the TKE schemes: it now includes a Langmuir cell parameterization \citep{ Axell_JGR02},258 the \citet{ Mellor_Blumberg_JPO04} surface wave breaking parameterization, and has a time discretization which259 is energetically consistent with the ocean model equations \citep{ Burchard_OM02, Marsaleix_al_OM08};257 major changes in the TKE schemes: it now includes a Langmuir cell parameterization \citep{axell_JGR02}, 258 the \citet{mellor.blumberg_JPO04} surface wave breaking parameterization, and has a time discretization which 259 is energetically consistent with the ocean model equations \citep{burchard_OM02, marsaleix.auclair.ea_OM08}; 260 260 \item 261 261 tidal mixing parametrisation (bottom intensification) + Indonesian specific tidal mixing 262 \citep{ Koch-Larrouy_al_GRL07};262 \citep{koch-larrouy.madec.ea_GRL07}; 263 263 \item 264 264 introduction of LIM-3, the new Louvain-la-Neuve sea-ice model 265 265 (C-grid rheology and new thermodynamics including bulk ice salinity) 266 \citep{ Vancoppenolle_al_OM09a, Vancoppenolle_al_OM09b}266 \citep{vancoppenolle.fichefet.ea_OM09*a, vancoppenolle.fichefet.ea_OM09*b} 267 267 \end{itemize} 268 268 … … 272 272 \item 273 273 introduction of a modified leapfrog-Asselin filter time stepping scheme 274 \citep{ Leclair_Madec_OM09};275 \item 276 additional scheme for iso-neutral mixing \citep{ Griffies_al_JPO98}, although it is still a "work in progress";277 \item 278 a rewriting of the bottom boundary layer scheme, following \citet{ Campin_Goosse_Tel99};279 \item 280 addition of a Generic Length Scale vertical mixing scheme, following \citet{ Umlauf_Burchard_JMS03};274 \citep{leclair.madec_OM09}; 275 \item 276 additional scheme for iso-neutral mixing \citep{griffies.gnanadesikan.ea_JPO98}, although it is still a "work in progress"; 277 \item 278 a rewriting of the bottom boundary layer scheme, following \citet{campin.goosse_T99}; 279 \item 280 addition of a Generic Length Scale vertical mixing scheme, following \citet{umlauf.burchard_JMR03}; 281 281 \item 282 282 addition of the atmospheric pressure as an external forcing on both ocean and sea-ice dynamics; 283 283 \item 284 addition of a diurnal cycle on solar radiation \citep{ Bernie_al_CD07};284 addition of a diurnal cycle on solar radiation \citep{bernie.guilyardi.ea_CD07}; 285 285 \item 286 286 river runoffs added through a non-zero depth, and having its own temperature and salinity; … … 296 296 coupling interface adjusted for WRF atmospheric model; 297 297 \item 298 C-grid ice rheology now available fro both LIM-2 and LIM-3 \citep{ Bouillon_al_OM09};298 C-grid ice rheology now available fro both LIM-2 and LIM-3 \citep{bouillon.maqueda.ea_OM09}; 299 299 \item 300 300 LIM-3 ice-ocean momentum coupling applied to LIM-2; … … 318 318 319 319 \begin{itemize} 320 \item finalisation of above iso-neutral mixing \citep{ Griffies_al_JPO98}";320 \item finalisation of above iso-neutral mixing \citep{griffies.gnanadesikan.ea_JPO98}"; 321 321 \item "Neptune effect" parametrisation; 322 322 \item horizontal pressure gradient suitable for s-coordinate;
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