[10186] | 1 | ===================== |
---|
| 2 | Build a configuration |
---|
| 3 | ===================== |
---|
| 4 | |
---|
| 5 | .. contents:: |
---|
| 6 | :local: |
---|
| 7 | :depth: 1 |
---|
| 8 | |
---|
| 9 | .. role:: underline |
---|
| 10 | :class: underline |
---|
| 11 | |
---|
| 12 | Official configurations |
---|
| 13 | ======================= |
---|
| 14 | |
---|
| 15 | | NEMO is distributed with some reference configurations allowing both the user to set up a first application and |
---|
| 16 | the developer to validate their developments. |
---|
| 17 | | :underline:`The NEMO System Team is in charge of these configurations`. |
---|
| 18 | |
---|
| 19 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 20 | | | OPA | SI3 | TOP | PISCES | AGRIF | Inputs | |
---|
| 21 | +======================+=====+=====+=====+========+=======+===============================+ |
---|
| 22 | | `AGRIF_DEMO`_ | X | X | | | X | - `AGRIF_DEMO_v4.0.tar`_ | |
---|
| 23 | | | | | | | | - `ORCA2_ICE_v4.0.tar`_ | |
---|
| 24 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 25 | | `AMM12`_ | X | | | | | `AMM12_v4.0.tar`_ | |
---|
| 26 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 27 | | `C1D_PAPA`_ | X | | | | | `INPUTS_C1D_PAPA_v4.0.tar`_ | |
---|
| 28 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 29 | | `GYRE_BFM`_ | X | | X | | | ``-`` | |
---|
| 30 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 31 | | `GYRE_PISCES`_ | X | | X | X | | ``-`` | |
---|
| 32 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 33 | | `ORCA2_ICE_PISCES`_ | X | X | X | X | | - `ORCA2_ICE_v4.0.tar`_ | |
---|
| 34 | | | | | | | | - `INPUTS_PISCES_v4.0.tar`_ | |
---|
| 35 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 36 | | `ORCA2_OFF_PISCES`_ | | | X | X | | - `INPUTS_PISCES_v4.0.tar`_ | |
---|
| 37 | | | | | | | | - `ORCA2_OFF_v4.0.tar`_ | |
---|
| 38 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 39 | | `ORCA2_OFF_TRC`_ | | | X | | | `ORCA2_OFF_v4.0.tar`_ | |
---|
| 40 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 41 | | `ORCA2_SAS_ICE`_ | | X | | | | - `ORCA2_ICE_v4.0.tar`_ | |
---|
| 42 | | | | | | | | - `INPUTS_SAS_v4.0.tar`_ | |
---|
| 43 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 44 | | `SPITZ12`_ | X | X | | | | `SPITZ12_v4.0.tar`_ | |
---|
| 45 | +----------------------+-----+-----+-----+--------+-------+-------------------------------+ |
---|
| 46 | |
---|
| 47 | ---------- |
---|
| 48 | AGRIF_DEMO |
---|
| 49 | ---------- |
---|
| 50 | |
---|
| 51 | .. image:: _static/AGRIF_DEMO.jpg |
---|
| 52 | |
---|
| 53 | ``AGRIF_DEMO`` is based on the ``ORCA2_LIM3_PISCES`` global 2° configuration but |
---|
| 54 | it includes 3 online nested grids that demonstrate the overall capabilities of AGRIF in a realistic context, |
---|
| 55 | including nesting sea ice models. |
---|
| 56 | |
---|
| 57 | The configuration includes a 1:1 grid in the Pacific and two successively nested grids with odd and |
---|
| 58 | even refinement ratios over the Arctic ocean. |
---|
| 59 | The finest grid spanning the whole Svalbard archipelago is of particular interest to check that |
---|
| 60 | sea ice coupling is done properly. |
---|
| 61 | The 1:1 grid, used alone, is used as a benchmark to check that the solution is not corrupted by grid exchanges. |
---|
| 62 | |
---|
| 63 | Note that since grids interact only at the baroclinic time level, |
---|
| 64 | numerically exact results can not be achieved in the 1:1 case. |
---|
| 65 | One has to switch to a fully explicit in place of a split explicit free surface scheme in order to |
---|
| 66 | retrieve perfect reproducibility. |
---|
| 67 | |
---|
| 68 | Corresponding ``AGRIF_FixedGrids.in`` file is given by:: |
---|
| 69 | |
---|
| 70 | 2 |
---|
| 71 | 42 82 49 91 1 1 1 |
---|
| 72 | 122 153 110 143 4 4 4 |
---|
| 73 | 0 |
---|
| 74 | 1 |
---|
| 75 | 38 80 71 111 3 3 3 |
---|
| 76 | 0 |
---|
| 77 | |
---|
| 78 | ----- |
---|
| 79 | AMM12 |
---|
| 80 | ----- |
---|
| 81 | |
---|
| 82 | ``AMM12`` for *Atlantic Margin Model 12kms* is a `regional model`_ covering the Northwest European Shelf domain on |
---|
| 83 | a regular lat-lon grid at approximately 12km horizontal resolution. |
---|
| 84 | The key ``key_amm_12km`` is used to create the correct dimensions of the AMM domain. |
---|
| 85 | |
---|
| 86 | | This configuration tests several features of NEMO functionality specific to the shelf seas. |
---|
| 87 | | In particular, the AMM uses s-coordinates in the vertical rather than z-coordinates and is forced with |
---|
| 88 | tidal lateral boundary conditions using a flather boundary condition from the BDY module (``key_bdy``). |
---|
| 89 | |
---|
| 90 | The AMM configuration uses the GLS (``key_zdfgls``) turbulence scheme, |
---|
| 91 | the VVL non-linear free surface (``key_vvl``) and time-splitting (``key_dynspg_ts``). |
---|
| 92 | |
---|
| 93 | In addition to the tidal boundary condition, the model may also take open boundary conditions from |
---|
| 94 | a North Atlantic model. |
---|
| 95 | Boundaries may be completely ommited by removing the BDY key (key_bdy) in ``./cfgs/AMM12/cpp_AMM12_fcm``. |
---|
| 96 | |
---|
| 97 | Sample surface fluxes, river forcing and a sample initial restart file are included to test a realistic model run. |
---|
| 98 | The Baltic boundary is included within the river input file and is specified as a river source. |
---|
| 99 | Unlike ordinary river points the Baltic inputs also include salinity and temperature data. |
---|
| 100 | |
---|
| 101 | -------- |
---|
| 102 | C1D_PAPA |
---|
| 103 | -------- |
---|
| 104 | |
---|
| 105 | ``C1D_PAPA`` is a 1D configuration (one water column called NEMO1D, activated with CPP key ``key_c1d``), |
---|
| 106 | located at the `PAPA station 145W-50N <http://www.pmel.noaa.gov/OCS/Papa/index-Papa.shtml>`_. |
---|
| 107 | |
---|
| 108 | | NEMO1D is useful to test vertical physics in NEMO |
---|
| 109 | (turbulent closure scheme, solar penetration, interaction ocean/atmosphere.,...) |
---|
| 110 | | Size of the horizontal domain is 3x3 grid points. |
---|
| 111 | |
---|
| 112 | This reference configuration uses a 75 vertical levels grid (1m at the surface), |
---|
| 113 | the GLS (key_zdfgls) turbulence scheme with K-epsilon closure and the CORE BULK formulae. |
---|
| 114 | The atmospheric forcing comes from ECMWF operational analysis with a modification of the long and short waves flux. |
---|
| 115 | This set has been rescaled at a frequency of 1h. 1 year is simulated in outputs, |
---|
| 116 | see below (June,15 2010 to June,14 2011) |
---|
| 117 | |
---|
| 118 | `Reffray 2015`_ describes some tests on vertical physic using this configuration. |
---|
| 119 | |
---|
| 120 | The inputs tar file includes: |
---|
| 121 | |
---|
| 122 | - forcing files covering the years 2010 and 2011 (``forcing_PAPASTATION_1h_y201*.nc``) |
---|
| 123 | - initialization file for June,15 2010 deduced from observed data and Levitus 2009 climatology |
---|
| 124 | (``init_PAPASTATION_m06d15.nc``) |
---|
| 125 | - surface chlorophyll file (``chlorophyll_PAPASTATION.nc``) deduced from Seawifs data. |
---|
| 126 | |
---|
| 127 | -------- |
---|
| 128 | GYRE_BFM |
---|
| 129 | -------- |
---|
| 130 | |
---|
| 131 | ``GYRE_BFM`` is the same configuration as `GYRE_PISCES`_, except that PISCES is replaced by |
---|
| 132 | BFM biogeochemichal model in coupled mode. |
---|
| 133 | |
---|
| 134 | ----------- |
---|
| 135 | GYRE_PISCES |
---|
| 136 | ----------- |
---|
| 137 | |
---|
| 138 | | Idealized configuration representing double gyres in the North hemisphere, Beta-plane with |
---|
| 139 | a regular grid spacing at 1° horizontal resolution (and possible use as a benchmark by |
---|
| 140 | easily inscreasing grid size), 101 vertical levels, forced with analytical heat, freshwater and |
---|
| 141 | wind-stress fields. |
---|
| 142 | | This configuration is coupled to `PISCES biogeochemical model`_. |
---|
| 143 | |
---|
| 144 | Running GYRE as a benchmark |
---|
| 145 | --------------------------- |
---|
| 146 | |
---|
| 147 | This simple configuration can be used as a benchmark since it is easy to increase resolution |
---|
| 148 | (and in this case no physical meaning of outputs): |
---|
| 149 | |
---|
| 150 | 1. Choose the grid size |
---|
| 151 | |
---|
| 152 | In ``./cfgs/GYRE/EXP00``, edit your ``namelist_cfg`` file to change the ``jp_cfg``, ``jpi``, ``jpj``, |
---|
| 153 | ``jpk`` variables in &namcfg: |
---|
| 154 | |
---|
| 155 | +------------+---------+---------+---------+------------------+---------------+ |
---|
| 156 | | ``jp_cfg`` | ``jpi`` | ``jpj`` | ``jpk`` | Number of points | Equivalent to | |
---|
| 157 | +============+=========+=========+=========+==================+===============+ |
---|
| 158 | | 1 | 30 | 20 | 101 | 60600 | GYRE 1° | |
---|
| 159 | +------------+---------+---------+---------+------------------+---------------+ |
---|
| 160 | | 25 | 750 | 500 | 101 | 37875000 | ORCA 1/2° | |
---|
| 161 | +------------+---------+---------+---------+------------------+---------------+ |
---|
| 162 | | 50 | 1500 | 1000 | 101 | 151500000 | ORCA 1/4° | |
---|
| 163 | +------------+---------+---------+---------+------------------+---------------+ |
---|
| 164 | | 150 | 4500 | 3000 | 101 | 1363500000 | ORCA 1/12° | |
---|
| 165 | +------------+---------+---------+---------+------------------+---------------+ |
---|
| 166 | | 200 | 6000 | 4000 | 101 | 2424000000 | ORCA 1/16° | |
---|
| 167 | +------------+---------+---------+---------+------------------+---------------+ |
---|
| 168 | |
---|
| 169 | 2. In `namelist_cfg` again, avoid problems in the physics (and results will not be meaningful in terms of physics) by setting `nn_bench = 1` in &namctl |
---|
| 170 | |
---|
| 171 | .. code-block:: fortran |
---|
| 172 | |
---|
| 173 | nn_bench = 1 ! Bench mode (1/0): CAUTION use zero except for bench |
---|
| 174 | |
---|
| 175 | 3. If you increase domain size, you may need to decrease time-step (for stability) by changing `rn_rdt` value in &namdom (i.e. for `jp_cfg = 150`, ORCA12 equivalent, use `rn_rdt = 1200`) |
---|
| 176 | |
---|
| 177 | .. code-block:: fortran |
---|
| 178 | |
---|
| 179 | rn_rdt = 1200. ! time step for the dynamics |
---|
| 180 | |
---|
| 181 | 4. Optional, in order to increase the number of MPI communication for benchmark purposes: |
---|
| 182 | you can change the number of sub-timesteps computed in the time-splitting scheme each iteration. |
---|
| 183 | First change the list of active CPP keys for your experiment, |
---|
| 184 | in `cfgs/"your configuration name"/cpp_"your configuration name".fcm`: |
---|
| 185 | replace ``key_dynspg_flt by key_dynspg_ts`` and recompile/create your executable again |
---|
| 186 | |
---|
| 187 | .. code-block:: fortran |
---|
| 188 | |
---|
| 189 | makenemo [...] add_key 'key_dynspg_ts' del_key 'key_dynspg_flt' |
---|
| 190 | |
---|
| 191 | In your ``namelist_cfg`` file, edit the &namsplit namelist by adding the following line: |
---|
| 192 | |
---|
| 193 | .. code-block:: fortran |
---|
| 194 | |
---|
| 195 | nn_baro = 30 ! Number of iterations of barotropic mode/ |
---|
| 196 | |
---|
| 197 | ``nn_baro = 30`` is a kind of minimum (we usually use 30 to 60). |
---|
| 198 | So than increasing the ``nn_baro`` value will increase the number of MPI communications. |
---|
| 199 | |
---|
| 200 | The GYRE CPP keys, namelists and scripts can be explored in the ``GYRE`` configuration directory |
---|
| 201 | (``./cfgs/GYRE`` and ``./cfgs/GYRE/EXP00``). |
---|
| 202 | |
---|
| 203 | Find `here <http://prodn.idris.fr/thredds/catalog/ipsl_public/reee451/NEMO_OUT/GYRE/catalog.html>`_ |
---|
| 204 | monthly mean outputs of 1 year run |
---|
| 205 | |
---|
| 206 | ---------------- |
---|
| 207 | ORCA2_ICE_PISCES |
---|
| 208 | ---------------- |
---|
| 209 | |
---|
| 210 | ORCA is the generic name given to global ocean configurations. |
---|
| 211 | Its specificity lies on the horizontal curvilinear mesh used to overcome the North Pole singularity found for |
---|
| 212 | geographical meshes. |
---|
| 213 | SI3 (Sea Ice Integrated Initiative) is a thermodynamic-dynamic sea ice model specifically designed for |
---|
| 214 | climate studies. |
---|
| 215 | A brief description of the model is given here. |
---|
| 216 | |
---|
| 217 | :underline:`Space-time domain` |
---|
| 218 | |
---|
| 219 | The horizontal resolution available through the standard configuration is ORCA2. |
---|
| 220 | It is based on a 2 degrees Mercator mesh, (i.e. variation of meridian scale factor as cosinus of the latitude). |
---|
| 221 | In the northern hemisphere the mesh has two poles so that the ratio of anisotropy is nearly one everywhere. |
---|
| 222 | The mean grid spacing is about 2/3 of the nominal value: for example it is 1.3 degrees for ORCA2. |
---|
| 223 | Other resolutions (ORCA4, ORCA05 and ORCA025) are running or under development within specific projects. |
---|
| 224 | In the coarse resolution version (i.e. ORCA2 and ORCA4) the meridional grid spacing is increased near |
---|
| 225 | the equator to improve the equatorial dynamics. |
---|
| 226 | Figures in pdf format of mesh and bathymetry can be found and downloaded here. |
---|
| 227 | The sea-ice model runs on the same grid. |
---|
| 228 | |
---|
| 229 | The vertical domain spreads from the surface to a depth of 5000m. |
---|
| 230 | There are 31 levels, with 10 levels in the top 100m. |
---|
| 231 | The vertical mesh is deduced from a mathematical function of z ([[AttachmentNum(1)]]). |
---|
| 232 | The ocean surface corresponds to the w-level k=1, and the ocean bottom to the w-level k=31. |
---|
| 233 | The last T-level (k=31) is thus always in the ground.The depths of the vertical levels and |
---|
| 234 | the associated scale factors can be viewed. |
---|
| 235 | Higher vertical resolution is used in ORCA025 and ORCA12 (see `DRAKKAR project <http://www.drakkar-ocean.eu>`_). |
---|
| 236 | |
---|
| 237 | The time step depends on the resolution. It is 1h36' for ORCA2 so that there is 15 time steps in one day. |
---|
| 238 | |
---|
| 239 | :underline:`Ocean Physics (for ORCA2)` |
---|
| 240 | |
---|
| 241 | - horizontal diffusion on momentum: the eddy viscosity coefficient depends on the geographical position. |
---|
| 242 | It is taken as 40000 $m^2/s$, reduced in the equator regions (2000 $m^2/s$) excepted near the western boundaries. |
---|
| 243 | - isopycnal diffusion on tracers: the diffusion acts along the isopycnal surfaces (neutral surface) with |
---|
| 244 | a eddy diffusivity coefficient of 2000 $m^2/s$. |
---|
| 245 | - Eddy induced velocity parametrization with a coefficient that depends on the growth rate of |
---|
| 246 | baroclinic instabilities (it usually varies from 15 $m^2/s$ to 3000 $m^2/s$). |
---|
| 247 | - lateral boundary conditions : zero fluxes of heat and salt and no-slip conditions are applied through |
---|
| 248 | lateral solid boundaries. |
---|
| 249 | - bottom boundary condition : zero fluxes of heat and salt are applied through the ocean bottom. |
---|
| 250 | The Beckmann [19XX] simple bottom boundary layer parameterization is applied along continental slopes. |
---|
| 251 | A linear friction is applied on momentum. |
---|
| 252 | - convection: the vertical eddy viscosity and diffusivity coefficients are increased to 1 $m^2/s$ in case of |
---|
| 253 | static instability. |
---|
| 254 | - forcings: the ocean receives heat, freshwater, and momentum fluxes from the atmosphere and/or the sea-ice. |
---|
| 255 | The solar radiation penetrates the top meters of the ocean. |
---|
| 256 | The downward irradiance I(z) is formulated with two extinction coefficients [Paulson and Simpson, 1977], |
---|
| 257 | whose values correspond to a Type I water in Jerlov's classification (i.e the most transparent water) |
---|
| 258 | |
---|
| 259 | ORCA2_ICE_PISCES is a reference configuration with the following characteristics: |
---|
| 260 | |
---|
| 261 | - global ocean configuration |
---|
| 262 | - based on a tri-polar ORCA grid, with a 2° horizontal resolution |
---|
| 263 | - 31 vertical levels |
---|
| 264 | - forced with climatological surface fields |
---|
| 265 | - coupled to the sea-ice model SI3. |
---|
| 266 | - coupled to TOP passive tracer transport module and `PISCES biogeochemical model`_. |
---|
| 267 | |
---|
| 268 | :underline:`AGRIF demonstrator` |
---|
| 269 | |
---|
| 270 | | From the ``ORCA2_ICE_PISCES`` configuration, a demonstrator using AGRIF nesting can be activated. |
---|
| 271 | It includes the global ``ORCA2_ICE_PISCES`` configuration and a nested grid in the Agulhas region. |
---|
| 272 | | To set up this configuration, after extracting NEMO: |
---|
| 273 | |
---|
| 274 | - Build your AGRIF configuration directory from ORCA2_ICE_PISCES, with the key_agrif CPP key activated: |
---|
| 275 | |
---|
| 276 | .. code-block:: console |
---|
| 277 | |
---|
| 278 | $ ./makenemo -r 'ORCA2_ICE_PISCES' -n 'AGRIF' add_key 'key_agrif' |
---|
| 279 | |
---|
| 280 | - Using the ``ORCA2_ICE_PISCES`` input files and namelist, AGRIF test configuration is ready to run |
---|
| 281 | |
---|
| 282 | :underline:`On-The-Fly Interpolation` |
---|
| 283 | |
---|
| 284 | | NEMO allows to use the interpolation on the fly option allowing to interpolate input data during the run. |
---|
| 285 | If you want to use this option you need files giving informations on weights, which have been created. |
---|
| 286 | | You can find |
---|
| 287 | `here <http://prodn.idris.fr/thredds/catalog/ipsl_public/reee512/ORCA2_ONTHEFLY/WEIGHTS/catalog.html>`_ |
---|
| 288 | 2 weights files `bil_weights` for scalar field (bilinear interpolation) and `bic_weights` for |
---|
| 289 | vector field (bicubic interpolation). |
---|
| 290 | | The data files used are `COREII forcing <http://data1.gdfl.noaa.gov/nomads/forms/mom4/COREv2>`_ extrapolated on |
---|
| 291 | continents, ready to be used for on the fly option: |
---|
| 292 | `COREII`_ forcing files extrapolated on continents |
---|
| 293 | |
---|
| 294 | ---------------- |
---|
| 295 | ORCA2_OFF_PISCES |
---|
| 296 | ---------------- |
---|
| 297 | |
---|
| 298 | ``ORCA2_OFF_PISCES`` uses the ORCA2 configuration in which the `PISCES biogeochemical model`_ has been activated in |
---|
| 299 | standalone using the dynamical fields that are pre calculated. |
---|
| 300 | |
---|
| 301 | See `ORCA2_ICE_PISCES`_ for general description of ORCA2. |
---|
| 302 | |
---|
| 303 | The input files for PISCES are needed, in addition the dynamical fields are used as input. |
---|
| 304 | They are coming from a 2000 years of an ORCA2_LIM climatological run using ERA40 atmospheric forcing. |
---|
| 305 | |
---|
| 306 | ------------- |
---|
| 307 | ORCA2_OFF_TRC |
---|
| 308 | ------------- |
---|
| 309 | |
---|
| 310 | ``ORCA2_OFF_TRC`` uses the ORCA2_LIM configuration in which the tracer passive transport module TOP has been |
---|
| 311 | activated in standalone using the dynamical fields that are pre calculated. |
---|
| 312 | |
---|
| 313 | See `ORCA2_ICE_PISCES`_ for general description of ORCA2. |
---|
| 314 | |
---|
| 315 | In ``namelist_top_cfg``, different passive tracers can be activated ( cfc11, cfc12, sf6, c14, age ) or my-trc, |
---|
| 316 | a user-defined tracer. |
---|
| 317 | |
---|
| 318 | The dynamical fields are used as input, they are coming from a 2000 years of an ORCA2_LIM climatological run using |
---|
| 319 | ERA40 atmospheric forcing. |
---|
| 320 | |
---|
| 321 | ------------- |
---|
| 322 | ORCA2_SAS_ICE |
---|
| 323 | ------------- |
---|
| 324 | |
---|
| 325 | ``ORCA2_SAS_ICE`` is a demonstrator of the SAS ( Stand-alone Surface module ) based on ORCA2_LIM configuration. |
---|
| 326 | |
---|
| 327 | The standalone surface module allows surface elements such as sea-ice, iceberg drift and surface fluxes to |
---|
| 328 | be run using prescribed model state fields. |
---|
| 329 | For example, it can be used to inter-compare different bulk formulae or adjust the parameters of |
---|
| 330 | a given bulk formula |
---|
| 331 | |
---|
| 332 | See `ORCA2_ICE_PISCES`_ for general description of ORCA2. |
---|
| 333 | |
---|
| 334 | Same input files as `ORCA2_ICE_PISCES`_ are needed plus fields from a previous ORCA2_LIM run. |
---|
| 335 | |
---|
| 336 | More informations on input and configuration files in `NEMO Reference manual`_. |
---|
| 337 | |
---|
| 338 | ------- |
---|
| 339 | SPITZ12 |
---|
| 340 | ------- |
---|
| 341 | |
---|
| 342 | ``SPITZ12`` |
---|
| 343 | |
---|
| 344 | Unsupported configurations |
---|
| 345 | ========================== |
---|
| 346 | |
---|
| 347 | Other configurations are developed and used by some projects with "NEMO inside", |
---|
| 348 | these projects are welcome to publicize it here: http://www.nemo-ocean.eu/projects/add-project |
---|
| 349 | |
---|
| 350 | :underline:`Obviously these "projects configurations" are not under the NEMO System Team's responsibility`. |
---|
| 351 | |
---|
| 352 | .. _regional model: http://www.tandfonline.com/doi/pdf/10.1080/1755876X.2012.11020128 |
---|
| 353 | .. _AMM12_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/AMM12_v4.0.tar |
---|
| 354 | .. _PISCES biogeochemical model: http://www.geosci-model-dev.net/8/2465/2015 |
---|
| 355 | .. _INPUTS_PISCES_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/INPUTS_PISCES_v4.0.tar |
---|
| 356 | .. _ORCA2_OFF_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/ORCA2_OFF_v4.0.tar |
---|
| 357 | .. _ORCA2_ICE_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/ORCA2_ICE_v4.0.tar |
---|
| 358 | .. _INPUTS_SAS_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/INPUTS_SAS_v4.0.tar |
---|
| 359 | .. _NEMO Reference manual: http://forge.ipsl.jussieu.fr/nemo/doxygen/index.html?doc=NEMO |
---|
| 360 | .. _INPUTS_C1D_PAPA_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/INPUTS_C1D_PAPA_v4.0.tar |
---|
| 361 | .. _Reffray 2015: http://www.geosci-model-dev.net/8/69/2015 |
---|
| 362 | .. _COREII: http://prodn.idris.fr/thredds/catalog/ipsl_public/reee512/ORCA2_ONTHEFLY/FILLED_FILES/catalog.html |
---|
| 363 | .. _SPITZ12_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/SPITZ12_v4.0.tar |
---|
| 364 | .. _AGRIF_DEMO_v4.0.tar: http://prodn.idris.fr/thredds/fileServer/ipsl_public/romr005/Online_forcing_archives/AGRIF_DEMO_v4.0.tar |
---|