| ACCESS-ESM |
The Australian Community Climate and Earth-System Simulator (ACCESS) is a coupled climate and earth system simulator to be developed as a joint initiative of the Bureau of Meteorology and CSIRO in cooperation with the university community in Australia.
http://climate-cms.wikis.unsw.edu.au/ACCESS-ESM_1.5 |
global |
|
[T4.5-3, T4.5-2, T4.4-2, T4.4-3] |
0 |
|
| AMM7 (NEMO) |
Atlantic Margin Model, 7 km resolution of the European shelf waters.
Terrain-following z-sigma coordinate.
300s time step. |
20W - 13W
40N - 65N |
NEMO v3.6 |
[EJK001, EJK002, EJK003] |
0 |
|
| ATLAS10 |
All-Atlantic nested configuration (1/10 degree nest within 0.5 degree global ocean) |
Global; Atlantic; Southern Ocean (Atlantic sector) |
ORCA05 |
[KTS016, KTS019, KTS021] |
0 |
|
| AWI-CM-REcoM |
REcoM - in its current standard set-up - carries 21 tracers, including dissolved inorganic carbon and alkalinity for the carbonate system, the macronutrients dissolved inorganic nitrogen (DIN) and silicic acid and the trace metal iron. REcoM2 has two phytoplankton classes, nanophytoplankton (with implicit representation of calcifiers) and diatoms. The intracellular stoichiometry of C:N:Si:Chl pools for diatoms and C:N:CaCO3:Chl pools for nanophytoplankton is allowed to respond dynamically to environmental conditions following Geider et al., 1998. The intracellular iron pool is a function of the intracellular nitrogen concentration (fixed Fe:N) as iron is physiologically linked to enzyme formation, especially the photosynthetic electron transport chain (Raven et al., 1988, Behrenfeld et al., 2013). Dead organic matter is transferred to detritus by aggregation and grazing by one zooplankton class and the sinking and advection of detritus is represented explicitly. |
global |
|
[T4.4-2, T4.5-1, T4.4-1, T4.4-3] |
0 |
|
| BSIOM |
Baltic Sea Ice-Ocean Model |
Baltic Sea |
|
[smhi-O2, era5, ERAinterim-WAVE-O2] |
0 |
|
| Bern3D-PISCES |
Biogeochemical Model |
global |
|
[_ctrl, o2, _ctrl, d2, delta1, _scen, d2, _ctrl, o4, _ctrl, o1, omega2, _ctrl, d4, _scen, o2, omega4, _scen, o4, _ctrl, d1, _scen, d4, _scen, d1, _scen, o1, delta2, omega1, delta4] |
0 |
|
| CROCO |
Coastal and Regional Ocean COmmunity model |
coastal area |
|
[ climatological calibration 2000-2008, BioEBUS, interannual 1990-2010] |
0 |
|
| EC-Earth |
EC-Earth - A European community Earth-System Model
http://www.ec-earth.org/ |
global |
|
[T4.5-3, T4.5-2, T4.5-1] |
0 |
|
| FOCI |
Flexible Ocean and Climate Infrastructure (FOCI) is a new Earth system model. |
global |
|
[TK201_FMESM_SSP126_alkEU_2014CC105, T4.3-2, CC101, NM001_FM_ESM_SSP370os_2014CC105, T4.3-3, 01, TK202_FMESM_SSP534os_alkEU_2014CC105, TM023, TS018, TM020, TM021, TM026, TM028, TS030, TS034, T4.3-1, TK200_FMESM_SSP370_alkEU_2014CC105, TM024] |
0 |
|
| IAM |
Integrated Assessment Model |
|
|
[1] |
0 |
|
| INALT20r |
INALT20r is the complementary configuration to INALT60 to analyse the impact of the higher resolution in the 2nd nest with INALT60.
The configurations INALT60 and INALT20r have been developed by Franziska U. Schwarzkopf and René Schubert in coordination with Arne Biastoch within three distinct phases: After the first phase, both configurations have been introduced as part of the INALT family in Schwarzkopf et al. (2019; https://doi.org/10.5194/gmd-12-3329-2019). Subsequently, in the second phase, the configurations have been further developed as described in Schubert et al. (2019; https://doi.org/10.1029/2019MS001724). Based on this development, a series of four parallel model experiments has been executed that formed the basis for the dissertation of René Schubert (https://nbn-resolving.org/urn:nbn:de:gbv:8-mods-2020-00151-7) and the publications Schubert et al. (2019, 2020 (https://doi.org/10.1175/JPO-D-19-0311.1), 2021(https://doi.org/10.1038/s43247-021-00271-y)). Finally, in a third phase, a series of longer parall |
global;
eastern South Atlantic Ocean;
western Indian Ocean;
Agulhas Region |
ORCA025 |
[KRS006, KRS001] |
0 |
|
| MOM-5 |
Modular Ocean Circulation Model |
|
|
[5] |
0 |
|
| MPIOM/HAMOCC |
HAMOCC is a sub-model that simulates biogeochemical tracers in the oceanic water column and in the sediment. www.mpimet.mpg.de/en/science/models/mpiom.html |
|
|
[Opt3, Seas-at, Opt2, Coast, Half, Ref, NDia, Equi, Opt1, Opt134, Opt24, Opt4, Dia] |
0 |
|
| NorESM |
Norwegian Earth System Model:
A climate model solves mathematically formulated natural laws on a three-dimensional grid. The climate model divides the soil system into components (atmosphere, sea, sea ice, land with vegetation, etc.) that interact through transmission of energy, motion and moisture. When the climate model also includes advanced interactive atmosphere chemistry and biogeochemical cycles (such as the carbon cycle), it is called an earth system model. |
global |
|
[T4.4-3, T4.2, T4.6-2, T4.5-1, T4.4-2, T4.6-1] |
0 |
|
| ORCA2 |
NEMOv3.6 ORCA2
NPZD biogeochemical model |
Global |
|
[PDOexperiments, SynopticVariability] |
0 |
|
| ORION12 |
nested OGCM (1/12 degree nest within 0.5 degree global ocean). |
|
ORCA05 |
[-] |
0 |
|
| ROMS-BioEBUS |
Regional Oceanic Modeling System (ROMS), Biogeochemical model for Eastern Boundary Upwelling Systems (BioEBUS) |
|
|
[BioEBUS, Sensitivity of zooplankton mortality (ref +/- 50 %))] |
0 |
|
| TRATL10 |
GCM |
|
ORCA05 |
[K003.hindcast, K004.hindcast, K001.spinup] |
0 |
|
| UVic-updates-opem |
Optimality-based plankton ecosystem model (OPEM) for the UVic-ESCM. OPEM includes optimality-based formulations for phytoplankton, diazotrophs, and zooplankton. Variable C:N:P stoichiometry is implemented for phytoplankton, diazotrophs, and detritus. It is mainly based on the version of Nickelsen et al. (2015) GMD. |
Global |
UVic ESCM-2.9 |
[H, default] |
1 |
|
| VIKING10 |
nested OGCM (1/10 degree Atlantic nest, 30-85N, within 0.5 degree global ocean) https://www.geomar.de/fb1-od/viking-family |
|
|
[KTM03p25, KTM03p26] |
0 |
|
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