| 1d AE model |
This model computes the additional CO2 uptake of the ocean after alkalinity enhancement (AE). Biogeochemical variables are taken from observational based data products and averaged over 4 regions for the time 1994-2019.
Model experiments are performed for the variation of the variables, for the case of reentrainment of alkalinity and CO2 into the mixed layer and for permanent and monthly AE. |
Region1:
55:W-45°W, 55°N-60°N
Region2:
60°W-50°W, 30°N-35°N
Region3:
20°W-10°W, 5°S-0°S
Region4:
40°W-30°W, 46.5°S-42.5°S |
|
[04, 03, 01, 01] |
0 |
|
| FESOM2.1, CORE mesh, REcoM3 |
The Finite VolumE Sea ice-Ocean Model (FESOM2.1) is a global ocean general circulaIon
model, coupled to the ocean biogeochemistry model Regulated Ecosystem Model version 3
(REcoM3). REcoM3 has 28 prognosIc tracers and the marine carbonate system along with
air-sea CO2 exchange is simulated using the mocsy rouInes. It represents two
phytoplankton classes and three zooplankton groups. REcoM3 resolves the cycling of the
macro nutrients dissolved inorganic nitrogen (DIN) and silicic acid (DSi) along with the trace
metal dissolved iron (DFe). The variable stoichiometric raIo represents the physiological
response of phytoplankton to changing environmental condiIons, such as light and nutrient
availability. The model simulaIons are carried out using the so-called CORE mesh with
126859 surface nodes. It has a resoluIon of ~20 km in the equatorial and polar regions and
a coarse resoluIon of ~75 km in the subtropical ocean basins. It has 47 unevenly spaced
verIcal levels, with thickness varying from 5 m at the surface to 250 m in the deep ocean.
Forcing: Output from AWI Climate Model (AWI-CM) contribuIon to CMIP6. The simulaIons
are forced with 3-hourly atmospheric momentum fluxes, freshwater fluxes, radiaIon and
daily output of terrestrial freshwater runoff from the first ensemble member of the historical
simulaIon unIl 2014 of the SSP1-2.6 or SSP3-7.0 from 2015 unIl 2100.
Code:
Via Github: hdps://github.com/tanvinagwekar/fesom2/tree/OAE_Experiments
Via Zenodo: hdps://zenodo.org/doi/10.5281/zenodo.10967051 |
global |
FESOM2.1-REcoM3 |
[5-NWS-ALK, 4-SO-ALK, 3-SUB-ALK, 6-NBS-ALK, 2-GLO-ALK, 09-SO-ALK-NUT, 07-GLO-ALK-NUT, 08-SUB-ALK-NUT, 1-CTRL] |
0 |
|
| FOCI-OpenIFS |
Atmosphere: OpenIFS
Ocean: NEMO
Land: HTESSEL
Sea ice: LIM2/SI3
Coupler: OASIS3-MCT |
Global |
FOCI |
[FOCI_GJK029, FOCI_GJK031_r1i1p1, FOCI_GJK032_r3i1p1, FOCI_GJK030_r1i1p1] |
0 |
|
| INALT20 |
nested OGCM (1/20 degree nest within 0.25 degree global ocean). |
global;
South Atlantic;
western Indian Ocean;
Atlantic sector of the Southern Ocean |
ORCA025 |
[-, KFS10X, KFS044, KFS119] |
0 |
|
| 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 parallel INALT20r experiments have been developed that has not yet been used for further publications. |
global;
Atlantic Ocean;
western Indian Ocean;
Southern Ocean;
Agulhas Region; |
ORCA025 |
[KFS004, KRS0020, KFS005, KFS006, KRS0005, KRS0002] |
0 |
|
| MITgcm-Darwin_ATL06_TROP |
Regional config for Tropical Atlantic (BGC) |
Lon [99.5°W - 28.7°E]
Lat [36.9°N - 30.5°S] |
MITgcm |
[] |
5 |
|
| MOMA |
Geophysical Fluid Dynamics Laboratory (GFDL) Modular Ocean Model
(MOM), version MOM4p1 (Griffies et al. 2009) [Griffies, S. M., and R. W. Hallberg, 2000: Biharmonic friction
with a Smagorinsky-Like viscosity for use in large-scale eddypermitting ocean models. Mon. Wea. Rev., 128, 2935–2946,
https://doi.org/10.1175/1520-0493(2000)128,2935:BFWASL.
2.0.CO;2.] |
The model domain covers most of the subtropical gyre
in the North Atlantic (15.5°–60°W, 6.25°–38.5°N). The boundaries are solid walls and there are no horizontal boundary
conditions such as restoring. |
regional model no nest |
[-] |
0 |
|
| OpenIFS |
An easy-to-use version of the ECMWF global IFS (Integrated Forecasting System), the OpenIFS model, is available to academic and research institutions.
The OpenIFS model provides the same forecast capability as IFS but without the data assimilation system. Supporting software and documentation is also provided.
OpenIFS has a support team at ECMWF for technical assistance but limited resources for detailed scientific assistance. |
Global model. |
IFS |
[OIFS_GAS_HighResMIP_NOAMV, OIFS_GJK029, OIFS_GAS_HighResMIP, OIFS-BAS003, OIFS_GAS_HighResMIP_NOIPV, OIFS-BAS001, OIFS_GAS_HighResMIP_NOIPV_NOAMV, OIFS-BAS002, OIFS-BAS004] |
0 |
|
| SP1D |
Process model for the performance prediction of Stommel Upwelling Pipes (SUP), which operate on the basis of the "Perpetual Salt Fountain" principle, described by Stommel et al. (1953) [ https://doi.org/10.1016/0146-6313(56)90095-8 ]. The model solves for a steady-state pressure and heat balance on a one-dimensional grid. A full description of the model is given in Kemper et al. (2023) [ http://dx.doi.org/10.23967/marine.2023.018 ] |
Process model |
|
[sup_potential_studies, sup_performance_studies, sup_performance_studies] |
0 |
|
| TMM-MOPS |
The coupled TMM - MOPS model framework, as available under:
https://doi.org/10.5281/zenodo.1246300 (Khatiwala, 2018)
|
|
|
[L4-SO, S6-All, S4-SO, S4-SO-PETSc3.6, S6-DOP, S6Star-All, S4-Org] |
0 |
|
| UVic2.9-MOBI |
The University of Victoria Earth System Climate Model of intermediate complexity with the Model of Ocean Biogeochemistry and Isotopes |
global |
|
[PreInd, Anthro_Hindcast_NoSuess, Anthro_Hindcast] |
0 |
|
| VIKING20X |
nested OGCM (1/20 degree Atlantic nest within 0.25 degree global ocean)
https://www.geomar.de/fb1-od/viking-family |
global;
Atlantic; |
ORCA025 |
[KFS003-4th, KFS001, KKG36107B, KKG36013H, KFS003-2nd, KFS003, KFS003-3rd, KKG36101H] |
0 |
|
| ocean4Foam |
Finite volume CFD modeling environment for engineering scale oceanic flow, based on the OpenFOAM environment. |
|
OpenFOAM |
[sup_performance_studies, turbulence_validation, wave_validation, sup_performance_studies, au_nutrient_re-sinking] |
0 |
|
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