Published August 28, 2019
| Version v1
Journal article
Open
The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features
Creators
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Adcroft, Alistair1
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Anderson, Whit2
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Balaji, V.1
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Blanton, Chris2
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Bushuk, Mitchell2
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Dufour, Carolina O.3
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Dunne, John P.2
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Griffies, Stephen M.1
- Hallberg, Robert1
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Harrison, Matthew J.2
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Held, Isaac M.1
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Jansen, Malte F.4
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John, Jasmin G.2
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Krasting, John P.2
- Langenhorst, Amy R.2
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Legg, Sonya1
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Liang, Zhi2
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McHugh, Colleen2
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Radhakrishnan, Aparna5
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Reichl, Brandon G.2
- Rosati, Tony2
- Samuels, Bonita L.2
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Shao, Andrew6
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Stouffer, Ronald2
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Winton, Michael2
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Wittenberg, Andrew T.2
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Xiang, Baoqiang2
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Zadeh, Niki2
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Zhang, Rong1
- 1. Princeton University
- 2. NOAA/GFDL
- 3. McGill University
- 4. University of Chicago
- 5. SAIC/GFDL
- 6. University of Victoria
Description
We document the configuration and emergent simulation features from the Geophysical Fluid Dynamics Laboratory (GFDL) OM4.0 ocean/sea ice model. OM4 serves as the ocean/sea ice component for the GFDL climate and Earth system models. It is also used for climate science research and is contributing to the Coupled Model Intercomparison Project version 6 Ocean Model Intercomparison Project. The ocean component of OM4 uses version 6 of the Modular Ocean Model and the sea ice component uses version 2 of the Sea Ice Simulator, which have identical horizontal grid layouts (Arakawa C-grid). We follow the Coordinated Ocean-sea ice Reference Experiments protocol to assess simulation quality across a broad suite of climate-relevant features. We present results from two versions differing by horizontal grid spacing and physical parameterizations: OM4p5 has nominal 0.5° spacing and includes mesoscale eddy parameterizations and OM4p25 has nominal 0.25° spacing with no mesoscale eddy parameterization. Modular Ocean Model version 6 makes use of a vertical Lagrangian-remap algorithm that enables general vertical coordinates. We show that use of a hybrid depth-isopycnal coordinate reduces the middepth ocean warming drift commonly found in pure z* vertical coordinate ocean models. To test the need for the mesoscale eddy parameterization used in OM4p5, we examine the results from a simulation that removes the eddy parameterization. The water mass structure and model drift are physically degraded relative to OM4p5, thus supporting the key role for a mesoscale closure at this resolution.
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J Adv Model Earth Syst - 2019 - Adcroft - The GFDL Global Ocean and Sea Ice Model OM4 0 Model Description and Simulation.pdf
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Additional details
Identifiers
- DOI
- 10.1029/2019MS001726
- Other
- oai:uchicago.tind.io:14157
Funding
- National Oceanic and Atmospheric Administration
- NA14OAR4320106
- Natural Sciences and Engineering Research Council of Canada
- RGPIN-2018-04985
- National Science Foundation
- 1536350