The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features
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Adcroft, AlistairAnderson, Whit
Balaji, V.
Blanton, Chris
Bushuk, Mitchell
Dufour, Carolina O.

Dunne, John P.
Griffies, Stephen M.

Hallberg, Robert
Harrison, Matthew J.
Held, Isaac M.
Jansen, Malte F.
John, Jasmin G.
Krasting, John P.
Langenhorst, Amy R.
Legg, Sonya
Liang, Zhi
McHugh, Colleen
Radhakrishnan, Aparna
Reichl, Brandon G.
Rosati, Tony
Samuels, Bonita L.
Shao, Andrew
Stouffer, Ronald
Winton, Michael

Wittenberg, Andrew T.
Xiang, Baoqiang
Zadeh, Niki
Zhang, Rong
Affiliation
Univ Arizona, Dept GeosciIssue Date
2019-10-18
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AMER GEOPHYSICAL UNIONCitation
Adcroft, A., Anderson, W., Balaji, V., Blanton, C., Bushuk, M., Dufour, C. O., et al. (2019). The GFDL global ocean and sea ice model OM4.0: Model description and simulation features. Journal of Advances in Modeling Earth Systems, 11. https://doi.org/10.1029/ 2019MS001726Rights
Copyright © 2019. The Authors. This is an open access article under the terms of the Creative Commons Attribution License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
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 degrees spacing and includes mesoscale eddy parameterizations and OM4p25 has nominal 0.25 degrees 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.Note
Open access journalISSN
1942-2466Version
Final published versionSponsors
National Oceanic and Atmospheric Administration, U.S. Department of CommerceNational Oceanic Atmospheric Admin (NOAA) - USA [NA14OAR4320106]; Carbon Mitigation Initiative (CMI) project at Princeton University - BP; Natural Sciences and Engineering Research Council of Canada (NSERC)Natural Sciences and Engineering Research Council of Canada [RGPIN-2018-04985]; National Science FoundationNational Science Foundation (NSF) [1536350]ae974a485f413a2113503eed53cd6c53
10.1029/2019ms001726
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Except where otherwise noted, this item's license is described as Copyright © 2019. The Authors. This is an open access article under the terms of the Creative Commons Attribution License.