4.6 Article

The GFDL Global Ocean and Sea Ice Model OM4.0: Model Description and Simulation Features

期刊

JOURNAL OF ADVANCES IN MODELING EARTH SYSTEMS
卷 11, 期 10, 页码 3167-3211

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1029/2019MS001726

关键词

ocean circulation model; CORE; hybrid coordinates

资金

  1. National Oceanic and Atmospheric Administration, U.S. Department of Commerce [NA14OAR4320106]
  2. Carbon Mitigation Initiative (CMI) project at Princeton University - BP
  3. Natural Sciences and Engineering Research Council of Canada (NSERC) [RGPIN-2018-04985]
  4. National Science Foundation [1536350]

向作者/读者索取更多资源

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.

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