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

  • Alistair Adcroft
  • , Whit Anderson
  • , V. Balaji
  • , Chris Blanton
  • , Mitchell Bushuk
  • , Carolina O. Dufour
  • , John P. Dunne
  • , Stephen M. Griffies
  • , Robert Hallberg
  • , Matthew J. Harrison
  • , Isaac M. Held
  • , Malte F. Jansen
  • , Jasmin G. John
  • , John P. Krasting
  • , Amy R. Langenhorst
  • , Sonya Legg
  • , Zhi Liang
  • , Colleen McHugh
  • , Aparna Radhakrishnan
  • , Brandon G. Reichl
  • Tony Rosati, Bonita L. Samuels, Andrew Shao, Ronald Stouffer, Michael Winton, Andrew T. Wittenberg, Baoqiang Xiang, Niki Zadeh, Rong Zhang

Research output: Contribution to journalArticlepeer-review

358 Scopus citations

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° 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.

Original languageEnglish
Pages (from-to)3167-3211
Number of pages45
JournalJournal of Advances in Modeling Earth Systems
Volume11
Issue number10
DOIs
StatePublished - Oct 1 2019
Externally publishedYes

Keywords

  • CORE
  • hybrid coordinates
  • ocean circulation model

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