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

被引:227
|
作者
Adcroft, Alistair [1 ,2 ]
Anderson, Whit [2 ]
Balaji, V. [1 ,2 ]
Blanton, Chris [2 ,3 ]
Bushuk, Mitchell [2 ]
Dufour, Carolina O. [4 ]
Dunne, John P. [2 ]
Griffies, Stephen M. [1 ,2 ]
Hallberg, Robert [1 ,2 ]
Harrison, Matthew J. [2 ]
Held, Isaac M. [1 ,2 ]
Jansen, Malte F. [5 ]
John, Jasmin G. [2 ]
Krasting, John P. [2 ]
Langenhorst, Amy R. [2 ]
Legg, Sonya [1 ,2 ]
Liang, Zhi [2 ]
McHugh, Colleen [2 ]
Radhakrishnan, Aparna [3 ]
Reichl, Brandon G. [2 ]
Rosati, Tony [2 ]
Samuels, Bonita L. [2 ]
Shao, Andrew [6 ]
Stouffer, Ronald [2 ,7 ]
Winton, Michael [2 ]
Wittenberg, Andrew T. [2 ]
Xiang, Baoqiang [2 ,8 ]
Zadeh, Niki [2 ]
Zhang, Rong [1 ,2 ]
机构
[1] Princeton Univ, Program Atmospher & Ocean Sci, Princeton, NJ 08544 USA
[2] NOAA GFDL, Princeton, NJ USA
[3] SAIC GFDL, Princeton, NJ USA
[4] McGill Univ, Dept Atmospher & Ocean Sci, Montreal, PQ, Canada
[5] Univ Chicago, Dept Geophys Sci, Chicago, IL USA
[6] Univ Victoria, Canadian Ctr Climate Modeling & Anal, Victoria, BC, Canada
[7] Univ Arizona, Dept Geosci, Tucson, AZ USA
[8] Univ Corp Atmospheric Res, Cooperat Programs Adv Earth Syst Sci, Boulder, CO USA
基金
美国国家科学基金会; 加拿大自然科学与工程研究理事会; 美国海洋和大气管理局;
关键词
ocean circulation model; CORE; hybrid coordinates; MERIDIONAL OVERTURNING CIRCULATION; ANTARCTIC CIRCUMPOLAR CURRENT; NORTH-ATLANTIC SIMULATIONS; COUPLED CLIMATE MODELS; SOUTHERN-OCEAN; PART I; MESOSCALE EDDIES; Z-COORDINATE; TRACER TRANSPORTS; DIURNAL CYCLE;
D O I
10.1029/2019MS001726
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
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.
引用
收藏
页码:3167 / 3211
页数:45
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