Eddy-resolving Simulation of CAS-LICOM3 for Phase 2 of the Ocean Model Intercomparison Project

被引:1
|
作者
Yiwen LI [1 ,2 ]
Hailong LIU [1 ,2 ]
Mengrong DING [1 ,2 ]
Pengfei LIN [1 ,2 ]
Zipeng YU [1 ,2 ]
Yongqiang YU [1 ,2 ]
Yao MENG [1 ,2 ]
Yunlong LI [3 ]
Xiaodong JIAN [3 ]
Jinrong JIANG [4 ]
Kangjun CHEN [1 ]
Qian YANG [1 ,2 ]
Yaqi WANG [1 ,2 ]
Bowen ZHAO [1 ,2 ]
Jilin WEI [1 ,2 ]
Jinfeng MA [1 ]
Weipeng ZHENG [1 ,2 ]
Pengfei WANG [1 ]
机构
[1] State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics, Chinese Academy of Sciences
[2] College of Earth and Planetary Sciences, University of Chinese Academy of Sciences
[3] National Supercomputer Center in Tianjin
[4] Computer Network Information Center,Chinese Academy of Sciences
基金
中国国家自然科学基金;
关键词
D O I
暂无
中图分类号
P714 [调查及观测方法];
学科分类号
0816 ;
摘要
A 61-year(1958–2018) global eddy-resolving dataset for phase 2 of the Ocean Model Intercomparison Project has been produced by the version 3 of Chinese Academy of Science, the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics/Institute of Atmospheric Physics(LASG/IAP) Climate system Ocean Model(CAS-LICOM3). The monthly and a part of the surface daily data in this study can be accessed on the Earth System Grid Federation(ESGF) node. Besides the details of the model and experiments, the evolutions and spatial patterns of large-scale and mesoscale features are also presented. The mesoscale features are reproduced well in the high-resolution simulation, as the mesoscale activities can contribute up to 50% of the total SST variability in eddy-rich regions. Also, the large-scale circulations are remarkably improved compared with the low-resolution simulation, such as the climatological annual mean SST(the RMSE is reduced from 0.59°C to 0.47°C, globally) and the evolution of Atlantic Meridional Overturning Circulation. The preliminary evaluation also indicates that there are systematic biases in the salinity, the separation location of the western boundary currents, and the magnitude of eddy kinetic energy. All these biases are worthy of further investigation.
引用
收藏
页码:1067 / 1080
页数:14
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