Knowledge Management System Of Institute of Oceanology, Chinese Academy of Sciences
Simulation and Improvements of Oceanic Circulation and Sea Ice by the Coupled Climate System Model FGOALS-f3-L | |
Yuyang GUO; Yongqiang YU; Pengfei LIN; Hailong LIU; Bian HE; Qing BAO; Bo AN; Shuwen ZHAO; Lijuan HUA | |
发表期刊 | Advances in Atmospheric Sciences
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ISSN | 0256-1530 |
2020-09-07 | |
出版年 | 2020 |
卷号 | v.37期号:10页码:119-134 |
文献类型 | CNKI期刊论文 |
摘要 | This study documents simulated oceanic circulations and sea ice by the coupled climate system model FGOALS-f3-L developed at the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics, Chinese Academy of Sciences, under historical forcing from phase 6 of the Coupled Model Intercomparison Project(CMIP6). FGOALS-f3-L reproduces the fundamental features of global oceanic circulations, such as sea surface temperature(SST), sea surface salinity(SSS), mixed layer depth(MLD), vertical temperature and salinity, and meridional overturning circulations. There are notable improvements compared with the previous version, FGOALS-s2, such as a reduction in warm SST biases near the western and eastern boundaries of oceans and salty SSS biases in the tropical western Atlantic and eastern boundaries, and a mitigation of deep MLD biases at high latitudes. However, several obvious biases remain. The most significant biases include cold SST biases in the northwestern Pacific(over 4°C), freshwater SSS biases and deep MLD biases in the subtropics, and temperature and salinity biases in deep ocean at high latitudes. The simulated sea ice shows a reasonable distribution but stronger seasonal cycle than observed. The spatial patterns of sea ice are more realistic in FGOALS-f3-L than its previous version because the latitude–longitude grid is replaced with a tripolar grid in the ocean and sea ice model. The most significant biases are the overestimated sea ice and underestimated SSS in the Labrador Sea and Barents Sea, which are related to the shallower MLD and weaker vertical mixing. |
关键词 | CMIP6 FGOALS-f3-L historical evaluation ocean sea ice |
CNKI专辑号 | A; |
CNKI专辑名称 | 基础科学; |
CNKI专题号 | A009;A010; |
CNKI专题名称 | 气象学;海洋学; |
分类号 | P467;P73 |
收录类别 | 中科院核心 ; 中科院扩展 |
语种 | 英文; |
资助项目(基金) | supported by the Strategic Priority Research Program of the Chinese Academy of Sciences (Grant Nos. XDA19060102 and XDB42000000) ; the National Natural Science Foundation of China (Grant Nos. 41530426, 91958201, and 41931183) |
文献类型 | CNKI期刊论文 |
条目标识符 | http://ir.qdio.ac.cn/handle/337002/188045 |
专题 | 中国科学院海洋研究所 |
作者单位 | 1.StateKeyLaboratoryofNumericalModelingforAtmosphericSciencesandGeophysicalFluidDynamics,InstituteofAtmosphericPhysics,ChineseAcademyofSciences 2.UniversityofChineseAcademyofSciences 3.CenterforOceanMega-Science,ChineseAcademyofSciences 4.StateKeyLaboratoryofSevereWeather(LASW),ChineseAcademyofMeteorologicalSciences |
推荐引用方式 GB/T 7714 | Yuyang GUO,Yongqiang YU,Pengfei LIN,et al. Simulation and Improvements of Oceanic Circulation and Sea Ice by the Coupled Climate System Model FGOALS-f3-L. 2020. |
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