FGOALS-g3 Model Datasets for CMIP6 Flux-Anomaly-Forced Model Intercomparison Project

被引:0
|
作者
Yaqi Wang
Zipeng Yu
Pengfei Lin
Hailong Liu
Jiangbo Jin
Lijuan Li
Yanli Tang
Li Dong
Kangjun Chen
Yiwen Li
Qian Yang
Mengrong Ding
Yao Meng
Bowen Zhao
Jilin Wei
Jinfeng Ma
Zhikuo Sun
机构
[1] Chinese Academy of Sciences,State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics
[2] University of Chinese Academy of Sciences,College of Earth and Planetary Sciences
[3] Chinese Academy of Sciences,International Center for Climate and Environment Sciences, Institute of Atmospheric Physics
[4] Sun Yat-sen University,School of Atmospheric Sciences, Guangdong Province Key Laboratory for Climate Change and Nature Disaster Studies
来源
关键词
FAFMIP; CMIP6; global mean sea level rise; dynamic sea level change; FAFMIP; CMIP6; 全球平均海平面上升; 动力海平面变化;
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学科分类号
摘要
The Flux-Anomaly-Forced Model Intercomparison Project (FAFMIP) is an endorsed Model Intercomparison Project in phase 6 of the Coupled Model Intercomparison Project (CMIP6). The goal of FAFMIP is to investigate the spread in the atmosphere-ocean general circulation model projections of ocean climate change forced by increased CO2, including the uncertainties in the simulations of ocean heat uptake, global mean sea level rise due to ocean thermal expansion and dynamic sea level change due to ocean circulation and density changes. The FAFMIP experiments have already been conducted with the Flexible Global Ocean-Atmosphere-Land System Model, gridpoint version 3.0 (FGOALS-g3). The model datasets have been submitted to the Earth System Grid Federation (ESGF) node. Here, the details of the experiments, the output variables and some baseline results are presented. Compared with the preliminary results of other models, the evolutions of global mean variables can be reproduced well by FGOALS-g3. The simulations of spatial patterns are also consistent with those of other models in most regions except the North Atlantic and the Southern Ocean, indicating large uncertainties in the regional sea level projections of these two regions.
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页码:1093 / 1101
页数:8
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