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DOI | 10.1029/2019MS002012 |
The Flexible Global Ocean-Atmosphere-Land System Model Grid-Point Version 3 (FGOALS-g3): Description and Evaluation | |
Li L.; Yu Y.; Tang Y.; Lin P.; Xie J.; Song M.; Dong L.; Zhou T.; Liu L.; Wang L.; Pu Y.; Chen X.; Chen L.; Xie Z.; Liu H.; Zhang L.; Huang X.; Feng T.; Zheng W.; Xia K.; Liu H.; Liu J.; Wang Y.; Wang L.; Jia B.; Xie F.; Wang B.; Zhao S.; Yu Z.; Zhao B.; Wei J. | |
发表日期 | 2020 |
ISSN | 19422466 |
卷号 | 12期号:9 |
英文摘要 | This paper introduces the Flexible Global Ocean-Atmosphere-Land System Model: Grid-Point Version 3 (FGOALS-g3) and evaluates its basic performance based on some of its participation in the sixth phase of the Coupled Model Intercomparison Project (CMIP6) experiments. Our results show that many significant improvements have been achieved by FGOALS-g3 in terms of climatological mean states, variabilities, and long-term trends. For example, FGOALS-g3 has a small (−0.015°C/100 yr) climate drift in 700-yr preindustrial control (piControl) runs and smaller biases in climatological mean variables, such as the land/sea surface temperatures (SSTs) and seasonal soil moisture cycle, compared with its previous version FGOALS-g2 during the historical period. The characteristics of climate variabilities, for example, Madden-Julian oscillation (MJO) eastward/westward propagation ratios, spatial patterns of interannual variability of tropical SST anomalies, and relationship between the East Asian Summer Monsoon and El Niño–Southern Oscillation (ENSO), are well captured by FGOALS-g3. In particular, the cooling trend of globally averaged surface temperature during 1940–1970, which is a challenge for most CMIP3 and CMIP5 models, is well reproduced by FGOALS-g3 in historical runs. In addition to the external forcing factors recommended by CMIP6, anthropogenic groundwater forcing from 1965 to 2014 was incorporated into the FGOALS-g3 historical runs. © 2020. The Authors. |
语种 | 英语 |
scopus关键词 | Atmospheric pressure; Atmospheric temperature; Climate models; Climatology; Groundwater; Soil moisture; Surface properties; Climate variability; Coupled Model Intercomparison Project; East Asian summer monsoon; Historical periods; Interannual variability; Madden-Julian oscillation; Southern oscillation; Surface temperatures; Oceanography; air-sea interaction; annual variation; climate forcing; climate variation; CMIP; El Nino-Southern Oscillation; Madden-Julian oscillation; monsoon; sea surface temperature; soil moisture; summer |
来源期刊 | Journal of Advances in Modeling Earth Systems
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/156653 |
作者单位 | State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, China; College of Earth and Planetary Sciences, University of Chinese Academy of Sciences, Beijing, China; Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao, China; Department of Earth System Science, Tsinghua University, Beijing, China; Key Laboratory of Meteorological Disaster, Ministry of Education (KLME)/Joint International Research Laboratory of Climate and Environmental Change (ILCEC)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters (CIC-FEMD), Nanjing University of Information Science and Technology, Nanjing, China; Department of Atmospheric Sciences, Yunnan University, Kunming, China; Anhui Meteorological Observatory, Hefei, China |
推荐引用方式 GB/T 7714 | Li L.,Yu Y.,Tang Y.,et al. The Flexible Global Ocean-Atmosphere-Land System Model Grid-Point Version 3 (FGOALS-g3): Description and Evaluation[J],2020,12(9). |
APA | Li L..,Yu Y..,Tang Y..,Lin P..,Xie J..,...&Wei J..(2020).The Flexible Global Ocean-Atmosphere-Land System Model Grid-Point Version 3 (FGOALS-g3): Description and Evaluation.Journal of Advances in Modeling Earth Systems,12(9). |
MLA | Li L.,et al."The Flexible Global Ocean-Atmosphere-Land System Model Grid-Point Version 3 (FGOALS-g3): Description and Evaluation".Journal of Advances in Modeling Earth Systems 12.9(2020). |
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