CAS FGOALS-f3-L Model Datasets for CMIP6 GMMIP Tier-1 and Tier-3 Experiments

被引:36
作者
He, Bian [1 ,2 ,3 ]
Liu, Yimin [1 ,2 ,3 ]
Wu, Guoxiong [1 ,2 ,3 ]
Bao, Qing [1 ,2 ,3 ]
Zhou, Tianjun [1 ,2 ,3 ]
Wu, Xiaofei [4 ]
Wang, Lei [1 ,3 ]
Li, Jiandong [1 ,3 ]
Wang, Xiaocong [1 ,2 ,3 ]
Li, Jinxiao [1 ,3 ]
Hu, Wenting [1 ,3 ]
Zhang, Xiaoqi [1 ,5 ]
Sheng, Chen [1 ,3 ]
Tang, Yiqiong [1 ,5 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing 100029, Peoples R China
[2] Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
[3] Univ Chinese Acad Sci, Coll Earth & Planetary Sci, Beijing 100029, Peoples R China
[4] Chengdu Univ Informat Technol, Sch Atmospher Sci, Plateau Atmosphere & Environm Key Lab Sichuan Pro, Chengdu 610225, Sichuan, Peoples R China
[5] Nanjing Univ Informat Sci & Technol, Nanjing 210044, Jiangsu, Peoples R China
基金
中国国家自然科学基金;
关键词
global monsoon; CMIP6; GMMIP; Tibetan Plateau; orographic perturbation; ASIAN SUMMER MONSOON; INTERANNUAL VARIABILITY; INDIAN-OCEAN; GENERAL-CIRCULATION; MOUNTAIN UPLIFT; TIBETAN PLATEAU; NORTH-AMERICAN; PARAMETERIZATION; CLIMATOLOGY; PRECIPITATION;
D O I
10.1007/s00376-019-9085-y
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The Chinese Academy of Sciences (CAS) Flexible Global Ocean-Atmosphere-Land System (FGOALS-f3-L) model datasets prepared for the sixth phase of the Coupled Model Intercomparison Project (CMIP6) Global Monsoons Model Intercomparison Project (GMMIP) Tier-1 and Tier-3 experiments are introduced in this paper, and the model descriptions, experimental design and model outputs are demonstrated. There are three simulations in Tier-1, with different initial states, and five simulations in Tier-3, with different topographies or surface thermal status. Specifically, Tier-3 contains four orographic perturbation experiments that remove the Tibetan-Iranian Plateau, East African and Arabian Peninsula highlands, Sierra Madre, and Andes, and one thermal perturbation experiment that removes the surface sensible heating over the Tibetan-Iranian Plateau and surrounding regions at altitudes above 500 m. These datasets will contribute to CMIP6's value as a benchmark to evaluate the importance of long-term and short-term trends of the sea surface temperature in monsoon circulations and precipitation, and to a better understanding of the orographic impact on the global monsoon system over highlands.
引用
收藏
页码:18 / 28
页数:11
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