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BCC-CSM2-MR模式对北极海冰和气候的模拟及预估
引用本文:任永建,肖莺,周兵. BCC-CSM2-MR模式对北极海冰和气候的模拟及预估[J]. 气候变化研究进展, 2021, 17(1): 58-69. DOI: 10.12006/j.issn.1673-1719.2019.168
作者姓名:任永建  肖莺  周兵
作者单位:湖北省气象服务中心,武汉 430074;武汉区域气候中心,武汉 430074;中国气象局国家气候中心,北京 100081
基金项目:全球变化研究国家重大科学研究计划(2015CB953900);中国气象局气候变化专项(CCSF202033,CCSF202008)。
摘    要:
基于第六次耦合模式比较计划(CMIP6),使用新一代全球模式BCC-CSM2-MR的历史试验和未来共享社会经济路径(SSPs)数据,依据Hadley中心的海表面温度和海冰密集度数据及NCEP/NCAR I再分析资料,评估了BCC-CSM2-MR模式对北极海冰及北极气候的模拟能力,并对未来变化进行了预估.结果表明:BCC...

关 键 词:北极  海冰密集度  模拟  共享社会经济路径(SSP)  预估
收稿时间:2019-07-19
修稿时间:2019-09-05

Simulation and projection of Arctic sea ice and climate by BCC-CSM2-MR
REN Yong-Jian,XIAO Ying,ZHOU Bing. Simulation and projection of Arctic sea ice and climate by BCC-CSM2-MR[J]. Progressus Inquisitiones DE, 2021, 17(1): 58-69. DOI: 10.12006/j.issn.1673-1719.2019.168
Authors:REN Yong-Jian  XIAO Ying  ZHOU Bing
Affiliation:1.Hubei Meteorological Service Center, Wuhan 430074, China2 Wuhan Regional Climate Center, Wuhan 430074, China3 National Climate Center, China Meteorological Administration, Beijing 100081, China
Abstract:
Based on the Coupled Model Intercomparison Project Phase 6(CMIP6),the paper evaluates the performance of the state-of-the-art climate model BCC-CSM2-MR in simulating the Arctic sea ice and the Arctic climate using sea surface temperature and sea ice density data from the Hadley Center and the reanalyzed data from National Center for Environmental Prediction and National Center for Atmospheric Research and further projected their potential changes in a future warmer world under Shared Socio-economic Path(SSP).The results show that the BCC-CSM2-MR model can better reproduce the multi-year average spatial distribution of Arctic sea ice concentration,near-surface atmospheric mean temperature and sea surface temperature.However,the simulation has a certain deviation from the observation of the atmospheric temperature in the Arctic,which possible leads to differences in the simulation of sea ice in the corresponding areas.In the 21st century,the Arctic sea ice range is projected to decrease continuously,with a significant reduction in September and a relatively weaker trend in March.In March,the atmospheric temperature would show a consistent increase over most of the Arctic except the North Atlantic.The increasement of atmosphere temperature is weaker in September than that in March.Unlike the atmosphere temperature,the sea surface temperature would both increase in March and September in most parts of the Arctic except the Labrador Sea.The increasement of sea surface temperature is much greater in September than that in March.
Keywords:Arctic  Sea ice intensity  Simulation  Shared Socio-economic Path(SSP)  Projection
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