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The climatology and interannual variability of the East Asian summer monsoonsimulated by a weakly coupled data assimilation system
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  • 英文篇名:The climatology and interannual variability of the East Asian summer monsoonsimulated by a weakly coupled data assimilation system
  • 作者:LIN ; Renping ; ZHENG ; Fei ; DONG ; Xiao
  • 英文作者:LIN Renping;ZHENG Fei;DONG Xiao;International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences;
  • 关键词:海洋资料同化 ; 耦合模式 ; 东亚夏季风 ; AMIP
  • 英文关键词:Ocean data assimilation;;coupled model;;East Asian summer monsoon;;AMIP
  • 中文刊名:AOSL
  • 英文刊名:大气和海洋科学快报(英文版)
  • 机构:International Center for Climate and Environment Sciences, Institute of Atmospheric Physics, Chinese Academy of Sciences;
  • 出版日期:2019-03-16
  • 出版单位:Atmospheric and Oceanic Science Letters
  • 年:2019
  • 期:v.12
  • 基金:supported by the Strategic Priority Research Program of the Chinese Academy of Sciences [grant number XDA19030403];; the National Natural Science Foundation of China [grant numbers 41606027 and 41706028];; the National Key R&D Program of China [grant number2017YFA0604201];; the China Postdoctoral Science Foundation [grant number 2015M571095]
  • 语种:英文;
  • 页:AOSL201902009
  • 页数:7
  • CN:02
  • ISSN:11-5693/P
  • 分类号:70-76
摘要
为了改进耦合模式对东亚夏季风的模拟,本文发展了一个基于中国科学院地球系统模式的海洋资料同化系统。基于该同化系统,本文开展了同化观测海温的试验,并将同化试验的结果与传统的AMIP试验进行比较。结果表明,同化系统显著改进了对西北太平洋地区降水的气候态和季节循环、与ENSO和东亚夏季风相关联的东亚地区的降水和环流异常等的模拟。本文的工作表明,海气相互作用对东亚夏季风的模拟非常重要。耦合框架下的海洋资料同化系统可以在引入观测信息的同时不切断海气相互作用,这是同化试验较之AMIP试验有显著改进的原因所在。
        With the motivation to improve the simulation of the East Asian summer monsoon(EASM) in coupled climate models, oceanic data assimilation(DA) was used in CAS-ESM-C(Chinese Academy of Sciences–Earth System Model–Climate Component) in this study. Observed sea surface temperature was assimilated into CAS-ESM-C. The climatology and interannual variability of the EASM simulated in CAS-ESM-C with DA were compared with a traditional AMIP-type run.Results showed that the climatological spatial pattern and annual cycle of precipitation in the western North Paci?c, and the ENSO-related and EASM-related EASM circulation and precipitation, were largely improved. As shown in this study, air–sea coupling is important for EASM simulation. In addition, oceanic DA synchronizes the coupled model with the real world without breaking the air–sea coupling process. These two successful factors make the assimilation experiment a more reasonable experimental design than traditional AMIP-type simulations.
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