Propagation and influence on tropical precipitation of intraseasonal variation over mid-latitude East Asia in boreal winter
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  • 英文篇名:Propagation and influence on tropical precipitation of intraseasonal variation over mid-latitude East Asia in boreal winter
  • 作者:JIAO ; Yang ; WU ; Renguang
  • 英文作者:JIAO Yang;WU Renguang;Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences;College of Earth and Planetary Sciences, University of Chinese Academy of Sciences;State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences;
  • 关键词:季节内风场变化 ; 东亚中纬度地区 ; 向东和向南传播 ; 热带降水
  • 英文关键词:Intraseasonal wind variation;;midlatitude East Asia;;eastward and southward propagation;;tropical precipitation
  • 中文刊名:AOSL
  • 英文刊名:大气和海洋科学快报(英文版)
  • 机构:Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences;College of Earth and Planetary Sciences, University of Chinese Academy of Sciences;State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences;
  • 出版日期:2019-05-16
  • 出版单位:Atmospheric and Oceanic Science Letters
  • 年:2019
  • 期:v.12
  • 基金:supported by the National Natural Science Foundation of China [grant numbers 41530425,41721004,41475081,and 41775080]
  • 语种:英文;
  • 页:AOSL201903002
  • 页数:7
  • CN:03
  • ISSN:11-5693/P
  • 分类号:11-17
摘要
本文研究冬季东亚中纬度地区9–29天季节内变化的传播特征和其对热带降水的影响。分析发现风场的季节内信号既可以向东传播,也可以向南传播。向东传播时,风场的季节内信号主要限于中纬度地区,表现为气旋和反气旋的向东移动。向南传播时,源于中纬度的经向风扰动可以深入到低纬度地区,甚至到达赤道附近。伴随的辐合辐散引起赤道附近地区降水异常,形成南海南部和中国东部-日本之间一个南北向偶极型降水异常。一个异常经向翻转环流在连接热带和中纬度季节内风场和降水变化中起着重要作用。
        The authors investigate the characteristics of propagation and the influence on tropical precipitation of 9–29-day intraseasonal variation over midlatitude East Asia during boreal winter, and find that the intraseasonal wind signal can propagate both eastward and southward. In the case of eastward propagation, the intraseasonal wind signal is mainly confined to the midlatitudes,featuring eastward migration of anomalous cyclones and anticyclones. In the case of southward propagation, intraseasonal meridional wind perturbations may extend from the mid to the low latitudes, and even the equatorial region. The accompanying wind convergence/divergence induces anomalous precipitation in the near-equatorial regions, forming a north–south dipole precipitation anomaly pattern between the southern South China Sea and the eastern China–Japan region. An anomalous meridional overturning circulation plays an important role in linking tropical and midlatitude intraseasonal wind and precipitation variations.
引文
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