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A Possible Mechanism of the Impact of Atmosphere-Ocean Interaction on the Activity of Tropical Cyclones Affecting China

机译:大气与海洋相互作用对热带气旋活动影响中国的可能机制

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摘要

In this study,tropical cyclone data from China Meteorological Administration (CMA) and the ECMWF reanalysis data for the period 1958 2001 was used to propose a possible mechanism for the impacts of airsea interaction on the activity of tropical cyclones (TCs) affecting China.The frequency of TCs affecting China over past 40 years has trended downward,while during the same period,the air sea interaction in the two key areas of the Pacific region has significantly weakened.Our diagnoses and simulations suggest that air sea interactions in the central North Pacific tropics and subtropics (Area 1) have an important role in adjusting typhoon activities in the Northwest Pacific in general,and especially in TC activity affecting China.On the contrary,impacts of the air-sea interaction in the eastern part of the South Pacific tropics (Area 2) were found to be rather limited.As both observational analysis and modeling studies show that,in the past four decades and beyond,the weakening trend of the latent heat released from Area 1 matched well with the decreasing Northwest Pacific TC frequency derived from CMA datasets.Results also showed that the weakening trend of latent heat flux in the area was most likely due to the decreasing TC frequency over the Northwest Pacific,including those affecting China.Although our preliminary analysis revealed a possible mechanism through which the air sea interaction may adjust the genesis conditions for TCs,which eventually affect China,other relevant questions,such as how TC tracks and impacts are affected by these trends,remain unanswered.Further in-depth investigations are required.
机译:在这项研究中,使用了来自中国气象局(CMA)的热带气旋数据和1958 2001年的ECMWF再分析数据,提出了可能的机制来影响海气相互作用对影响中国的热带气旋(TC)的活动。在过去40年中,影响中国的TC频率呈下降趋势,而同期,太平洋地区两个关键区域的海气相互作用大大减弱。我们的诊断和模拟表明,北太平洋中部的海气相互作用热带和亚热带(区域1)在总体上调节西北太平洋的台风活动,特别是在影响中国的TC活动方面起着重要作用。相反,南太平洋热带地区的海海相互作用的影响(第2区)被发现是相当有限的。正如观察分析和模型研究表明,在过去的40年及以后的时间里, 1区释放的潜热与从CMA数据集获得的西北太平洋TC频率下降吻合得很好。结果还表明,该区域的潜热通量减弱趋势最可能是西北太平洋TC频率下降的原因,包括尽管我们的初步分析揭示了一种可能的机制,海气相互作用可能通过这种机制调整了TC的形成条件,最终影响了中国,但其他相关问题(如这些趋势如何影响TC的轨迹和影响)仍然没有得到答案。 。需要进行进一步的深入研究。

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  • 来源
    《大气科学进展(英文版)》 |2012年第4期|661-674|共14页
  • 作者单位

    Laboratory for Climate Studies, China Meteorological Administration, Beijing 100081;

    Key Laboratory of Mesoscale Severe Weather of Ministry of Education,Nanjing University, Nanjing 210093;

    Shanghai Typhoon Institute, China Meteorological Adminstration, Shanghai 200030;

    Atmospheric Physics Research Institute of Chinese Academy of Sciences, Beijing 100029;

    Laboratory for Climate Studies, China Meteorological Administration, Beijing 100081;

    Key Laboratory of Mesoscale Severe Weather of Ministry of Education,Nanjing University, Nanjing 210093;

  • 收录信息 中国科学引文数据库(CSCD);中国科技论文与引文数据库(CSTPCD);
  • 原文格式 PDF
  • 正文语种 chi
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