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首页> 外文期刊>Weather and forecasting >Potential Influence of the East Asia-Pacific Teleconnection Pattern on Persistent Precipitation in South China: Implications of Atypical Yangtze River Valley Cases
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Potential Influence of the East Asia-Pacific Teleconnection Pattern on Persistent Precipitation in South China: Implications of Atypical Yangtze River Valley Cases

机译:东亚 - 太平洋遥理模式对华南持续降水的潜在影响:非典型长江谷案件的含义

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摘要

In this study, cases of the East Asia-Pacific (EAP) teleconnection pattern not responsible for persistent precipitation processes in the Yangtze River valley (YRV) have been investigated. The results suggest that such a type of EAP pattern has some linkage with persistent precipitation processes in south China (SC) with the following properties: 1) in response to the negative SSTAs and anticyclone near the Philippines, the meridional energy propagates from the low latitudes over the north of the Philippines; 2) the western Pacific subtropical high (WPSH) then intensifies and extends westward; 3) a meridional triple structure of the EAP teleconnection pattern is established; 4) at the same time, the cyclonic circulation over northeastern China introduces cold and dry air to the lower latitudes, merging with the water vapor into SC and leading to heavy precipitation from the fringe of the WPSH, the South China Sea, and the Bay of Bengal and the combination of systems persists for at least 3 days, leading to the persistent precipitation processes in SC; and 5) compared with the EAP teleconnection responsible for the precipitation in YRV, the positions of the three centers in the mid- and low latitudes are more southerly located than the YRV EAP centers. Further study indicates that the ocean surface heat conditions in the areas near the Philippines seem to be important in affecting the EAP teleconnection pattern for persistent precipitation processes in SC. Finally, all of the cases with persistent precipitation in SC during 1961-2010 linked with the EAP pattern have been investigated; the results are consistent with the above conclusions.
机译:在这项研究中,东亚-太平洋(EAP)遥相关模式与长江流域(YRV)的持续降水过程无关。结果表明,这种EAP模式与华南持续降水过程有一定的联系,具有以下特点:1)响应菲律宾附近的负SSTA和反气旋,经向能量从菲律宾北部低纬度传播;2) 西太平洋副热带高压随后增强并向西延伸;3) 建立了EAP遥相关模式的经向三重结构;4) 同时,中国东北部的气旋环流将冷干空气引入低纬地区,与水汽合并进入南太平洋副热带高压,导致西太平洋副热带高压边缘、南海和孟加拉湾的强降水,这些系统的组合持续至少3天,导致南太平洋的持续降水过程;5)与造成YRV降水的EAP遥相关相比,中低纬三个中心的位置比YRV EAP中心更偏南。进一步的研究表明,菲律宾附近地区的海洋表面热条件似乎对南太平洋持续降水过程的EAP遥相关模式有重要影响。最后,对1961-2010年期间南太平洋持续降水与EAP模式相关的所有案例进行了调查;结果与上述结论一致。

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  • 来源
    《Weather and forecasting》 |2018年第1期|共16页
  • 作者单位

    China Acad Meteorol Sci State Key Lab Severe Weather Beijing Peoples R China;

    China Acad Meteorol Sci State Key Lab Severe Weather Beijing Peoples R China;

    China Acad Meteorol Sci State Key Lab Severe Weather Beijing Peoples R China;

    Nanjing Univ Informat Sci &

    Technol Joint Int Res Lab Climate &

    Environm Change ILCEC Collaborat Innovat Ctr Forecast &

    Evaluat Meteoro Key Lab Meteorol Disaster Minist Educ KLME Nanjing Jiangsu Peoples R China;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类 大气科学(气象学);
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