首页> 外文会议>Fuzzy Systems and Knowledge Discovery, 2009. FSKD '09 >Nonlinear Dynamical Structure of precipitation in China and its Regional Climatic Characters
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Nonlinear Dynamical Structure of precipitation in China and its Regional Climatic Characters

机译:中国降水非线性动力结构及其区域气候特征

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The statistical data show that weather(precipitation) in the five dynamic climate characteristic regions simultaneously becomes dry, wet and normal, that is to say, each region possesses a common spatial-temporal characteristic structure. Further analysis of physical mechanisms suggests that the Jianghuai pattern and South China pattern are close related with ENSO, which may results from the effect of the India-East Asia (IEA) tele connection pattern; among the other three patterns North and Northeast China patterns are positively related with the ridge line position of subtropical high, but the ENSO shows no obvious influence on the three patterns, which may be associated with that the regions are mainly out of the weak impact area of ENSO;further more the influence of the ridge line of subtropical high on precipitation in North China is most remarkable. This has instructive significance for the development of regional climate models, and the analysis of precipitation characters and precipitation forecast.
机译:统计数据表明,五个动态气候特征区域的天气(降水)同时变为干燥,潮湿和正常,也就是说,每个区域都具有共同的时空特征结构。对物理机制的进一步分析表明,江淮模式和华南模式与ENSO密切相关,这可能是由于印度—东亚(IEA)远程连接模式的影响所致。在其他三种模式中,华北和东北模式与副热带高压的脊线位置成正相关,但是ENSO对这三种模式没有明显的影响,这可能与该地区主要在弱势影响区之外有关ENSO的影响;此外,华北地区副高脊线对华北降水的影响最为显着。这对于区域气候模式的发展以及降水特征的分析和降水预报具有指导意义。

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