Extratropical Southern Hemisphere Cyclones: Harbingers of Climate Change?
南半球温带气旋：气候变化的先兆？
Mei-yu front belongs to a semi-tropical and semi-extratropical weather system;
梅雨锋是半热带、半温带性质的天气系统；
SONGDA finally turned into an extratropical cyclone as it reached the southern coast of Honshu, Japan.
桑达最后在到达日本本州南部时演变为温带气旋。
In this Paper, relations between tne Pacific SST field and extratropical cyclones in East Asia are analysed.
本文分析了太平洋海温场与东亚温带气旋之间的相关关系。
North Pacific extratropical cyclone is an important weather system severely threatening the ships sailing on high latitude routes.
北太平洋温带气旋是对航行在北太平洋中高纬航线上的船舶构成严重威胁的重要天气系统。
We study the interannual variability of the extratropical westerly jet over East Asian (EAJS), its impacts and possible mechanisms.
探讨了东亚地区副热带西风急流(EAJS)位置的年际变化特征、影响及其可能机制。
In this paper, a extratropical storm surge model, which includes boundary layer wind model over sea and storm surge numerical model, is built.
本文建立一个温带风暴潮模式，包括海上边界层风场模式和风暴潮数值模式。
In this paper the correlation is analysed between the sea surface temperature (SST) of the North Atlantic and the extratropical cyclone in East Asia.
本文分析了北大西洋海温场与东亚各月温带气旋个数的相关。
In the extratropical North Pacific Ocean, significant correlation exists between anomalous latent and sensible heat flux and SST tendency anomalies in boreal winter.
在冬季热带外北太平洋上，海洋向大气释放的湍流热通量同sst倾向存在显著的相关。
IT is pointed out that the nature of the Mei-Yu front's structures has changed into the sub-tropical style, something between extratropical fronts and ITCZ during the torrential rain period.
研究表明，出现强降水时的梅雨锋结构已经变性或者说它是介于温带锋面结构和ITCZ结构之间的副热带锋系结构。
Through the analysis, it is shown that the Matsa s extratropical transition and the re-intensification are due to the intrusion of cold air from the upper-level trough into the typhoons circulation.
以一个在陆上长久维持并最终演变成温带气旋的登陆台风“麦莎”为研究对象，通过对其北上变性过程的分析发现，台风与中高纬西风槽的相互作用使得冷空气侵入是其变性加强的原因。
Through the analysis, it is shown that the Matsa s extratropical transition and the re-intensification are due to the intrusion of cold air from the upper-level trough into the typhoons circulation.
以一个在陆上长久维持并最终演变成温带气旋的登陆台风“麦莎”为研究对象，通过对其北上变性过程的分析发现，台风与中高纬西风槽的相互作用使得冷空气侵入是其变性加强的原因。
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