摘要
通过相关普查及分析发现,冬季(11～1月500hPa环流特征与夏季(8～9月)西北太平洋(含我国南海)热带风景生成的多少有良好的相关关系。并通过两个热带风暴异常(特少和特多)年份的对比分析探讨了其相关机制。
An analysis of the past meterological data is made and a good correlation is found between the circulative characteristics at 500 hPa in winter from November through January and the frequency of tropical storms in the Northwest Pacific Ocean,including the South China Sea,in summer from August through September.The correlative mechanism is discussed through comparing the two anomalous years at each end of the frequency spectrum,least and most respectively.
出处
《海洋通报》
CAS
CSCD
北大核心
1991年第4期19-24,共6页
Marine Science Bulletin
