研究了西北太平洋夏季风特征及其季风槽结构对台风生成的影响。
The influence of Northwest Pacific summer monsoon(NWPSM) characteristics and the structure of monsoon trough on typhoon genesis is studied.
由季风槽和ITCZ引起的加热，是影响急流强度重要的热力因子。
Therefore, the heating caused by the monsoon trough and ITCZ is an important thermodynamical factor affecting the intensity of the jet.
亚洲夏季风槽包括两大重要组成部分，即南海夏季风槽和印度夏季风槽。
The Asian summer monsoon trough consists of two major components: the South China Sea (SCS) summer monsoon trough and the Indian summer monsoon trough.
结果表明，无论是辐合还是对流，南海夏季风槽都强于副热带夏季风槽。
The results show that the SCSSMT is stronger whether in convergence or convection than the STSMT.
其中，季风槽的异常偏西及在盛夏的异常偏北对TC的异常活动产生了主要影响。
And in which the anomalous westward and northward movements of monsoon trough in midsummer exerted a main effect on the TC anomalous activities.
而且，季风槽向南移动轴的今天经过比卡内尔，迪萨，贾巴尔普尔，赖布尔，低压区中心。
And, the southward moved axis of monsoon trough today passes through Bikaner, Deesa, Jabalpur, Raipur, Center of low pressure area.
而且，季风槽向南移动轴的今天经过比卡内尔，迪萨，贾巴尔普尔，赖布尔，低压区中心。
And, the southward moved axis of monsoon trough today passes through Bikaner, Deesa, Jabalpur, Raipur, Center of low pressure area.
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