通过我们的分析,可以看到强对流云和上冲强对流云主要位于热带辐合带(ITCZ),南太平洋辐合区(SPCZ),位于南纬15度和北纬15度之间的非洲大陆、南美大陆、印度洋和印度尼西亚,而在陆地上所观测到的上冲强对流云...
基于824个网页-相关网页
Therefore, the heating caused by the monsoon trough and ITCZ is an important thermodynamical factor affecting the intensity of the jet.
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。
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。
应用推荐