摘要
台风是影响我国沿海地区的主要灾害性天气之一。对台风发生、发展及移行规律的研究是海洋气象研究工作的重要内容。本文拟分析8114号台风的天气学特性,计算和讨论台风进入东海后的热力学和动力学结构,以期进一步了解台风的基本特性及其变化规律。
In this paper,synoptic situation and cloud characteristics are analyzed,and dynamical and thermal structures are calculated during Typhoon No.8114.It was concluded that this Typhoon was asymmetry.In the right half and left front quadrants of the Typhoon,convergence occurred in bottom layer,divergence in intermediate and upper layers,upward motion in the whole column;heat flux was downward in bottom layer and upward in intermediate and upper layers,However,the situation was opposite to the above in the left rear quadrants of the Typhoon.It was also shown that the maintenance and evolutions of Typhoon was strongly correlated to the large scale heat budget between atmosphere and ocean.
作者
赵永平
Zhao Yongping(Institute of Oceanology,Academia Sinica)
出处
《海洋与湖沼》
1983年第6期548-559,共12页
Oceanologia Et Limnologia Sinica
