摘要
本文利用中、美海-气联合调查资料,对8626号台风活动与周围水文气象要素相互作用进行了初步分析,得出了以下结果:1.随着台风的接近,海-气间热量和水汽交换增大,是台风发展的必要条件。2.当船接近台风时,抬升凝结高度和自由对流高度越来越低,这对潜热释放是有利的。3.海面温度较高(≥28℃)对台风形成和发展是重要的。
A primary study of the interaction between No. 8626 Typhoon and its oceanic and atmospheric environment has been made by using the data from the Joint Sino—US Air-Sea Interaction Investigation. The results show that 1. with the approach of Typhoon the air-sea heat and moisture exchange become greater, which is the necessary condition for the development of Typhoon, 2. when the ship is approaching to the Typhoon, the ascending condensation level and the free convection level are getting lower and lower. This is favorable for the release of the latent heat, 3. the high sea surface temperature (≥28℃) is importa. for the formation and the development of Typhoon.
出处
《黄渤海海洋》
CSCD
1990年第2期22-27,共6页
Journal of Oceanography of Huanghai & Bohai Seas
