摘要
本文分析了雷达观测结果，发现近海海面上的水汽向上输送随季节而变化，由于季节的变化和不同的天气情况，海表面大气现象在雷达中有不同的显示，根据这些显示得到了不同的信息，由此而得出春秋两季海表面水汽向上输送量的不同。
In this paper, the observed results by radar over the coastal sea are analysed It is found that the yertical transport of water vapor from the sea surface to the atmosphere is different in different seasons. Owing to the change of season and weather conditions, the radarscope display is different for different atmospheric states oyer the sea surface. From the different echoes, it follows that the quantity of vertical transport of water vapor over the sea surface is different in spring and autumn.
出处
《海洋湖沼通报》
CSCD
北大核心
1994年第2期202-207,共6页
Transactions of Oceanology and Limnology
关键词
海面
水汽输送
季节变化
雷达波
Radar Wave,Clear Air Echo, Refractive Index,Inversion,Vertical Transport,Water Vapor
