摘要
根据调研资料,运用大气物理学原理从宏观和微观两个角度,初步分析了夏季期间潮汐的变化对华南沿海局地降雨形成的影响。发现遇到涨潮时,海上积云移到沿海陆地上空容易造成局地性降雨,即在开始降雨前几小时通常是高潮位。
The effect of the tide variation during summer on the formation of coastal local rain in South China has been analysed preliminarily from the macro and micro angles on the basis of research dare and atmospheric physics. When the flood tide occurs, cumulus moves toward the land and the local rain happens easily. In other words, the high tide level appears usually several hours before it begins to rain.
出处
《海洋通报》
CAS
CSCD
北大核心
2001年第2期83-86,共4页
Marine Science Bulletin
关键词
潮汐
局地性降雨
凝结核
大气物理学
积云
tide
the out-growth of the coastal local rain
condensation nucleus