摘要
本文从空气稳定度和天气型两方面讨论海雾生成之后,如何持续和消散问题。发现在一定条件下、低空空气层结中“干层”的存在,利于雾的持续,而天气型转变带来的风和降水,常使海雾趋于消散。
Using air stability and weather patterns, we discuss the continuation and dissipation of sea fog. From which we find under certain conditions the existence of 'dry layer' in the lower air is available to the fog continuation; while on the other hand, sea fog always dissipated after the wind ( direction and Telocity ) and precipitation from changed weather patterns.
