摘要
海洋考察资料分析表明 ,夏季风期间南海南部海区海洋输向大气的热通量倍增 ,热通量的增、减过程与对流天气密切相关 ,季风潮天气过程中的热通量值居各天气过程之首 ,某些时段感热通量会出现大气向海洋的反向输送过程 ,地理环境使同一天气过程影响下海区内各通量的水平分布明显不均 ,海洋输向大气的热通量明显影响 5 0 0hPa以下各层大气。
The analysis on the oceanology data shows heat flux increase from ocean transport to air in the southern south China sea during summer monsoon Heat flux increase or deciease is relateal with to convective weather Heat flux Volume is maximum during the monsoon surge.The transport of sensible heat flux was from air to sea some times Geographic environment leads to homzontal distribution obviously different under the same weather process Heat flux from ocean to air obviously influences the blow 500hPa
出处
《广东气象》
2003年第2期5-7,共3页
Guangdong Meteorology
