摘要
本文对东亚(100°E以东)地区1951—1956年的阻塞形势进行了分析.结果得出:东亚的阻塞形势六、七月出现得最多,位置多集中在沿海的大陆上,维持的时间多为七天.在阻塞形势下降水区分为三带:一在阻塞高压西侧一在其南面,另一带在副热带高压北缘.温度距平基本上与雨量距平相反.
Firstly in this paper,the seasonal occurance and geographical distribution of these blocking highs over Eastern Asia are described.Secondly,the preciptation and temperature departures over China during the period of the blocking in summer are studied.Finally,the effects of locations of blocking highs on climatology are also discussed.
作者
汤懋苍
TANG MOU-TSANG(Institute of the Geophysics and Meteorology,Academia Sinica)
出处
《气象学报》
1957年第4期282-293,共12页
Acta Meteorologica Sinica
