摘要
用施能定义的东亚夏季风指数,分别找出典型夏季风强弱年1961和1980年,分析水平风速、假相当位温、高度等的逐候变化特征与盛夏季节松嫩流域逐候降水量的关系。分析表明:东亚夏季风强弱对松嫩流域盛夏降水量有显著影响。在强夏季风年,较大的南风、较高的假相当位温、较深的东亚大槽使降水持续偏多。同时还发现,无论夏季风强弱,假相当位温高值总是与多降水相联系。
Applying the index of -the summer mon soon of East -Asia defined by Shineng,summer monsoon strong and weak years including 1961and 1980are selected respectively,and the relationship between every pentad midsummer precipitation over the Song -Nen river valley and every variable feature of horizontal wind velocity,geopotential height field,pseudo -potential temperature is analyzed.Results show that the and w eak East -Asia summer monsoon affect the midsummer precipitation over the Song -Nen river valley,and in the strong summer monsoon year,the high er southern wind,higher pseudo -potential temperature and deeper East -Asia trough bring about the pre cipitation above normal.The higher value of pseudo -potential temper-ature is always related closely to th e precipitation above normal in summer monsoon strong and weak years.
出处
《黑龙江气象》
2002年第3期12-14,共3页
Heilongjiang Meteorology
关键词
东亚夏季风
物理量变化
松嫩流域
降水
夏季
strong and weak years of the summer mo nsoon of East -Asia
physical quantity variation
the Song -Nen river valley
midsummer pr ecipitation