摘要
本文采用对两种气象要素场的相关场作EOF分解的方法,对1951-1979年太平洋海-气感热、潜热通量与长江流域降水和东亚500hPa环流作了分析。结果表明,太平洋海-气感热、潜热通量与后期(τ=6)长江流域降水存在显著相关区,感热和潜热的异常分布能造成长江流域降水分布不均。同时,冬季(12-2月)太平洋潜热通量的变化与夏季(6-8月)对流层中层的赤道辐会带、副热带高压等系统有较密切的联系。
In this paper.the EOF technique is utilized to analyze the field of time cross-correlationcoefticients between two meteorological fields, such as the correlations between the air-sea latent andsensible heat flux in the Pacific and the precipitation over the Yangtze River valley and the 500 hPa cir-culation in the period of 1951-1979.The results show that there exists teleconnectionship between thesensible and latent heat flux in the Pacific and the precipitation over the Yangtze River valley for thelags (τ=6). The anomalies of the latent and sensible heat flux in the eastern equatorial Pacific may causethe uneven distribution of precipitation over the above mentioned area.Moreover, the variations of la-tent heat flux in the winter (DJF) are also associated with the variations of equatorial convergence belt,subtropical anticyclone etc. over the mid-troposphere in the summer (JJA).
出处
《大气科学》
CSCD
北大核心
1994年第1期89-95,共7页
Chinese Journal of Atmospheric Sciences
关键词
太平洋
海-气
热通量
降水
簂atent heat flux
sensible heat flux, telecorrelation
empirical orthogonal function (EOF)