冬半年北半球大气对赤道东太平洋海温的响应  

THE WINTERTIME NORTHERN HEMISPHERE ATMOSPHERIC RESPONSE TO SST I-N THE EASTERN EQUATORIAL PACIFIC

作　　者：蒋全荣[1] 

机构地区：[1]南京大学大气科学系

出　　处：《气象科学》1989年第3期255-262,共8页Journal of the Meteorological Sciences

摘　　要：分析表明,亦道东太平洋海温与北半球中太平洋海温有着不同的变化特征。冬半年大气对赤道东太平洋海温的响应表现为不同于PNA的呈纬向分布的模态结构。夏半年赤道东太平洋海温的强的“记忆”能力对长期天气趋势预报有一定的意义。The different features of SST variations in theC entral and the Eastern Equatorial Pacific (EEP) are shown. The wintertime Northern Hemisphere atmospheric response to SST in EEP is the zonal mode structure which is different from PNA. The strong memory of summer half year SST in EEP plays a role in the long forecast.

关 键 词：大气 海温 北半球 赤道 

分 类 号：P732.6[天文地球—海洋科学]