首页 | 本学科首页   官方微博 | 高级检索  
     检索      

CHARACTERISTICS ON INTERANNUAL VARIATIONS OF NORTH PACIFIC SST AND ITS RELATION TO EAST ASIA CLIMATE
作者姓名:解思梅  TAKASHI AOKI  MASATOSHI M. YOSHINO
作者单位:National Research Center For Marine Environment Forecasts,SOA,Beijing,China,Japan Meteorological Agency Tokyo Japan,Institute of Geoscience University of Tsukuba Japan
摘    要:The interannual variations of the monthly sea surface temperature (SST) in the North Pacific (including Equatorial East Pacific) during 1951-1980 are analysed by means of EOF method. The findings are:(1) In the cold and warm ocean current areas, such as the North Pacific Current, the California Current and the Equatorial East Pacific areas, the convergence speeds are the fastest, while in the Kuroshio and the western part of the North Equatorial Current areas they are fast only in winter.(2) The physical features of the first 3 eigenvectors are obvious. The first eigenvector shows that the SST values are high in the south and low in the north in the latitudinal distribution of the SST field. The warm current area, i.e. the northwestern part of the North Pacific is positive and the cold current area, i.e. the southeastern part of the North Pacific including the Eastern Equatorial Pacific is negative. The zero line of the 2nd eigenvector field runs from northeast to southwest, in the same direction as the

收稿时间:1985/10/20 0:00:00
修稿时间:1986/3/31 0:00:00

CHARACTERISTICS ON INTERANNUAL VARIATIONS OF NORTH PACIFIC SST AND ITS RELATION TO EAST ASIA CLIMATE
XlE SlMEI,TAKASHI AOKI and MASATOSHI M. YOSHINO.CHARACTERISTICS ON INTERANNUAL VARIATIONS OF NORTH PACIFIC SST AND ITS RELATION TO EAST ASIA CLIMATE[J].Acta Oceanologica Sinica,1987,6(1):68-79.
Authors:XlE SlMEI  TAKASHI AOKI and MASATOSHI M YOSHINO
Institution:1.National Research Center For Marine Environment Forecasts, SOA, Beijing, China2.Japan Meteorological Agency, Tokyo, Japan3.Institute of Geoscience, University of Tsukuba, Japan
Abstract:The interannual variations of the monthly sea surface temperature (SST) in the North Pacific (including Equatorial East Pacific) during 1951-1980 are analysed by means of EOF method.The findings are:(1) In the cold and warm ocean current areas,such as the North Pacific Current,the California Current and the Equatorial East Pacific areas,the convergence speeds are the fastest,while in the Kuroshio and the western part of the North Equatorial Current areas they are fast only in winter.(2) The physical features of the first 3 eigenvectors are obvious.The first eigenvector shows that the SST values are high in the south and low in the north in the latitudinal distribution of the SST field.The warm current area,i.e.the northwestern part of the North Pacific is positive and the cold current area,i.e.the southeastern part of the North Pacific including the Eastern Equatorial Pacific is negative.The zero line of the 2nd eigenvector field runs from northeast to southwest,in the same direction as the 1st term.For the 3rd eigenvector field,the role of the Kuroshio area is striking.The sign of components of this eigenvector is negative in the north,the North Pacific Current area; on the contrary,the other 3 ocean current areas show positive.The Central Pacific is weakly negative.(3) The characteristics of the annual variation of the monthly SST are obtained from analyses of time amplitude coefficients associated with eigenvectors.There are quasi-periodic oscillations of 5-6 years in the 1950's and early 1960's,while 2-3 years in the 1960's and 1970's.These characteristics affect the interannual variation of East Asia climate.
Keywords:
本文献已被 CNKI 等数据库收录!
点击此处可从《海洋学报(英文版)》浏览原始摘要信息
点击此处可从《海洋学报(英文版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号