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冬季北太平洋优势气候模态的转移
引用本文:吕庆平,张立凤,张铭.冬季北太平洋优势气候模态的转移[J].气候变化研究进展,2016,12(6):494-499.
作者姓名:吕庆平  张立凤  张铭
作者单位:1.解放军东海舰队司令部海洋水文气象中心,宁波 315122; 2 解放军理工大学气象海洋学院,南京 211101
基金项目:西北太平洋海洋多尺度变化过程、机理及可预报性
摘    要:采用EOF分解和小波分析,并引入相似度,分析冬季北太平洋的两个主要气候模态,即太平洋年代际振荡(PDO)模态与北太平洋涡旋振荡(NPGO)模态,及其结构特征随时间的演变。结果表明:1988/1989年的气候转移后,冬季海温距平(SSTA)优势模态为NPGO模态的年份越来越多,这种优势气候模态的转移现象表现出准18 a的年代际周期;SSTA与NPGO模态相似度的20年滑动平均在20世纪80年代中后期之后超过了SSTA与PDO模态的相应值,这表明此后SSTA的优势模态发生了转移,由PDO型转换为NPGO型;对典型时间段SSTA的合成分析显示,其优势模态由1988年前的PDO型转变为之后的NPGO型。

关 键 词:北太平洋  SSTA  优势气候模态  气候模态转移  
收稿时间:2016-03-15
修稿时间:2016-07-25

The Climate Shift of the Dominant Modes of North Pacific During Winter
Lü Qingping,Zhang Lifeng,Zhang Ming.The Climate Shift of the Dominant Modes of North Pacific During Winter[J].Advances in Climate Change,2016,12(6):494-499.
Authors:Lü Qingping  Zhang Lifeng  Zhang Ming
Institution:1.Oceanography and Meteorology Center, China People’s Liberation Army East Sea Fleet, Ningbo 315122, China; 2.College of Meteorology and Oceanography, China People’s Liberation Army University of Science and Technology, Nanjing 211101, China
Abstract:Empirical Orthogonal Function (EOF), wavelet analysis and resemblance analysis methods were used to research the variation of the structure feature of Pacific Decadal Oscillation (PDO) mode and North Pacific Gyre Oscillation (NPGO) mode. The spatial similarity coefficients between the Sea Surface Temperature Anomaly (SSTA) and the PDO mode, NPGO mode were computed separately. The results show that the spatial field of SSTA was more and more similar to that of the NPGO mode after 1988/1989, and the climate shift had a period of 18 years. Then, the 20-year moving average of the two similarity coefficients show that the latter one was greater than the former after 1984, which meant that the spatial shift of SSTA occurred about 1984. Lastly, the spatial feature of the averaged SSTA of some special periods also show that the structure feature of SSTA became NPGO-like mode from PDO-like mode after the 1980s.
Keywords:North Pacific  SSTA  dominant climate mode  climate shift  
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