中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
The regime shift in the 1960s and associated atmospheric change over the southern Indian Ocean

文献类型:期刊论文

作者Wang, TY; Du, Y; Liao, XM
刊名ACTA OCEANOLOGICA SINICA
出版日期2017
卷号36期号:1页码:1-8
关键词sea surface temperature regime shift southern Indian Ocean interdecadal variabilities linear trend
通讯作者duyan@scsio.ac.cn
中文摘要The change of sea surface temperature (SST) in the southern Indian Ocean (SIO) during the recent six decades has been analyzed based on oceanic reanalysis and model, as well as atmospheric data. The results show that a thermal regime shift in SIO during the 1960s, which is not caught enough attentions, has been of equal magnitude to the linear warming since 1970. Empirical Orthogonal Function (EOF) analyses reveal that a thermal shift is combined with atmospheric changes such as the weakening of westerly during the period of 1960-1967. Inner dynamic connections can be defined that when the westerly winds turn weak, the anticyclonic wind circulation between westerly winds and the trade winds decreases, which further reduces the SST to a negative peak in this period. It is noted that the shifts in the 1960s are also evident for Southern Hemisphere. For example, subtropical high and the entire westerly winds belt at high latitudes both change dramatically in the 1960s. This large-scaled process maybe link to the change of southern annular mode (SAM).
源URL[http://ir.scsio.ac.cn/handle/344004/16421]  
专题南海海洋研究所_热带海洋环境国家重点实验室(LTO)
推荐引用方式
GB/T 7714
Wang, TY,Du, Y,Liao, XM. The regime shift in the 1960s and associated atmospheric change over the southern Indian Ocean[J]. ACTA OCEANOLOGICA SINICA,2017,36(1):1-8.
APA Wang, TY,Du, Y,&Liao, XM.(2017).The regime shift in the 1960s and associated atmospheric change over the southern Indian Ocean.ACTA OCEANOLOGICA SINICA,36(1),1-8.
MLA Wang, TY,et al."The regime shift in the 1960s and associated atmospheric change over the southern Indian Ocean".ACTA OCEANOLOGICA SINICA 36.1(2017):1-8.

入库方式: OAI收割

来源:南海海洋研究所

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