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学科主题: Oceanography
题名: Interannual variability of mixed layer depth and heat storage of upper layer in the tropical Pacific Ocean
作者: Lin, YH ; You, XB ; Guan, YP
通讯作者: linyh@lasg.iap.ac.cn
关键词: interannual variability ; heat storage ; mixed layer depth ; tropical Pacific Ocean
刊名: ACTA OCEANOLOGICA SINICA
发表日期: 2004
卷: 23, 期:1, 页:31-39
收录类别: sci
部门归属: Chinese Acad Sci, LASG, Inst Atmospher Phys, Beijing 100029, Peoples R China; Chinese Acad Sci, S China Sea Inst Oceanol, Guangzhou 510301, Peoples R China
项目归属: LED
摘要: By using the upper layer data (downloaded from the web of the Scripps Institution of Oceanography),the interannual variability of the heat storage of upper layer(from surface to 400 in depth) and the mixed layer depth in the tropical Pacific Ocean are investigated. The abnormal signal of the warm event comes from the central and west Pacific Ocean, whereas it is regarded that the abnormal signal of the warm event comes from the east Pacific Ocean in the popular viewpoint. From the viewpoint on the evolution of the interannual variability of the mixed layer depth and the heat storage of the whole upper layer, the difference between the two types of El Nino is so small that it can be neglected. During these two El Nino/La Nina events(1972/1973 and 1997/1998), other than the case of the heat storage or for the mixed layer depth, the abnormal signal propagates from the central and west Pacific Ocean to the east usually by the path along the equator whereas the abnormal signal propagates from the east to the west by the path northern to the equator. For the interannual variability, the evolution of the mixed layer depth corresponds to that of the heat storage in the upper layer very well. This is quite different from the evolution of seasonality.
原文出处: 查看原文
WOS记录号: WOS:000220678300004
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内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/5649
Appears in Collections:热带海洋环境动力实验室(LTO)_期刊论文

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Recommended Citation:
Lin, YH; You, XB; Guan, YP.Interannual variability of mixed layer depth and heat storage of upper layer in the tropical Pacific Ocean,ACTA OCEANOLOGICA SINICA,2004,23(1):31-39
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