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学科主题: Limnology; Oceanography
题名: A dipole wind curl pattern induced by Taiwan Island and its effect on upper stratification in the northeastern South China Sea
作者: Deng, Y ; Shi, P ; Zhou, W ; Du, Y ; Xie, Q ; Zhuang, W ; Wang, DX
通讯作者: dxwang@scsio.ac.cn
关键词: Taiwan Island ; dipole wind stress curl ; mixed layer depth ; thermocline
刊名: CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
发表日期: 2012
卷: 30, 期:6, 页:944-952
部门归属: [Deng Yi; Shi Ping; Du Yan; Xie Qiang; Zhuang Wei; Wang Dongxiao] Chinese Acad Sci, State Key Lab Trop Oceanog, S China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China; [Zhou Wen] City Univ Hong Kong, Guy Carpenter Asia Pacific Climate Impact Ctr, Sch Energy & Environm, Hong Kong, Hong Kong, Peoples R China; [Xie Qiang] Chinese Acad Sci, Sanya Inst Deep Sea Sci & Engn, Sanya 572000, Peoples R China
项目归属: LTO
摘要: Using hydrographic data sampled during four successive late summer-early autumn cruises in 2004-2007, vertical stratification along transects in the lee of Taiwan Island was analyzed to investigate upper ocean responses to orographically induced dipole wind stress curl (WSC). Results indicate that mixed-layer depth (MLD) and its relationship with thermocline depth varied under different local wind forcings. Average MLD along the transects from the 2004 to 2007 cruises were 18.5, 30.7, 39.2 and 24.5 m, respectively. The MLD along the transects deepened remarkably and resulted in thermocline ventilation in 2005 and 2006, whereas ventilation did not occur in 2004 and 2007. Estimates indicate that frictional wind speed was the major factor in MLD variations. To a large degree, the combined effects of frictional wind speed and Ekman pumping are responsible for the spatial pattern of MLD during the cruises.
语种: 英语
WOS记录号: WOS:000311286500005
Citation statistics:
内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/10055
Appears in Collections:热带海洋环境国家重点实验室(LTO)_期刊论文

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Recommended Citation:
Deng, Y; Shi, P; Zhou, W; Du, Y; Xie, Q; Zhuang, W; Wang, DX.A dipole wind curl pattern induced by Taiwan Island and its effect on upper stratification in the northeastern South China Sea,CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2012,30(6):944-952
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