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Image of a subsurface current core in the southern South China Sea
[Tang, Q. S.; Yan, P.] Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China; [Wang, D. X.; Li, J.] Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China; [Li, J. B.] State Ocean Adm, Inst Oceanog 2, Key Lab Submarine Geosci, Hangzhou 310012, Zhejiang, Peoples R China; dxwang@scsio.ac.cn
2013
发表期刊OCEAN SCIENCE
ISSN1812-0784
卷号9期号:4页码:631-638
摘要A legacy seismic transect acquired on 30 and 31 May 2009 in the southern South China Sea (SCS) was reprocessed to reveal the thermohaline structure of the water column. In the study region, a mesoscale subsurface lens with extraordinary features was detected at 113.5 degrees E, 11.5 degrees N. It is centred at 450m depth, occupies both the subsurface and intermediate water from 250 to 600 m, and has an intersection diameter of around 60 km. The simulated results from Hybrid Coordinate Ocean Model reveal an eddy-induced subsurface current running southwestward along the deep basin edge and suggest that the imaged lens is a snapshot of the subsurface current core rather than a subsurface eddy.
部门归属海洋地质
学科领域Meteorology & Atmospheric Sciences ; Oceanography
资助者We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706). ; We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706). ; We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706). ; We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706).
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语种英语
资助者We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706). ; We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706). ; We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706). ; We thank the R/V Tanbao crew for the seismic data acquisition. We thank T. D. Qu for his helpful discussions. B. Ruddick and an anonymous reviewer are greatly acknowledged for their constructive comments and suggestions. The altimeter products were produced by Ssalto/Duacs and distributed by the AVISO, with support from the CNES (www.aviso.oceanobs.com/duacs). The HYCOM data are available from http://hycom.org/dataserver. This research is supported financially by the NSFC (Grants 41176026, 91228202, and 41006027) and the 973 Program (Grants 2007CB411700 and 2007CB411706).
WOS记录号WOS:000321611000004
引用统计
被引频次:5[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.scsio.ac.cn/handle/344004/11141
专题中科院边缘海地质重点实验室
通讯作者dxwang@scsio.ac.cn
推荐引用方式
GB/T 7714
[Tang, Q. S.,Yan, P.] Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China,[Wang, D. X.,et al. Image of a subsurface current core in the southern South China Sea[J]. OCEAN SCIENCE,2013,9(4):631-638.
APA [Tang, Q. S.,Yan, P.] Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou 510301, Guangdong, Peoples R China,[Wang, D. X.,Li, J.] Chinese Acad Sci, South China Sea Inst Oceanol, State Key Lab Trop Oceanog, Guangzhou 510301, Guangdong, Peoples R China,[Li, J. B.] State Ocean Adm, Inst Oceanog 2, Key Lab Submarine Geosci, Hangzhou 310012, Zhejiang, Peoples R China,&dxwang@scsio.ac.cn.(2013).Image of a subsurface current core in the southern South China Sea.OCEAN SCIENCE,9(4),631-638.
MLA [Tang, Q. S.,et al."Image of a subsurface current core in the southern South China Sea".OCEAN SCIENCE 9.4(2013):631-638.
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