Mesoscale structure of the central South China Sea detected by SCSMEX Buoy and Argo float
Zeng Lili1; Wang Dongxiao1; Du Yan1; Shi Ping1,2
发表期刊CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY
ISSN0254-4059
2010-09-01
卷号28期号:5页码:1102-1111
关键词South China Sea (Scs) Upper Ocean Water Mass Argo Floats Scsmex Buoy
产权排序[Zeng Lili; Wang Dongxiao; Du Yan; Shi Ping] Chinese Acad Sci, Key Lab Trop Marine Environm Dynam, S China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China; [Shi Ping] Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
通讯作者Du, Y, Chinese Acad Sci, Key Lab Trop Marine Environm Dynam, S China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China
作者部门信息集成与应用实验室 
英文摘要We addressed the mesoscale structure variation of the central South China Sea (SCS) with the measurements by a long-lived Argo float and a high-resolution ATLAS buoy during 1998-2002. T-S diagram indicates cooling and freshening events in 2000 and 2001 with lower salinity (0.5-0.8) and lower temperature (1-1.7A degrees C). Significant decrease in the net heat flux and increase in the precipitation suggest that the cooling and freshening is due to extra forcing by the atmosphere. Additional to large year-to-year changes, intraseasonal variability is moderate in the research area. The axis of the maximum intraseasonal temperature and salinity signals are mainly located on the thermocline. Typically, amplitude and period of intraseasonal temperature is about 2A degrees C and 40-60 days, and that of salinity is 0.3-0.5 and 35-60 days. Rapidly-changing winds, heat flux, and precipitation are critical in controlling the intraseasonal fluctuations of the mixed layer of the area. Studies on heat and freshwater balance in the mixed-layer further suggest that horizontal advection plays an important role in intraseasonal fluctuation in the upper ocean. In addition, the energetic mesoscale propagation radiated from the east boundary is linked to the intraseasonal variability in winter.; We addressed the mesoscale structure variation of the central South China Sea (SCS) with the measurements by a long-lived Argo float and a high-resolution ATLAS buoy during 1998-2002. T-S diagram indicates cooling and freshening events in 2000 and 2001 with lower salinity (0.5-0.8) and lower temperature (1-1.7A degrees C). Significant decrease in the net heat flux and increase in the precipitation suggest that the cooling and freshening is due to extra forcing by the atmosphere. Additional to large year-to-year changes, intraseasonal variability is moderate in the research area. The axis of the maximum intraseasonal temperature and salinity signals are mainly located on the thermocline. Typically, amplitude and period of intraseasonal temperature is about 2A degrees C and 40-60 days, and that of salinity is 0.3-0.5 and 35-60 days. Rapidly-changing winds, heat flux, and precipitation are critical in controlling the intraseasonal fluctuations of the mixed layer of the area. Studies on heat and freshwater balance in the mixed-layer further suggest that horizontal advection plays an important role in intraseasonal fluctuation in the upper ocean. In addition, the energetic mesoscale propagation radiated from the east boundary is linked to the intraseasonal variability in winter.
文章类型Article
资助机构Chinese Academy of Sciences [KZCX1-YW-12-01, KZCX2-YW-BR-04, SQ200916, SQ200809]; National Natural Science Foundation of China [40806003]; National High Technology Research and Development Program of China [2008AA09A402]
收录类别SCI
语种英语
关键词[WOS]NORTH PACIFIC ; MODE WATER ; LAYER ; VARIABILITY ; ALGORITHM
研究领域[WOS]Marine & Freshwater Biology ; Oceanography
WOS记录号WOS:000281711600020
引用统计
被引频次:6[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.yic.ac.cn/handle/133337/3809
专题中国科学院海岸带环境过程与生态修复重点实验室_海岸带信息集成与战略规划研究中心
作者单位1.Chinese Acad Sci, Key Lab Trop Marine Environm Dynam, S China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China
2.Chinese Acad Sci, Yantai Inst Coastal Zone Res, Yantai 264003, Peoples R China
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Zeng Lili,Wang Dongxiao,Du Yan,et al. Mesoscale structure of the central South China Sea detected by SCSMEX Buoy and Argo float[J]. CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,2010,28(5):1102-1111.
APA Zeng Lili,Wang Dongxiao,Du Yan,&Shi Ping.(2010).Mesoscale structure of the central South China Sea detected by SCSMEX Buoy and Argo float.CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY,28(5),1102-1111.
MLA Zeng Lili,et al."Mesoscale structure of the central South China Sea detected by SCSMEX Buoy and Argo float".CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY 28.5(2010):1102-1111.
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