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 |
ISSN | 0254-4059 |
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 | |
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 |
推荐引用方式 GB/T 7714 | 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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