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学科主题: Oceanography
题名: Mean seasonal cycle of isothermal depth in the South China Sea
作者: Qu, TD ; Du, Y ; Gan, JP ; Wang, DX
通讯作者: tangdong@hawaii.edu
刊名: JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
发表日期: 2007
卷: 112, 期:C2, 页:-
收录类别: sci
部门归属: Univ Hawaii Manoa, Int Pacific Res Ctr, SOEST, Honolulu, HI 96822 USA; Hong Kong Univ Sci & Technol, Dept Math & Atmospher, Marine & Coastal Environm Program, Kowloon, Hong Kong, Peoples R China; Chinese Acad Sci, Lab Trop Marine Environm Dynam, S China Sea Inst Oceanol, Guangzhou 510301, Peoples R China
项目归属: LED
摘要: [1] The mean seasonal cycle of isothermal depth is examined using all available temperature profiles in the South China Sea. On the annual average, the isothermal depth has two deep cores (> 45 m). One extends westward from the Luzon Strait along the continental slope south of China, and the other in the deep basin of the southern South China Sea. Harmonic analysis shows that the seasonal variation of isothermal depth is predominantly annual in the northern South China Sea, exceeding 70 m in winter and falling below 20 m in summer near the continental slope south of China. The annual variation is weaker in the southern South China Sea, where the isothermal depth approaches its seasonal maximum (> 55 m) in fall and minimum (< 35 m) in spring. The semiannual variation is most prominent in the southern South China Sea, being of comparable strength with the annual variation. Among others, local Ekman pumping appears to be an important process responsible for the semiannual variation in the southern South China Sea. A detailed description of the month-to-month variations is provided, to set a basic background for further understanding the South China Sea mixed layer dynamics and thermodynamics.
原文出处: 查看原文
WOS记录号: WOS:000244477600001
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内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/5907
Appears in Collections:热带海洋环境动力实验室(LTO)_期刊论文

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Qu, TD; Du, Y; Gan, JP; Wang, DX.Mean seasonal cycle of isothermal depth in the South China Sea,JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2007,112(C2):-
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