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学科主题: Environmental Sciences; Geosciences, Multidisciplinary
题名: Seasonal phytoplankton blooms associated with monsoonal influences and coastal environments in the sea areas either side of the Indochina Peninsula
作者: Tang, DL ; Kawamura, H ; Shi, P ; Takahashi, W ; Guan, L ; Shimada, T ; Sakaida, F ; Isoguchi, O
通讯作者: lingzis@scsio.ac.cn ; kamu@ocean.caos.tohoku.ac.jp ; pshi@scsio.ac.cn ; wataru@janus.co.jp ; leiguan@orsi.ouc.edu.cn ; shimada@ocean.caos.tohoku.ac.jp ; toki@ocean.caos.tohoku.ac.jp ; guchi@ocean.caos.tohoku.ac.jp
刊名: JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
发表日期: 2006
卷: 111, 期:G1, 页:-
收录类别: sci
部门归属: Chinese Acad Sci, S Chiense Sea Inst Oceanol, Lab Trop Marine Environm Dynam, Guangzhou 510301, Peoples R China; Tohoku Univ, Grad Sch Sci, Ctr Atmospher & Ocean Studies, Sendai, Miyagi 8908578, Japan; Ocean Univ China, Ocean Remote Sensing Inst, Qingdao 266003, Peoples R China; NUS Co Ltd, Tokyo 1080022, Japan
项目归属: LED
摘要: The Gulf of Thailand (GoT) is a semienclosed sea on the west and southwest side of the Indochina Peninsula and connects with the near-coastal waters of the South China Sea (SCS) on the east and northeast side of the Malay Peninsula. The objective of the present study is to understand dynamic features of the phytoplankton biology in the GoT and the nearby SCS, on both sides of the Indochina Peninsula, using remote-sensing measurements of chlorophyll-a (Ch1 a), sea surface temperature (SST), and surface vector winds obtained during the period from September 1997 to March 2003. Results show that seasonal variations of the phytoplankton blooms are primarily controlled by the monsoonal winds and related coastal environments. The GoT and the near-coastal SCS have a peak in the averaged monthly Ch1 a in December and January, which is associated with the winter northeaster monsoon. The near-coastal SCS have another big peak in the averaged monthly Ch1 a in summer (July to September), which is associated with the summer southwest monsoon. The offshore bloom in the GoT occurs in its southern part and enhances the December-January peak of averaged monthly Ch1 a. By contrast, the offshore bloom in the nearby SCS is observed northeast of the Peninsula, and represents the primary source of the July-September peak Ch1 a. Here the coastal upwelling associated with the offshore Ekman transport caused by the coastal surface winds parallel to the Vietnam east coast gives physical conditions favorable to the development of offshore phytoplankton blooms. The Mekong River discharge waters flow in different directions, depending on the monsoon winds, and contributes to seasonal blooms on both sides of the Peninsula.
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WOS记录号: WOS:000240985900001
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内容类型: 期刊论文
URI标识: http://ir.scsio.ac.cn/handle/344004/5771
Appears in Collections:热带海洋环境动力实验室(LTO)_期刊论文

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Recommended Citation:
Tang, DL; Kawamura, H; Shi, P; Takahashi, W; Guan, L; Shimada, T; Sakaida, F; Isoguchi, O.Seasonal phytoplankton blooms associated with monsoonal influences and coastal environments in the sea areas either side of the Indochina Peninsula,JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES,2006,111(G1):-
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文件名: Seasonal phytoplankton blooms associated with monsoonal influences and coastal environments in the sea areas either side of the Indochina Peninsula .pdf
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