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Biological response to typhoon in northern South China Sea: A case study of "Koppu"
[Liu, Huaxue; Hu, Zifeng; Huang, Liangmin; Song, Xingyu; Ke, Zhixin; Zhou, Linbin] Chinese Acad Sci, South China Sea Inst Oceanol, Lab Marine Bioresource Sustainable Utilizat, Guangzhou 510301, Guangdong, Peoples R China; Huang, Honghui; Chen, Zuozhi] Chinese Acad Fisheries Sci, South China Sea Fisheries Res Inst, Guangzhou 510300, Guangdong, Peoples R China; [Song, Xingyu] Chinese Acad Sci, Marine Biol Res Stn Daya Bay, Shenzhen 518121, Peoples R China; songxy@scsio.ac.cn
2013
Source PublicationCONTINENTAL SHELF RESEARCH
ISSN0278-4343
Volume68Pages:123-132
AbstractObviously increased phytoplankton biomass and primary production was observed via both in situ investigation and remote sensing analysis in the northern South China Sea during typhoon Koppu's intrusion in September 2009. Sea surface temperature declined in both coastal and offshore area when Koppu arrived. In the offshore waters, stratification was weakened due to vertical mixing and sea surface temperature distribution pattern changed after the Koppu's arrival. The in situ data showed that extreme high primary production (PP) value (35 mgC m(-3) h(-1)) appeared near the Dan'gan Island indicating a potential algal bloom around the southern coastal waters of Hong Kong. Obviously increased nutrient loadings were also observed in the near-shore surface waters shortly after the typhoon's arrival. According to both in situ observation and remote sensing results, it is suggested that PP in the offshore water was stimulated by extra vertical nutrient transport induced by Koppu; while the enhanced phytoplankton biomass and potential bloom along the coastal was mostly contributed by the increased Pearl River discharge after rainfall, which was also regulated by the typhoon event. (C) 2013 Elsevier Ltd. All rights reserved.
DepartmentLMB
KeywordBloom Typhoon South China Sea
Subject AreaOceanography
Funding OrganizationThis research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support. ; This research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support. ; This research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support. ; This research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support.
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Language英语
Funding OrganizationThis research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support. ; This research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support. ; This research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support. ; This research was supported by the CAS Strategic Pilot Science and Technology under contract No. XDA10020200 and XDA05030403; the National Project of basic Sciences and Technology under contract No. 2012FY112400 and 2013FY111200; the Financial Fund of the Ministry of Agriculture (NO.NFZX2013); the Special Fund of Basic Research for Centre Commonweal Scientific Research Institute (NO. 2013TS07); and the National Nature Science Foundation of China (41276161, 41130855 and 41276162). The in situ research work was supported by the South China Sea Open Cruise by R/V Shiyan 3, South China Sea Institute of Oceanology, CAS. The authors thank the Hong Kong Environmental Protection Department, the Hong Kong Observatory and the NASA's Ocean Color Working Group for their data support.
WOS IDWOS:000327169700011
Citation statistics
Cited Times:4[WOS]   [WOS Record]     [Related Records in WOS]
Document Type期刊论文
Identifierhttp://ir.scsio.ac.cn/handle/344004/10980
Collection中科院海洋生物资源可持续利用重点实验室
Corresponding Authorsongxy@scsio.ac.cn
Recommended Citation
GB/T 7714
[Liu, Huaxue,Hu, Zifeng,Huang, Liangmin,et al. Biological response to typhoon in northern South China Sea: A case study of "Koppu"[J]. CONTINENTAL SHELF RESEARCH,2013,68:123-132.
APA [Liu, Huaxue.,Hu, Zifeng.,Huang, Liangmin.,Song, Xingyu.,Ke, Zhixin.,...&songxy@scsio.ac.cn.(2013).Biological response to typhoon in northern South China Sea: A case study of "Koppu".CONTINENTAL SHELF RESEARCH,68,123-132.
MLA [Liu, Huaxue,et al."Biological response to typhoon in northern South China Sea: A case study of "Koppu"".CONTINENTAL SHELF RESEARCH 68(2013):123-132.
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