China's observation of dissolved oxygen in polar waters as a hydrological parameter
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- 英文论文题名：China's observation of dissolved oxygen in polar waters as a hydrological parameter
- 论文作者：Liu Na ; Lin Li'na ; Wang Yingjie ; Kong Bin ; He Yan
- 英文论文作者：Liu Na ; Lin Li'na ; Wang Yingjie ; Kong Bin ; He Yan ; The First Institute of Oceanography ; State Oceanic Administration ; Tongji University
- 年：2016
- 作者机构：The First Institute of Oceanography,State Oceanic Administration;Tongji University;
- 英文论文关键词：Chinese polar hydrological observation ; dissolved oxygen observation ; review
- 会议召开时间：2016-10-21
- 会议录名称：第八届海洋强国战略论坛论文集
- 语种：英文
- 分类号：P734
- 学会代码：EGVE
- 会议名称：第八届海洋强国战略论坛
- 会议地点：中国福建厦门
- 主办单位：中国海洋学会、中国太平洋学会
- 学会名称：中国海洋学会
- 页数：8
- 文件大小：609k
- 原文格式：O
- 会议级别：全国
摘要
Dissolved oxygen is a crucial indicator in water mass and circulation research,but it has not been given due emphasis in Chinese polar physical oceanographic observation and research.This article comprehensively discusses the observation of dissolved oxygen in polar waters as a hydrological parameter by Chinese researchers,aiming to introduce the observation of dissolved oxygen as part of regular polar hydrological investigation to enrich the hydrological data library.In this paper,we first introduce the significance of dissolved oxygen in hydrological observation.Then,China's observation and research status of dissolved oxygen in polar waters are summarized.Finally,some suggestions are provided for improving Chinese in situ observation and research of dissolved oxygen in polar waters,involving the acquisition of dissolved oxygen data by in situ observation,data post-processing and data correction.
Dissolved oxygen is a crucial indicator in water mass and circulation research,but it has not been given due emphasis in Chinese polar physical oceanographic observation and research.This article comprehensively discusses the observation of dissolved oxygen in polar waters as a hydrological parameter by Chinese researchers,aiming to introduce the observation of dissolved oxygen as part of regular polar hydrological investigation to enrich the hydrological data library.In this paper,we first introduce the significance of dissolved oxygen in hydrological observation.Then,China's observation and research status of dissolved oxygen in polar waters are summarized.Finally,some suggestions are provided for improving Chinese in situ observation and research of dissolved oxygen in polar waters,involving the acquisition of dissolved oxygen data by in situ observation,data post-processing and data correction.
Dissolved oxygen is a crucial indicator in water mass and circulation research,but it has not been given due emphasis in Chinese polar physical oceanographic observation and research.This article comprehensively discusses the observation of dissolved oxygen in polar waters as a hydrological parameter by Chinese researchers,aiming to introduce the observation of dissolved oxygen as part of regular polar hydrological investigation to enrich the hydrological data library.In this paper,we first introduce the significance of dissolved oxygen in hydrological observation.Then,China's observation and research status of dissolved oxygen in polar waters are summarized.Finally,some suggestions are provided for improving Chinese in situ observation and research of dissolved oxygen in polar waters,involving the acquisition of dissolved oxygen data by in situ observation,data post-processing and data correction.
引文
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[2]Reid J L.On the use of dissolved oxygen concentration as an indicator of winter convection[J].Naval Research Reviews,1982,34:28-38.
[3]Wyrtki K.The oxygen minima in relation to ocean circulation[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1962,9(1):11-23.
[4]Garcia H E,Boyer T P,Levitus S,et al.On the variability of dissolved oxygen andapparent oxygen utilization content for the upper world ocean;1955 to 1998[J].Geophysical Research Letters,2005,32(9):1-4.
[5]Keeling R,Garcia H.The change in oceanic O_2 inventory associated with recent global warming[J].Proceedings of the National Academy of Sciences,2002,99(12):7848-7853.
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[8]Li F R.On the relationship between the distribution of dissolved oxygen and water masses in the Yellow Sea and East China Sea late in spring[J].Journal of Ocean University of Qingdao,1995,25(2):255-263.
[9]Xiang Y T,Zheng X J,Tang G P.Distribution feature of dissolved oxygen in Kuroshio area of the East China Sea[J].Marine Environmental Science,1988,7(4):32-38.
[10]Jiang G C,Wang Y H.Dissolved oxygen and nutrient distribution in circulations of the East China Sea in winter[J].Marine Science Bulletin,1990,9(5):25-32.
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[13]Chen S T,Ruan W Q.Summer upwelling and saturation dissolved oxygen distribution in the Central and Northern Taiwan Strait[J].Journal of Oceanography in Taiwan Strait,1991,10(1):16-23.
[14]Lin J P.Calculating the velocity of coastal upwelling off Zhejiang Province using dissolved oxygen data[J].Marine Sciences,1985,9(1):24-28.
[15]Liu Y.Study on the Structures and the Kinetics Characteristics for the Subsurface and Intermediate Water Masses in the South China Sea[D].Qingdao:Ocean University of China,2010.
[16]Gordon A L.Potential temperature,oxygen and circulation of bottom water in the Southern Ocean[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1966,13(6):1125-1138.
[17]Jacobs S S,Amos A F,Bruchhausen P M.Ross Sea oceanography and Antarctic bottom water formation[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1970,17(6):935-962.
[18]Gordon A L,VisbeckM,Huber B.Export of Weddell Sea deep and bottom water[J].Journal of Geophysical Research:Oceans(1978-2012),2001,106(C5):9005-9017.
[19]Orsi A H,Methie W M,Bullister J L.On the total input of Antarctic waters to the deep ocean:A preliminary estimate from chlorofluorocarbon measurements[J].Journal of Geophysical Research:Oceans(1978-2012),2002,107(C8):31.
[20]Jacobs S S,Amos A F,Bruchhausen P M.Ross Sea oceanography and Antarctic bottom water formation[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1970,17(6):935-962.
[21]Foster T D,Carmack E C.Frontal zone mixing and Antarctic Bottom Water formation in the southern Weddell Sea[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1976,23(4):301-317.
[22]Williams G D,Bindoff N L,Marsland S J,et al.Formation and export of dense shelf water from the Adelie Depression,East Antarctica[J].Journal of Geophysical Research,2008,113(C4):C4039.
[23]Ohshima K I,Fukamachi Y,Williams G D,et al.Antarctic Bottom Water production by intense sea-ice formation in the Cape Damley polynya[J].Nature Geoscience,2013,6(3):235-240.
[24]Kitade Y,Shimada K,Tamura T,et al.Antarctic Bottom Water production from the Vincennes Bay Polynya,East Antarctica[J].Geophysical Research Letters,2014,41(10):3528-3534.
[25]Li F R.Distribution of oxygen-minimum layer and factors controlling on it in areas adjacent to South Shetlands and North of Adelaide,Antarctica,in summer[J].Chinese Journal of Polar Research,1989(4):21-27.
[26]Wang Y H,Dong H L,Ren D Y.The chemical characteristics of seawater in the Prydz Bay,Antarctica[J].Antarctic Research(Chinese edition),1993,5(4):83-89.
[27]Ren D Y.The maximum value of O_2 in the Prize Bay and its adjacent sea area[J].Donghai Marine Science,1995,13(1):53-60.
[28]Jin M M,Lin Y A,Lu Y,et al.Vertical features of nutrient and dissolved oxygen of the Bering basin in July 1999[J].Chinese Journal of Polar Research,2015(4):37-45.
[29]Gao G P,Dong Z Q,Shi M C.Water properties of the seas surveyed by Chinese first Arctic research expedition in summer,1999[J].Chinese Journal of Polar Research,2003,15(1):11-20.
[30]Pu S Z,Dong Z Q,Yu W D,et al.Features and spatial distributions of circumpolar deep water in the Southern Indian Ocean and effects of Antarctic circumpolar current[J].Advances in Marine Science,2007,25(1):1-8.
[31]Han Z B,Pan J M,Hu Z Y,et al.Decomposition of organic carbon and inorganic carbon beneath euphotic zone in Prydz Bay,Antarctica[J].Chinese Journal of Polar Research,2010,22(3):254-261.
[32]SunX,Lin C,Chen Y,et al.Distribution of dissolved oxygen and causes of maximum concentration in the Bering Sea in July 2010[J],Acta Oceanologica Sinica,2014,33(6):20-27.
[33]Ge R F,Yu F,Guo B H,et al.Discussion on the correction method for dissolved oxygen data observed by 911 Plus CTD System[J].Advances in Marine Science,2003,21(3):336-341.
[34]Chen L Q.The report of First Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2000.
[35]Zhang Z H.The report of Second Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2004.
[36]Zhang H S.The report of Third Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2009.
[37]Yu X G.The report of Fourth Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2011.
[38]Ma D Y.The report of Fifth Chinese Arctic Research Expedition(in Chinese)[M].Beijing;China Ocean Press,2013.
[39]Pan Z D.The report of Sixth Chinese Arctic Research Expedition(in Chinese)[M].Beijing;China Ocean Press,2016.
[40]Liu Q Y,Liu J,Guo J L.Determination of dissolved oxygen by spectrophotometry[J].Environmental Engineering,2008,26(5):92-94.
[2]Reid J L.On the use of dissolved oxygen concentration as an indicator of winter convection[J].Naval Research Reviews,1982,34:28-38.
[3]Wyrtki K.The oxygen minima in relation to ocean circulation[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1962,9(1):11-23.
[4]Garcia H E,Boyer T P,Levitus S,et al.On the variability of dissolved oxygen andapparent oxygen utilization content for the upper world ocean;1955 to 1998[J].Geophysical Research Letters,2005,32(9):1-4.
[5]Keeling R,Garcia H.The change in oceanic O_2 inventory associated with recent global warming[J].Proceedings of the National Academy of Sciences,2002,99(12):7848-7853.
[6]Joos F,Plattner G K,Stacker T F,et al.Trends in marine dissolved oxygen;Implications for ocean circulation changes and the carbon budget[J].Eos Trans.AGU,2003,84(21):197-201.
[7]Li F R.Study on the relationship between dissolved oxygen distribution and water masses in the Yellow Sea and East China Sea in late spring[J].Oceanologia et Limnologia Sinica(S),1995,26(5):47-53.
[8]Li F R.On the relationship between the distribution of dissolved oxygen and water masses in the Yellow Sea and East China Sea late in spring[J].Journal of Ocean University of Qingdao,1995,25(2):255-263.
[9]Xiang Y T,Zheng X J,Tang G P.Distribution feature of dissolved oxygen in Kuroshio area of the East China Sea[J].Marine Environmental Science,1988,7(4):32-38.
[10]Jiang G C,Wang Y H.Dissolved oxygen and nutrient distribution in circulations of the East China Sea in winter[J].Marine Science Bulletin,1990,9(5):25-32.
[11]Sheng T Q,Xu Y Z.Distribution of dissolved oxygen and pH in Kuroshio area of East China Sea[J].Marine Science Bulletin,1993,12(4):55-62.
[12]Chen S T,Ruan W Q.Characteristics of dissolved oxygen in summer at upwelling areas of Taiwan Strait[J].Tropic Oceanography,1992,11(3):29-36.
[13]Chen S T,Ruan W Q.Summer upwelling and saturation dissolved oxygen distribution in the Central and Northern Taiwan Strait[J].Journal of Oceanography in Taiwan Strait,1991,10(1):16-23.
[14]Lin J P.Calculating the velocity of coastal upwelling off Zhejiang Province using dissolved oxygen data[J].Marine Sciences,1985,9(1):24-28.
[15]Liu Y.Study on the Structures and the Kinetics Characteristics for the Subsurface and Intermediate Water Masses in the South China Sea[D].Qingdao:Ocean University of China,2010.
[16]Gordon A L.Potential temperature,oxygen and circulation of bottom water in the Southern Ocean[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1966,13(6):1125-1138.
[17]Jacobs S S,Amos A F,Bruchhausen P M.Ross Sea oceanography and Antarctic bottom water formation[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1970,17(6):935-962.
[18]Gordon A L,VisbeckM,Huber B.Export of Weddell Sea deep and bottom water[J].Journal of Geophysical Research:Oceans(1978-2012),2001,106(C5):9005-9017.
[19]Orsi A H,Methie W M,Bullister J L.On the total input of Antarctic waters to the deep ocean:A preliminary estimate from chlorofluorocarbon measurements[J].Journal of Geophysical Research:Oceans(1978-2012),2002,107(C8):31.
[20]Jacobs S S,Amos A F,Bruchhausen P M.Ross Sea oceanography and Antarctic bottom water formation[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1970,17(6):935-962.
[21]Foster T D,Carmack E C.Frontal zone mixing and Antarctic Bottom Water formation in the southern Weddell Sea[C]//Deep Sea Research and Oceanographic Abstracts.Elsevier,1976,23(4):301-317.
[22]Williams G D,Bindoff N L,Marsland S J,et al.Formation and export of dense shelf water from the Adelie Depression,East Antarctica[J].Journal of Geophysical Research,2008,113(C4):C4039.
[23]Ohshima K I,Fukamachi Y,Williams G D,et al.Antarctic Bottom Water production by intense sea-ice formation in the Cape Damley polynya[J].Nature Geoscience,2013,6(3):235-240.
[24]Kitade Y,Shimada K,Tamura T,et al.Antarctic Bottom Water production from the Vincennes Bay Polynya,East Antarctica[J].Geophysical Research Letters,2014,41(10):3528-3534.
[25]Li F R.Distribution of oxygen-minimum layer and factors controlling on it in areas adjacent to South Shetlands and North of Adelaide,Antarctica,in summer[J].Chinese Journal of Polar Research,1989(4):21-27.
[26]Wang Y H,Dong H L,Ren D Y.The chemical characteristics of seawater in the Prydz Bay,Antarctica[J].Antarctic Research(Chinese edition),1993,5(4):83-89.
[27]Ren D Y.The maximum value of O_2 in the Prize Bay and its adjacent sea area[J].Donghai Marine Science,1995,13(1):53-60.
[28]Jin M M,Lin Y A,Lu Y,et al.Vertical features of nutrient and dissolved oxygen of the Bering basin in July 1999[J].Chinese Journal of Polar Research,2015(4):37-45.
[29]Gao G P,Dong Z Q,Shi M C.Water properties of the seas surveyed by Chinese first Arctic research expedition in summer,1999[J].Chinese Journal of Polar Research,2003,15(1):11-20.
[30]Pu S Z,Dong Z Q,Yu W D,et al.Features and spatial distributions of circumpolar deep water in the Southern Indian Ocean and effects of Antarctic circumpolar current[J].Advances in Marine Science,2007,25(1):1-8.
[31]Han Z B,Pan J M,Hu Z Y,et al.Decomposition of organic carbon and inorganic carbon beneath euphotic zone in Prydz Bay,Antarctica[J].Chinese Journal of Polar Research,2010,22(3):254-261.
[32]SunX,Lin C,Chen Y,et al.Distribution of dissolved oxygen and causes of maximum concentration in the Bering Sea in July 2010[J],Acta Oceanologica Sinica,2014,33(6):20-27.
[33]Ge R F,Yu F,Guo B H,et al.Discussion on the correction method for dissolved oxygen data observed by 911 Plus CTD System[J].Advances in Marine Science,2003,21(3):336-341.
[34]Chen L Q.The report of First Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2000.
[35]Zhang Z H.The report of Second Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2004.
[36]Zhang H S.The report of Third Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2009.
[37]Yu X G.The report of Fourth Chinese Arctic Research Expedition(in Chinese)[M].Beijing:China Ocean Press,2011.
[38]Ma D Y.The report of Fifth Chinese Arctic Research Expedition(in Chinese)[M].Beijing;China Ocean Press,2013.
[39]Pan Z D.The report of Sixth Chinese Arctic Research Expedition(in Chinese)[M].Beijing;China Ocean Press,2016.
[40]Liu Q Y,Liu J,Guo J L.Determination of dissolved oxygen by spectrophotometry[J].Environmental Engineering,2008,26(5):92-94.