Volume 12 Issue 4
Aug.  2016
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YU Jie, CHEN Guobao, ZHANG Kui, CHEN Zuozhi. Vertical distribution of summer chlorophyll a concentration in the middle South China Sea[J]. South China Fisheries Science, 2016, 12(4): 1-8. DOI: 10.3969/j.issn.2095-0780.2016.04.001
Citation: YU Jie, CHEN Guobao, ZHANG Kui, CHEN Zuozhi. Vertical distribution of summer chlorophyll a concentration in the middle South China Sea[J]. South China Fisheries Science, 2016, 12(4): 1-8. DOI: 10.3969/j.issn.2095-0780.2016.04.001
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Vertical distribution of summer chlorophyll a concentration in the middle South China Sea

  • Key Lab. of South China Sea Fishery Resources Exploitation & Utilization, Ministry of Agriculture; Scientific Observing and Experimental Station of South China Sea Fishery Resources & Environments, Ministry of Agriculture; South China Sea Fisheries Research Institute, Chinese Academy of Fishery Sciences, Guangzhou 510300, China

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  • Received Date: January 26, 2016
  • Revised Date: March 24, 2016
    Graphical Abstract
    • Abstract

  • We investigated the chlorophyll a (Chl-a) concentration in the middle South China Sea (12°N~18°N, 110°E~117°E) in July and August 2014 to provide valuable data for the study of vertical distribution of Chl-a. The results show that: 1) Chl-a in the middle South China Sea increased first and then decreased in depth. High concentration accumulated in depth of 30~70 m. 2) At subsurface layer, the maximum of Chl-a (SCM) intensity varied from 0.94 mg·m-3to 4.69 mg·m-3 with an average of 1.90 mg·m-3, which was 18.10 times compared with satellite surface Chl-a. SCM depth varied from 4 m to 75.36 m. SCM thickness varied from 19.01 m to 80.36 m. 3) The upwelling had great effect on the vertical distribution of Chl-a according to the distribution characteristics in Transect A and B. Coastal upwelling in Transect A showed the greatest intensity, smallest depth and largest thickness of SCM, while Zhongsha Islands upwelling in Transect B showed the greatest intensity, smallest depth and thickness.

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  • [1]
    郝锵, 宁修仁, 刘诚刚, 等. 南海北部初级生产力遥感反演及其环境调控机制[J]. 海洋学报(中文版), 2007, 29(3): 58-68. https://www.cnki.com.cn/Article/CJFDTOTAL-SEAC200703007.htm
    [2]
    毛志华, 朱乾坤, 龚芳. 卫星遥感北太平洋渔场叶绿素a浓度[J]. 水产学报, 2005, 29(2): 270-274. https://www.cnki.com.cn/Article/CJFDTOTAL-SCKX200502022.htm
    [3]
    李婷. 基于长时序遥感数据和EOF分析南海北部海表叶绿素-a时空特征[D]. 北京: 中国地质大学, 2013: 1-72. https://xueshu.baidu.com/usercenter/paper/show?paperid=69801e8374bc85af9a34930b69178ac5&site=xueshu_se&hitarticle=1
    [4]
    郝锵, 宁修仁, 蔡昱明, 等. 南海北部初级生产力的物理-生物海洋学耦合特征及其对固碳量的影响[J]. 海洋学研究, 2011, 29(2): 46-57. doi: 10.3969/j.issn.1001-909X.2011.02.005
    [5]
    TANG D L, KAWAMURA H, DOAN-NHU H, et al. Remote sensing oceanography of a harmful algal bloom off the coast of southeastern Vietnam[J]. J Geophys Res-Oceans, 2004, 109(C3): 1-7. https://xueshu.baidu.com/usercenter/paper/show?paperid=958c2649aaf8a1f55157559b69cbae0d&site=xueshu_se&hitarticle=1
    [6]
    王磊, 林丽贞, 谢聿原, 等. 冬季东海及南海北部海域初级生产力和新生产力的初步研究[J]. 海洋学研究, 2012, 30(1): 59-66. doi: 10.3969/j.issn.1001-909X.2012.01.008
    [7]
    高姗. 基于遥感的南海初级生产力时空变化特征与环境影响因素研究[D]. 北京: 中国气象科学研究院, 2008: 1-68. https://xueshu.baidu.com/usercenter/paper/show?paperid=b8da95468117fd1b36522e3c49c59f80&site=xueshu_se&hitarticle=1
    [8]
    宫响. 南海北部次表层叶绿素最大值特征的理论分析及数值模拟研究[D]. 青岛: 中国海洋大学, 2012: 1-164. https://cdmd.cnki.com.cn/Article/CDMD-10423-1012505760.htm
    [9]
    WANG J J, TANG D L. Phytoplankton patchiness during spring intermonsoon in western coast of South China Sea[J]. Deep-Sea Res Ⅱ, 2014, 101(3): 120-128. https://xueshu.baidu.com/usercenter/paper/show?paperid=dc1273e74d5c4f13aecb48eac7f78c0e&site=xueshu_se&hitarticle=1
    [10]
    陈兴群, 陈其焕, 庄亮钟. 南海中部叶绿素a分布和光合作用及其与环境因子的关系[J]. 海洋学报(中文版), 1989, 11(3): 349-355. https://www.cnki.com.cn/Article/CJFDTOTAL-SEAC198903010.htm
    [11]
    TAKAHASHI M, HORI T. Abundance of picphytoplankton in the subsurface chlorophyll maximum layer in subtropical and tropical waters[J]. Mar Biol, 1984, 79(2): 177-186. doi: 10.1007/BF00951826
    [12]
    马超, 吴德星, 鞠霞. 利用Argos浮标资料对黑潮入侵南海问题的分析[J]. 海洋湖沼通报, 2010(2): 1-5. doi: 10.3969/j.issn.1003-6482.2010.02.001
    [13]
    刘华雪, 宋星宇, 黄洪辉, 等. 典型低纬度海区(南海、孟加拉湾)初级生产力比较[J]. 生态学报, 2012, 32(18): 5900-5906. https://www.cnki.com.cn/Article/CJFDTOTAL-STXB201218033.htm
    [14]
    张鹏, 曾晓光, 杨吝, 等. 南海区大型灯光罩网渔场渔期和渔获组成分析[J]. 南方水产科学, 2013, 9(3): 74-79. doi: 10.3969/j.issn.2095-0780.2013.03.012
    [15]
    邹建伟, 陈立峰, 林蒋进, 等. 南海外海灯光罩网主要渔场分布及变动研究——基于广西渔船的生产监测统计[J]. 南方水产科学, 2014, 10(4): 78-84. doi: 10.3969/j.issn.2095-0780.2014.04.013
    [16]
    GONG X, SHI J, GAO H W, et al. Steady-state solutions for subsurface chlorophyll maximum instratified water columns with a bell-shaped vertical profile of chlorophyll[J]. Biogeosciences, 2015, 12(6): 905-919. https://xueshu.baidu.com/usercenter/paper/show?paperid=97a5f7211dfa71ea9212d34bae84dd68&site=xueshu_se&hitarticle=1
    [17]
    PÉREZ V, FERNÁNDEZ E, MARAÑÓN E, et al. Vertical distribution of phytoplankton biomass, production and growth in the Atlantic subtropical gyres[J]. Deep-Sea Res Ⅰ, 2006, 53(10): 1616-1634. doi: 10.1016/j.dsr.2006.07.008
    [18]
    PRAIRIE J C, FEANKS P S, JAFFE J S, et al. Physical and biological controls of vertical gradients in phytoplankton[J]. Limnol Oceanogr, 2011(1): 75-90. https://xueshu.baidu.com/usercenter/paper/show?paperid=509436cab4de1abf9e64d350cdfa5928&site=xueshu_se&hitarticle=1
    [19]
    HANSON C E, PESANT S, WAITE A M, et al. Assessing the magnitude and significance of deep chlorophyll maxima of the coastal eastern Indian Ocean[J]. Deep-Sea Res Ⅱ, 2007, 54(8/9/10): 884-901. https://xueshu.baidu.com/usercenter/paper/show?paperid=1n2p0t20191p0rr05a520vd0k4357892&site=xueshu_se&hitarticle=1
    [20]
    武扬, 程国胜. 南海混合层深度的季节和年际变化特征[J]. 海洋预报, 2013, 30(3): 9-17. https://www.cnki.com.cn/Article/CJFDTOTAL-HYYB201303002.htm
    [21]
    吴荣军, 吕瑞华, 朱明远, 等. 海水混合和层化对叶绿素a垂直分布的影响[J]. 生态环境, 2004, 13(4): 515-519. https://www.cnki.com.cn/Article/CJFDTOTAL-TRYJ20040400D.htm
    [22]
    许艳苹. 南海西部冷涡区域上层海洋营养盐的动力学[D]. 厦门: 厦门大学, 2009: 1-95. https://cdmd.cnki.com.cn/Article/CDMD-10384-2009181029.htm
    [23]
    李敏. 南海海洋叶绿素a时空分布及对季风变动响应的研究[D]. 北京: 中国气象科学研究院, 2009: 1-57.
    [24]
    黄良民. 南海不同海区叶绿素a和海水荧光值的垂向变化[J]. 热带海洋, 1992, 11(4): 89-95. https://www.cnki.com.cn/Article/CJFDTOTAL-RDHY199204013.htm
    [25]
    柯志新, 黄良民, 谭烨辉, 等. 2008年夏末南海北部叶绿素a的空间分布特征及其影响因素[J]. 热带海洋学报, 2013, 32(4): 51-57. https://www.cnki.com.cn/Article/CJFDTOTAL-RDHY201304008.htm
    [26]
    宫响, 史洁, 高会旺. 海洋次表层叶绿素最大值的特征因子及其影响因素[J]. 地球科学进展, 2012, 27(5): 539-548. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ201205005.htm
    [27]
    倪晓波, 黄大吉. 海洋次表层叶绿素最大值的分布和形成机制研究[J]. 海洋科学, 2006, 30(5): 58-64, 70. https://www.cnki.com.cn/Article/CJFDTOTAL-HYKX200605011.htm
    [28]
    唐世林, 陈楚群, 詹海刚, 等. 南海真光层深度的遥感反演[J]. 热带海洋学报, 2007, 26(1): 9-15. https://www.cnki.com.cn/Article/CJFDTOTAL-RDHY200701001.htm
    [29]
    于杰, 王新星, 李永振, 等. 南海中西部渔场上升流时空变化特征分析[J]. 海洋科学, 2015, 39(6): 104-113. https://www.cnki.com.cn/Article/CJFDTOTAL-HYKX201506016.htm
    [30]
    YANG Y J, XIAN T, SUN L, et al. Summer monsoon impacts on chlorophyll-a concentration in the middle of the South China Sea: climatological mean and annual variability[J]. Atmos Ocean Sci Lett, 2012, 5(1): 15-19.
    [31]
    XIE S P, XIE Q, WANG D X, et al. Summer upwelling in the South China Sea and its role in regional climate variations[J]. J Geogr Res, 2003, 108(C8): 1-13. https://xueshu.baidu.com/usercenter/paper/show?paperid=9fbf21632a051c789b9c3a4698bb6a55&site=xueshu_se&hitarticle=1
    [32]
    KUO N J, ZHENG Q A, HO C R. Satellite observation of upwelling along the western coast of the South China Sea[J]. Remote Sens Environ, 2000, 74(3): 463-470. https://xueshu.baidu.com/usercenter/paper/show?paperid=c619d6a9652000231248922cdde43854&site=xueshu_se&hitarticle=1
    [33]
    AN N T, THU P M. Biogeochemical variability of Vietnamese coastal waters influenced by natural and anthropogenic processes[J]. Asian J Water Environ Poll, 2006, 4(1): 37-46. https://xueshu.baidu.com/usercenter/paper/show?paperid=1u2x0v20691e0vj00r4b0680t3066962&site=xueshu_se&hitarticle=1
    [34]
    XUE H J, CHAI F, PETTIGREW N, et al. Kuroshio intrusion and the circulation in the South China Sea[J]. J Geophys Res-Oceans, 2004, 109(C2): 1-14. https://xueshu.baidu.com/usercenter/paper/show?paperid=fb93120c97188647788a97170388910e&site=xueshu_se&hitarticle=1
    [35]
    TANG D L, KAWAMURA H, van DIEN T, et al. Offshore phytoplankton biomass increase and its oceanographic causes in the South China Sea[J]. Mar Ecol Prog Ser, 2004, 268(1): 31-41. https://xueshu.baidu.com/usercenter/paper/show?paperid=186c628ab1f4440651298c71ff05cf67&site=xueshu_se
    [36]
    LIU K K, CHAO S Y, SHAW P T, et al. Monsoon-forced chlorophyll distribution and primary production in the South China Sea: observations and a numerical study[J]. Deep-Sea Res Ⅰ, 2002, 49(8): 1387-1412. https://xueshu.baidu.com/usercenter/paper/show?paperid=e8eec4e526cd7598b3f6b4765a2ea171&site=xueshu_se&hitarticle=1
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