| 夏季南海西部中尺度物理过程对营养盐和叶绿素a分布特征的影响 |
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| 引用本文： | 冷晓云,杨阳,孙军,张桂成,徐文喆,冯媛媛,郭术津,陈建芳,王东晓. 夏季南海西部中尺度物理过程对营养盐和叶绿素a分布特征的影响[J]. 海洋学报, 2016, 38(4): 66-75. DOI: 10.3969/j.issn.0253-4193.2016.04.006 |
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| 作者姓名： | 冷晓云 杨阳 孙军 张桂成 徐文喆 冯媛媛 郭术津 陈建芳 王东晓 |
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| 作者单位： | 1.天津科技大学海洋与环境学院, 天津 300457;天津科技大学天津市海洋资源与化学重点实验室, 天津 300457 |
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| 基金项目： | 教育部新世纪优秀人才计划(NCET-12-1065);国家自然科学基金(41176136,41276124,41306118,91128212);全球变化与海气相互作用"专项"(GASI-03-01-03-03)。 |
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| 摘 要： | 通过对2014年8月31日-9月26日国家自然科学基金委南海西部综合航次的调查结果分析,发现在中南半岛沿岸海域存在具有低温高盐的冷涡和位于其东南部海域具有高温低盐的暖涡。相对于暖涡和其他海域,冷涡水团含有更高的营养盐,并在50 m、75 m和100 m层增加明显,DIP分别高0.21 μmol/L、0.39 μmol/L和0.23 μmol/L,DIN分别高4.94 μmol/L、7.56 μmol/L和3.76 μmol/L,DSi分别高2.55 μmol/L、5.25 μmol/L和3.46 μmol/L,说明冷涡对提高初级生产力具有明显的营养优势条件和巨大潜力;叶绿素a最大值均出现在50 m层,其中以海南岛近岸海域最大,冷涡在25 m层提高初级生产力明显,主要是受营养盐影响显著;而在75 m、100 m层可能受到冷涡带来的低温环境而导致叶绿素a含量不高。
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| 关 键 词： | 南海西部 营养盐 叶绿素a |
| 收稿时间： | 2015-07-01 |
| 修稿时间： | 2015-12-10 |
Mesoscale physical processes on the effects of distribution of nutrients and chlorophyll a in the western South China Sea in summer |
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| Leng Xiaoyun,Yang Yang,Sun Jun,Zhang Guicheng,Xu Wenzhe,Feng Yuanyuan,Guo Shujin,Chen Jianfang and Wang Dongxiao. Mesoscale physical processes on the effects of distribution of nutrients and chlorophyll a in the western South China Sea in summer[J]. Acta Oceanologica Sinica (in Chinese), 2016, 38(4): 66-75. DOI: 10.3969/j.issn.0253-4193.2016.04.006 |
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| Authors: | Leng Xiaoyun Yang Yang Sun Jun Zhang Guicheng Xu Wenzhe Feng Yuanyuan Guo Shujin Chen Jianfang Wang Dongxiao |
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| Affiliation: | College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China,College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China,College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China,College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China,College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China,College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China,College of Marine and Environmental Sciences, Tianjin University of Science and Technology, Tianjin 300457, China;Tianjin Key Laboratory of Marine Resources and Chemistry, Tianjin University of Science and Technology, Tianjin 300457, China,State Oceanic Administration Key Laboratory of Marine Ecosystems and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China;State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration Hangzhou 310012, China and State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China |
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| Abstract: | Samples for seawater nutrients and chlorophyll a were collected in the western South China Sea from 31 August to 26 September,2014. Results show that coast of IndoChina have cold-core eddy with low temperature,high salinity and warm-core eddy with high temperature,low salinity which is located in the lower right relative to cold-core eddy. Relative to warm-core eddy and other areas,nutrients of cold-core eddy have higher concentration,50 m,75 m and 100 m layer of which is increased remarkably. DIP higher by 0.21 μmol/L,0.39 μmol/L and 0.23 μmol/L respectively,DIN higher by 4.94 μmol/L,7.56 μmol/L and 3.76 μmol/L respectively,and DSi higher by 2.55 μmol/L,5.25 μmol/L and 3.46 μmol/L respectively. It indicates cold-core eddy on improving primary production with significant nutritional advantages and huge potential. DCM layer appear in 50 m layer,maximum value of which is located in coast of Hainan island. Under the influence of nutrients,cold-core eddy increases primary productivity significantly in 25 m layer,while value of Chl a is not high in 75m,100m layer,which may be caused by low temperature with cold-core eddy. |
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| Keywords: | western South China Sea nutrients chlorophyll a |
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