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南黄海绿潮暴发与硝酸盐及水文环境因子的关系
引用本文:潘俊,于非,魏传杰,任强,孙淑慧,李靖.南黄海绿潮暴发与硝酸盐及水文环境因子的关系[J].海洋与湖沼,2018,49(5):1031-1037.
作者姓名:潘俊  于非  魏传杰  任强  孙淑慧  李靖
作者单位:中国科学院海洋研究所;中国科学院大学;中国科学院海洋大科学研究中心;中国科学院海洋研究所海洋环境工程中心;中国科学院海洋环流与波动重点实验室;青岛海洋科学与技术国家实验室海洋动力过程与气候功能实验室;中国科学院海洋生态与环境科学重点实验室
基金项目:鳌山科技创新计划项目,2016ASKJ02-04号;国家自然科学基金项目,41806164号,41376031号,U1406401号;中国科学院战略性先导科技专项项目,XDA11020301号。
摘    要:为了解浒苔绿潮的发展态势、马尾藻分布区与漂移状况,本文基于2016—2017年浒苔暴发季(春末夏初)在黄海绿潮潜在起源区获取的多航次及参考2015年布放定点潜标的环境因子资料,通过高频的精细化硝酸盐监测,对影响黄海浒苔绿潮的起源和发生发展过程中的重要环境要素进行了分析。结果表明:不同年份,黄海浒苔绿潮具有相似的发生发展过程,两个年度的黄海表层硝酸盐分布趋势有差异;年际变化上, 2017年绿潮规模较上一年度显著偏小,该年度出现的黄海赤潮、金潮对绿潮规模有一定抑制作用。

关 键 词:黄海  绿潮  春末夏初  环境因子
收稿时间:2017/12/28 0:00:00
修稿时间:2018/5/9 0:00:00

RELATIONSHIP BETWEEN GREEN TIDE OUTBREAK AND NITRATE AND HYDROLOGICAL ENVIRONMENTAL FACTORS IN THE SOUTH YELLOW SEA
PAN Jun,YU Fei,WEI Chuan-Jie,REN Qiang,SUN Shu-Hui and LI Jing.RELATIONSHIP BETWEEN GREEN TIDE OUTBREAK AND NITRATE AND HYDROLOGICAL ENVIRONMENTAL FACTORS IN THE SOUTH YELLOW SEA[J].Oceanologia Et Limnologia Sinica,2018,49(5):1031-1037.
Authors:PAN Jun  YU Fei  WEI Chuan-Jie  REN Qiang  SUN Shu-Hui and LI Jing
Institution:Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;University of Chinese Academy of Sciences, Beijing 100049, China;Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;Center for Marine Environmental Engineering, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China,Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;University of Chinese Academy of Sciences, Beijing 100049, China;Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;CAS Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;Laboratory for Ocean Dynamics and Climate, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China,Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;University of Chinese Academy of Sciences, Beijing 100049, China;Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;Center for Marine Environmental Engineering, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China,Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;University of Chinese Academy of Sciences, Beijing 100049, China;Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;CAS Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China,Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;Center for Marine Environmental Engineering, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China and Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China;Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China;CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
Abstract:Based on the data of environmental factors from multiple voyages and fixed-point buoy about the green tide in the Yellow Sea during the spring to summer in 2016-2017. We focus on the recent progress on the origin and development process of the Yellow Sea green tides. The drifting and distribution of Sargassum horneri were surveyed by multi-disciplinary scientific investigation and research. In the present paper, we analyzed the key biological features of the causative algae and the main environmental factors affecting blooming and drifting of the green algae. The results showed that the bloating green algae of developmental processes were similar, while the impact weaker than 2016, while the impact obvious weaker than 2016, the "Red tide" and "Brown tide" exist at the same time and the trace of nitrate have different. Both of them in the Yellow Sea have certain inhibitory effects on the scale change of the green tide. By analyzing the environmental background of the Subei coastal and the South Yellow Sea to provide in-site data support, we concerned about the causes of the early development of the green tide and the changes in the scale of the green tide. These results can provide decision-making service for environmental management system of marine pollution prevention, ecological protection, and environmental restoration.
Keywords:the Yellow Sea  Green tide  late spring and early summer  environmental factor
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