摘要:
|
从海气相互作用角度,利用东海区20年的赤潮实况资料以及EAR-40海洋高分辨率再分析资料,分析赤潮年际变化规律,重点研究赤潮发生频次与厄尔尼诺年份的相关关系,得出厄尔尼诺次年赤潮发生次数偏多的结论.同时探讨了东亚季风的年际变化及异常对东海赤潮的影响,尤其是东海近海对于气候异常的响应主要表现在近地层大气辐散能力增强,且大值区集中在长江口以南至台湾海峡海域,正与赤潮发生次数剧增的时间和海区相吻合.本文讨论了大尺度的气候异常对东海赤潮的影响,为赤潮的年度预测研究作提供分析依据,也为赤潮的监测和预警报工作提供新的思考角度. |
According to the requirements of Marine disaster assessment and the annual forecast work of State Oceanic administration, we study the relationships between the east Asian monsoon anomalous and the red tide occurrence frequency in the East China Sea from the angle of air-sea interaction. Based on the 20 years red tides historical data and EAR - 40 high resolution re-analyzed data, red tide occurred frequency in the annual scale was analyzed, and the relationships between red tide occurrence frequency and El-Ni駉 year was derived, which showed that red tide becomes more frequent in the next year of EI-Ni駉. Meanwhile, the annual variation of the East Asia monsoon and exception on the influence of the red tides was discussed. The response to the climate anomalous in the offshore of the East China Sea performs as atmospheric divergence ability enhancement in the surface layer, and the extreme center appeared in the area from Changjiang river mouth to the Taiwan Strait, which coincided with the time and area of red tide outbreaks frequency excursion. The influence of the large-scale climate anomalies on red tide outbreaks frequency in the East China Sea was discussed, which provided reference for the annual prediction research work of the red tides and new thinking angle for monitoring and forecast warning work of red tide. |
参考文献:
|
[1] 蔡榕硕, 陈际龙, 黄荣辉. 我国近海和邻近海的海洋环境对最近全球气候变化的响应[J].大气科学, 2006, 30(5): 1020-1033. [2] 黄光杨.教育统计与测量评价综合教程[M].福建科学与技术出版社, 2003,69-73. [3] M H 格兰茨. 变化的洋流?#21380;尔尼诺对气候和社会的影响[M],北京: 气象出版社.1998,16-17. [4] 杨红, 何春良. 我国海域赤潮发生与海温及厄尔尼诺的相关分析[J]. 海洋湖沼通报, 2009,2(1): 1-6. [5] 陈美榕, 石少华, 沈红海. 长江口海域海水表层温度与厄尔尼诺事件的关系[J]. 海洋预报, 2005, 22(1): 80-85. [6] 国家海洋局, 2000?008 年中国海洋环境质量公报[R]. 北京:国家海洋局, 2008. [7] Matrin J H. Cordon R M. Northeast Pacific iron distribution inrelation tophytonplankton productivity[J]. Deep Sea Res, 1988,135: 177-179. [8] 田荣湘.东亚季风与东海赤潮[J].浙江大学学报(理学版), 2005,32(3): 356-360.图13 中国近海陆架海洋上升流和营养盐输送变动的示意图13 |
服务与反馈:
|
【文章下载】【发表评论】【查看评论】【加入收藏】
|
|
|