文献类型：期刊文献

中文题名：冬季吕宋岛西北海域叶绿素时空变化特征

英文题名：Spatial-temporal variation of winter phytoplankton blooms in the northwest of Luzon Island

作者：高慧[1];赵辉[2];沈春燕[3];陈法锦[1]

机构：[1]广东海洋大学海洋与气象学院,广东湛江524088;[2]广东海洋大学化学与环境学院,广东湛江524088;[3]广东海洋大学水产学院,广东湛江524088

年份：2018

卷号：36

期号：1

起止页码：75

中文期刊名：海洋学研究

外文期刊名：Journal of Marine Sciences

收录：CSTPCD、、北大核心2017、CSCD2017_2018、北大核心、CSCD

基金：国家自然科学基金项目资助(41376125);广东省高等学校优秀青年教师培养计划项目资助(Yq2014004);广东省普通高校国际暨港澳台合作创新平台及国际合作重大项目资助(2015KGJHZ017)

语种：中文

中文关键词：吕宋岛;冬季浮游植物藻华;上升流;EOF分析;叶绿素

外文关键词：Luzon Island;winter phytoplankton blooms; upwelling; EOF analysis; chlorophyll

中文摘要：冬季吕宋岛西北海域频繁出现藻华现象,本文使用吕宋岛西北部海域1999年11月至2015年2月共16 a冬季多卫星融合水色遥感资料,利用经验正交函数(EOF)分解方法对长时间序列的Chl-a质量浓度的时空变化进行分析讨论,并结合海表温度(SST)、风速(WS)、海面高度异常(SLA)等数据以及上述数据计算获得的相关物理环境参数,分析其与海表Chl-a质量浓度之间的关系,探讨吕宋岛西北海域海表Chl-a质量浓度的时空分布规律以及Chl-a质量浓度与周边环境的响应关系。研究结果表明通常冬季吕宋岛西北海域海表均会出现大约以(19°N,119°E)为中心的高Chl-a质量浓度现象,平行海岸的风应力以及风应力涡旋引起冬季上升流,增加了营养盐的输入,很可能是该区域藻华形成的主要机制。同时背景流场的平流效应很可能诱发上升流区域与叶绿素藻华区中心不一致,可能引起了藻华中心的北移。

外文摘要：The phenomenon of phytoplankton blooms in the northwest of Luzon Island is frequently observed in winter.In our study,using the multi-satellite merged ocean color remote sensing data from November 1999 to February 2015 in the northwestern region of Luzon Island,the spatial and temporal changes of Chl-a concentration in long time series were investigated by means of the empirical orthogonal function（ EOF） decomposition method and multiple correlation analysis（ MCA）. Combined with physical environmental parameters such as wind speed（ WS）,sea surface temperature（SST） and sea level anomalies（ SLA）,the relationship between Chl-a and surrounding sea environments was then investigated in the study. The results show that centers of winter Chl-a blooms in northwest of Luzon Island appear often at the location of about（19°N,119° E）. Significant multiple correlation coefficient（ R = 0. 782 6,P〈0. 05）from the multiple correlation analysis between Chl-a and oceanic conditions indicates that the wind parallel to the coastline and the wind stress curls enhance winter upwelling in the study area,increasing the input of the nutrients into the upper layer,which is probably the main mechanism of the formation of phytoplankton blooms in the area. At the same time,the advection effect of the background flow field is likely to induce the upwelling area to be inconsistent with the center of phytoplankton blooms,triggering the phenomenon that the centers of phytoplankton blooms shifted northward along with the water body in the area.