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夏季台湾海峡水及黑潮次表层涌升水向东海近陆架区营养盐输送通量的估算
作者姓名:LI Hongmei  SHI Xiaoyong  WANG Hao  HAN Xiurong
作者单位:College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;National Marine Hazard Mitigation Service, Beijing 100194, China;Fujian Marine Environment and Fishery Resource Monitoring Center, Fuzhou 350003, China;College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China
基金项目:The National Basic Research Program(973 Program)of China under contract No.2010CB428701
摘    要:According to historical mean ocean current data through the field observations of the Taiwan Ocean Research Institute during 1991–2005 and survey data of nutrients on the continental shelf of the East China Sea(ECS) in the summer of 2006, nutrient fluxes from the Taiwan Strait and Kuroshio subsurface waters are estimated using a grid interpolation method, which both are the sources of the Taiwan Warm Current. The nutrient fluxes of the two water masses are also compared. The results show that phosphate(PO4-P), silicate(SiO3-Si) and nitrate(NO3-N) fluxes to the ECS continental shelf from the Kuroshio upwelling water are slightly higher than those from the Taiwan Strait water in the summer of 2006. In contrast, owing to its lower velocity, the nutrient flux density(i.e., nutrient fluxes divided by the area of the specific section) of the Kuroshio subsurface water is lower than that of the Taiwan Strait water. In addition, the Taiwan Warm Current deep water, which is mainly constituted by the Kuroshio subsurface water, might directly reach the areas of high-frequency harmful alga blooms in the ECS.

关 键 词:东海大陆架  台湾海峡  物质通量  东中国海  营养素  水域  黑潮  估计
收稿时间:2013/11/18 0:00:00
修稿时间:2014/5/26 0:00:00

An estimation of nutrient fluxes to the East China Sea continental shelf from the Taiwan Strait and Kuroshio subsurface waters in summer
LI Hongmei,SHI Xiaoyong,WANG Hao,HAN Xiurong.An estimation of nutrient fluxes to the East China Sea continental shelf from the Taiwan Strait and Kuroshio subsurface waters in summer[J].Acta Oceanologica Sinica,2014,33(11):1-10.
Authors:LI Hongmei  SHI Xiaoyong  WANG Hao and HAN Xiurong
Institution:1.College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China2.College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao 266100, China;National Marine Hazard Mitigation Service, Beijing 100194, China3.Fujian Marine Environment and Fishery Resource Monitoring Center, Fuzhou 350003, China
Abstract:According to historical mean ocean current data through the field observations of the Taiwan Ocean Research Institute during 1991-2005 and survey data of nutrients on the continental shelf of the East China Sea (ECS) in the summer of 2006, nutrient fluxes from the Taiwan Strait and Kuroshio subsurface waters are estimated using a grid interpolation method, which both are the sources of the Taiwan Warm Current. The nutrient fluxes of the two water masses are also compared. The results show that phosphate (PO4-P), silicate (SiO3-Si) and nitrate (NO3-N) fluxes to the ECS continental shelf from the Kuroshio upwelling water are slightly higher than those from the Taiwan Strait water in the summer of 2006. In contrast, owing to its lower velocity, the nutrient flux density (i.e., nutrient fluxes divided by the area of the specific section) of the Kuroshio subsurface water is lower than that of the Taiwan Strait water. In addition, the Taiwan Warm Current deep water, which is mainly constituted by the Kuroshio subsurface water, might directly reach the areas of high-frequency harmful alga blooms in the ECS.
Keywords:nutrient  flux  Taiwan Warm Current  summer  East China Sea
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