Seasonal and spring interannual variations in satellite-observed chlorophyll-a in the Yellow and East China Seas: New datasets with reduced interference from high concentration of resuspended sediment

被引:62
作者
Yamaguchi, Hisashi [1 ]
Ishizaka, Joji [2 ]
Siswanto, Eko [3 ]
Son, Young Baek [4 ]
Yoo, Sinjae [5 ]
Kiyomoto, Yoko [6 ]
机构
[1] Japan Aerosp Explorat Agcy, Tsukuba Space Ctr, Tsukuba, Ibaraki 3058505, Japan
[2] Nagoya Univ, Hydrospher Atmospher Res Ctr, Chikusa Ku, Nagoya, Aichi 4648601, Japan
[3] Japan Agcy Marine Earth Sci & Technol, Yokosuka, Kanagawa 2370061, Japan
[4] KIOST, Korea Ocean Satellite Ctr, Seoul 425600, South Korea
[5] Korea Inst Ocean Sci & Technol, Ansan 425600, Gyeonggi Do, South Korea
[6] Seikai Natl Fisheries Res Inst, Nagasaki 8512213, Japan
关键词
Yellow Sea; East China Sea; SeaWiFS; Chlorophyll-a; Total suspended matter; Spring bloom; DISSOLVED ORGANIC-MATTER; ALGAL BLOOMS; ATMOSPHERIC CORRECTION; CHANGJIANG RIVER; DILUTED WATER; PHYTOPLANKTON; COASTAL; DYNAMICS; ECOSYSTEMS; ALGORITHMS;
D O I
10.1016/j.csr.2013.03.009
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Seasonal and spring interannual variations in chlorophyll-a (Chl) and total suspended matter (TSM) in the Yellow and East China Seas through a 10-year period were examined by using new datasets from Yellow Sea Large Marine Ecosystem Ocean Color Project (YOC) algorithms. YOC SCHL calculations are based on a combination of the SeaWiFS standard algorithm and a local empirical algorithm for areas of low and high normalized water-leaving radiance 555 nm, respectively. YOC SCHL was lower than the standard SCHL in areas with high concentrations of resuspended sediment, especially along the Chinese and Korean coasts and around the Changjiang Bank from fall to spring. YOC SCHL was high in areas of low TSM in the middle of the Yellow Sea, and offshore of the Changjiang Bank in April, indicating the occurrence of spring blooms. In these areas, ISM was dominated by phytoplankton cells and phytoplankton-related organic particles. Offshore from the Changjiang River mouth and around the Changjiang Bank, YOC SCHL and ism in March were low and high, respectively, with maximum YOC SCHL values occurring around the Changjiang Bank in May. Spring bloom started with decrease in resuspended sediment concentrations in these areas. During summer, YOC SCHL values were high and TSM concentrations were low; TSM was dominated by organic particles related to phytoplankton activity when Changjiang River diluted water moved from the river mouth to east of the bank. YOC SCHL in spring offshore from the Changjiang River mouth increased significantly during the 10 years, and correspond to an increase in red tide events. In the middle of the Yellow Sea, maximum YOC SCHL in spring increased gradually and significantly during the 10 years. Many of the spatial and temporal variations in YOC SCHL were consistent with a range of earlier in situ descriptions. Our results indicate that the satellite ocean data with proper algorithms is a powerful tool to analyze phytoplankton dynamics in moderate-high suspended sediment area. (C) 2013 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1 / 9
页数:9
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