Hourly changes in sea surface salinity in coastal waters recorded by Geostationary Ocean Color Imager

被引:18
作者
Liu, Rongjie [1 ,2 ]
Zhang, Jie [2 ]
Yao, Haiyan [3 ]
Cui, Tingwei [2 ]
Wang, Ning [4 ]
Zhang, Yi [4 ]
Wu, Lingjuan [4 ]
An, Jubai [1 ]
机构
[1] Dalian Maritime Univ, Informat Sci & Technol Coll, Dalian 116026, Peoples R China
[2] State Ocean Adm, Inst Oceanog 1, Qingdao 266061, Peoples R China
[3] State Ocean Adm, North China Sea Environm Monitoring Ctr, Qingdao 266033, Peoples R China
[4] State Ocean Adm, North China Sea Marine Forcasting Ctr, Qingdao 266061, Peoples R China
基金
中国国家自然科学基金;
关键词
Sea surface salinity; Hourly dynamics; Bohai sea; GOCI; EAST CHINA SEA; SUSPENDED PARTICULATE MATTER; HARMFUL ALGAL BLOOM; BOHAI SEA; OPTICAL-PROPERTIES; CHESAPEAKE BAY; CLYDE SEA; GOCI; VARIABILITY; ESTUARINE;
D O I
10.1016/j.ecss.2017.07.004
中图分类号
Q17 [水生生物学];
学科分类号
071004 ;
摘要
In this study, we monitored hourly changes in sea surface salinity (SSS) in turbid coastal waters from geostationary satellite ocean color images for the first time, using the Bohai Sea as a case study. We developed a simple multi-linear statistical regression model to retrieve SSS data from Geostationary Ocean Color Imager (GOCI) based on an in situ satellite matched-up dataset (R-2 = 0.795; N = 41; Range: 26.4 to 31.9 ps mu). The model was then validated using independent continuous SSS measurements from buoys, with the average percentage difference of 0.65%. The model was applied to GOCI images from the dry season during an astronomical tide to characterize hourly changes in SSS in the Bohai Sea. We found that the model provided reasonable estimates of the hourly changes in SSS and that trends in the modeled and measured data were similar in magnitude and direction (0.43 vs 0.33 ps mu, R-2 = 0.51). There were clear diurnal variations in the SSS of the Bohai Sea, with a regional average of 0.455 +/- 0.079 psji (0.02-3.77 ps mu). The magnitude of the diurnal variations in SSS varied spatially, with large diurnal variability in the nearshore, particularly in the estuary, and small variability in the offshore area. The model for the riverine area was based on the inverse correlation between SSS and CDOM absorption. In the offshore area, the water mass of the North Yellow Sea, characterized by high SSS and low CDOM concentrations, dominated. Analysis of the driving mechanisms showed that the tidal current was the main control on hourly changes in SSS in the Bohai Sea. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:227 / 236
页数:10
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