Seasonal and Interannual Variability of Satellite-Derived Chlorophyll-a (2000–2012) in the Bohai Sea, China

• Published in: Remote sensing (Basel, Switzerland) Vol. 9; no. 6; p. 582
• Main Authors: Zhang, Hailong, Qiu, Zhongfeng, Sun, Deyong, Wang, Shengqiang, He, Yijun
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 01-06-2017
• Subjects: Annual variations; Bohai Sea; Chlorophyll; Coastal waters; Ecosystem assessment; long-term changes; Marine ecosystems; Nutrient dynamics; Physical factors; Plankton; Regression analysis; Remote sensing; River discharge; River flow; Rivers; satellite data; Seasonal variations; Straits; sub-regions; Summer; Trends; Water circulation; Water column; Three Gorges Dam; East China Sea; Yellow Sea; China; Bohai Sea
• ISSN: 2072-4292; 2072-4292
• DOI: 10.3390/rs9060582

Knowledge of the chlorophyll-a dynamics and their long-term changes is important for assessing marine ecosystems, especially for coastal waters. In this study, the spatial and temporal variability of sea surface chlorophyll-a concentration (Chl-a) in the Bohai Sea were investigated using 13-year (2000–2012) satellite-derived products from MODIS and SeaWiFS observations. Based on linear regression analysis, the results showed that the entire Bohai Sea experienced an increase in Chl-a on a long-term scale, with the largest increase in the central Bohai Sea and the smallest increase in the Bohai strait. Distinct seasonal patterns of Chl-a existed in different sub-regions of the Bohai Sea. A long-lasting Chl-a peak was observed from May to September in coastal waters (Liaodong bay, Qinhuangdao coast, and Bohai bay) and the central Bohai Sea, whereas Laizhou bay had relatively low Chl-a in early summer. In the Bohai strait, two pronounced Chl-a peaks occurred in March and September, but the lowest Chl-a was in summer. This pattern was quite different from those in other regions of the Bohai Sea. The water column condition (stratified or mixed) was likely an important physical factor that affects the seasonal pattern of Chl-a in the Bohai Sea. Meanwhile, increased human activity (e.g., river discharge) played a significant role in changing the Chl-a distribution in both coastal waters and the central Bohai Sea, especially in summer. The increasing trend of Chl-a in the Bohai Sea might be attributed to the increase in nutrient contents from riverine inputs. The Chl-a dynamics documented in this study provide basic knowledge for the future exploration of marine biogeochemical processes and ecosystem evolution in the Bohai Sea.