Abstract
Abstract Nutrient dynamics and its influence on the distribution of chlorophyll-a in the upwelling area of the Changjiang (Yangtze) River estuary were investigated in the spring (May) and summer (August) of 2004. In the spring, upwelling was apparent in the region of 122°20′–123°00′ E, 31°00′–32°00′ N and was associated with low temperature (16–21°C), high salinity (24–33 practical salinity units [psu]), and low dissolved oxygen (2.5–6.0 mg L−1) in the upper 10 m of the water column. The spring upwelling increased the mixed-layer phosphate, nitrate, and silicate concentrations to roughly 1, 15, and 15 μmol L−1, respectively, and improved the light transparency in the euphotic zone. This improvement in phytoplankton growing conditions was followed by an increase in chlorophyll-a concentrations. The summer upwelling was weaker and occurred over a smaller geographical area (122°20′–123°00′ E, 31°15′–31°50′ N). Strongly influenced by turbid Changjiang diluted water (CDW), it had little impact on the upper 10 ...
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