The serial remote sensing based imageries clearly revealed large scale of upwelling within large regional enhancement of chlorophyll‐ a (Chl‐ a ) concentration in the southern East China Sea (ECS) after the passage of super typhoon Hai‐Tang in July 2005. After the typhoon on 22 July, the upwelling area (<26°C) expanded rapidly to 9146 km 2 on the shelf‐break. The large increased upwelling persisted for more than a week. Ocean color images also reveled that high Chl‐ a concentration of >3.0 mg/m 3 appeared in the shelf region, where the high Chl‐ a pattern matched the upwelling in terms of location and time. On the other hand, a large offshore SST cooling was also observed mainly to the right of typhoon track on 20 July, it lasted in a period of 2–3 days. This paper provides clear and high‐resolution evidence that typhoon significant increased upwelling and Chl‐ a concentration in the southern ECS.
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Chang et al. (2008) studied this question.
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