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周伟华副研究员在《Estuarine Coastal and Shelf Science》发表文章

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时间:2012-07-11  作者:LMB  来源:文本大小:【 |  | 】  【打印

题目: The influence of late summer typhoons and high river discharge on water quality in Hong Kong waters 

作者: Weihua Zhou, Kedong Yin*, Paul J. Harrison, Joseph H.W. Lee 

刊物: Estuarine Coastal and Shelf Science,IF=2.247III区)

刊号: 2012, 111 , 35e47 

摘要: A typhoon produces a rapid mixing and flushing event and it can be added to the list of other factors such as shallow water depth, spring tidal mixing, the Pearl River discharge, summer upwelling that make Hong Kong waters relatively resistant to eutrophication impacts. Two typhoons passed over Hong Kong waters and provided an opportunity to document the changes in water quality in late summer 2003. Before the typhoon (Aug 19e20) and during a neap tide, a large algal bloom (>10 mg Chl-a L_1) occurred in the stratified southern waters influenced by the Pearl River estuarine waters with high NO3. However, PO4 and SiO4 were drawn down to near limiting concentrations by the large bloom. After the typhoons, Chl-a decreased to 2 mg L_1 due to vertical mixing and advection. The heavy rainfall and increased river discharge quickly re-set the water column to the usual strong summer stratification in only a few days. As a result, high nutrients in the river discharge stimulated another large algal bloom a few days after the next neap tide when tidal mixing was reduced. In the southern waters, the deeper station showed stronger stratification and lower bottom dissolved oxygen (DO) than the shallower station suggesting that the low DO in the bottom water may have come from offshore transport. 

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