作者: Dubravko Justic , Robert R. Twilley , Brian C. Perez , John W. Day
DOI: 10.1016/S0272-7714(03)00010-6
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摘要: Abstract Nutrient fluxes were measured between Fourleague Bay, a shallow Louisiana estuary, and the Gulf of Mexico every 3 h February 1 April 30, 1994 to determine how high velocity winds associated with cold fronts peak Atchafalaya River discharge influenced transport. Net water ebb-dominated throughout study because wind forcing volumes entering northern Bay from River. Flushing time averaged