title: Turbidity maximum of the northern chesapeake bay.
abstract: The turbidity maximum near the head of the Chesapeake Bay is produced primarily by the local resuspension of bottom sediments, and by the estuarine "sediment trap" which is formed in the upper reaches of the estuarine circulation regime by the net nontidal circulation.
authors.forename: J R
authors.initials: JR
authors.lastname: Schubel