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Abstract
Time series measurements of current velocity, depth and suspended-solids concentration (SSC) were used to obtain suspended-solids fluxes (SSF) during the fall at central Honker Bay and Spoonbill Creek. A wind-induced shear stress increases SSF out of Honker Bay through Spoonbill Creek by combining two effects: (1) wind-wave resuspension of bed sediments, and (2) wind shear raises the water level at the Honker Bay. High SSC water advected from Honker Bay into the Sacramento River does not return on the following ebb tide, which creates the dispersive SSF. The total SSF was always out of Honker Bay during the fall suggesting that high metals and pesticides concentrations are not caused by transport through Spoonbill Creek into Honker Bay.
Study Area
Publication type | Conference Paper |
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Publication Subtype | Conference Paper |
Title | Sediment transport pathway in the back of a nearly semienclosed subembayment of San Francisco Bay, California |
ISBN | 9780784402818 |
Volume | B pt 2 |
Year Published | 1997 |
Language | English |
Publisher | American Society of Civil Engineers |
Contributing office(s) | San Francisco Bay-Delta, Woods Hole Coastal and Marine Science Center, Pacific Regional Director's Office |
Description | 6 p. |
Larger Work Type | Book |
Larger Work Subtype | Conference publication |
Larger Work Title | Water for a chancing global community: Proceedings of the the 27th Congress of the International Association for Hydraulic Research |
First page | 1096 |
Last page | 1101 |
Conference Title | 27th Congress of the International Association for Hydraulic Research (IAHR) |
Conference Location | San Francisco, CA |
Conference Date | August 10-15, 1997 |
Country | United States |
State | California |
Other Geospatial | Honker Bay, San Francisco Bay, Spoonbill Creek |
Online Only (Y/N) | N |
Additional Online Files (Y/N) | N |
Google Analytic Metrics | Metrics page |