Research Article
Feb 1968
Movement of Seabed Drifters Near the Columbia River
Authors: Betty-Ann Morse, M. Grant Gross, and Clifford A. BarnesAuthor Affiliations
Publication: Journal of the Waterways and Harbors Division
Volume 94, Issue 1
Abstract
Seabed drifters were released on the continental shelf within 50 km of the mouth of the Columbia River to study near-bottom water and sediment movements. From June, 1966 to October, 1966, the net movement in water deeper than 55 m was northward; at lesser depths, the movement was southward and toward the coast. Drifters grounded in considerable numbers on the ocean beach within 5 km north of the north jetty of the Columbia River and also on Clatsop Spit 5 km upriver on its south bank. Relatively few were found on the ocean beach near the south jetty. The movement near shore is in agreement with that deduced for bottom water, considering the prevailing seasonal winds and waves and the intrusion of seawater into the estuary.
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Information
Published In
Journal of the Waterways and Harbors Division
Volume 94 • Issue 1 • February 1968
Pages: 93 - 103
Copyright
© 1968 American Society of Civil Engineers.
History
Published in print: Feb 1968
Published online: Feb 12, 2021
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Authors
Affiliations
Betty-Ann Morse
Oceanogra pher, Dept. of Oceanography, Univ. of Washington, Seattle, Wash.
M. Grant Gross
Assoc. Prof., Dept. of Oceanography, Univ. of. Washington, Seattle, Wash., and Assoc. Curator of Sedimentology, Smithsonian Institution, Washmgton, D.C.
Clifford A. Barnes
Prof., Dept. of Oceanography, Univ. of Washington, Seattle, Wash.
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