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Science 26 April 2002: Vol. 296. no. 5568, pp. 724 - 727 DOI: 10.1126/science.1069803
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Reports
The Shaping of Continental Slopes by Internal Tides
D. A. Cacchione,1
L. F. Pratson,2
A. S. Ogston3
The angles of energy propagation of semidiurnal internal tides may
determine the average gradient of continental slopes in ocean basins
(~2 to 4 degrees). Intensification of near-bottom water velocities
and bottom shear stresses caused by reflection of semi-diurnal internal
tides affects sedimentation patterns and bottom gradients, as indicated
by recent studies of continental slopes off northern California and New
Jersey. Estimates of bottom shear velocities caused by semi-diurnal
internal tides are high enough to inhibit deposition of fine-grained
sediment onto the slopes.
1 Coastal and Marine Geology MS-999, U.S. Geological
Survey, 345 Middlefield Road, Menlo Park, CA 94025, USA.
2 Earth & Ocean Sciences, Nicholas School of the Environment
and Earth Sciences, Duke University, Durham, NC 27708, USA.
3 University of Washington, Box 357940, Seattle, WA 98195, USA.
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