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- W4311434584 abstract "of signal-to-noise ratios and the phase of the horizontal and vertical velocities, are consistent with generation of the internal tide as a wide beam (approx.80 m) along the continental slope between 474 and 1050 m. The beam reflects from the sea surface and from the sea floor over the shelf as it passes through the mooring sites. The beam is present at least 50 km from the generation area. Barotropic and baroclinic components of the current were separated at each sensor. It was shown that the baroclinic components satisfy the momentum balance for internal waves. Baroclinic currents were as large or slightly larger than barotropic currents, which is consistent with available models. Baroclinic dissipation rates in mide-shelf and inner shelf regions (1.5 x 10/sup -5/ Wm/sup -3/) are comparable to those found by Wang and Mooers (1977) for the same data set but using different methods of analysis. Baroclinic energy was dissipated more strongly on the outer shelf (2.5 x 10/sup -5/ Wm/sup -3/)." @default.
- W4311434584 created "2022-12-26" @default.
- W4311434584 creator A5066951617 @default.
- W4311434584 date "1971-01-01" @default.
- W4311434584 modified "2023-09-26" @default.
- W4311434584 title "BAROTROPIC TIDE OVER THE CONTINENTAL SHELF OFF THE WASHINGTON--OREGON COAST. Special Report No. 46." @default.
- W4311434584 doi "https://doi.org/10.2172/4007072" @default.
- W4311434584 hasPublicationYear "1971" @default.
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