Abstract
A vertical array of moored velocity and temperature sensors was used to study the high-frequency (periods of less than 24 hr) structure during a coastal upwelling event. The upwelling event, which represents a wind-generated mesoscale response of the ocean circulation along a meridional coastline, changes the environment in which the high-frequency disturbances are produced and propagated....
Recommended Citation
Hayes, Stanley P., and David Halpern. 1976. "Observations of internal waves and coastal upwelling off the Oregon Coast." Journal of Marine Research 34, (2). https://elischolar.library.yale.edu/journal_of_marine_research/1358
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