"Observations of internal waves and coastal upwelling off the Oregon Co" by Stanley P. Hayes and David Halpern
 

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....

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