"Semi-daily fluctuations in geopotential off the Washington coast" by H. O. Mofjeld and R. K. Reed
 

Abstract

Fluctuations in geopotential anomaly at eight 12-hr time-series stations off Washington appeared to result from semi-daily internal tides propagating seaward from the shelf break. Comparison of the observations with computations suggests the existence of a first mode wave. The oscillations did not appreciably decay offshore, perhaps as a result of bathymetric focusing.

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