Spectral Wave Decay due to Bottom Friction on the Inner Shelf

Abstract

The primary scientific objective of this project is to measure the bottom dissipation of surface gravity waves as they shoal across the continental shelf as a component of the Shoaling Waves Experiment, SHOWEX. Detailed observations of the bottom boundary layer (BBL), resolving the thin oscillatory wave boundary layer over a rippled sandy bed, have been… (More)

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