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Remote sensing of wave roller lengths in the laboratory

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Title Remote sensing of wave roller lengths in the laboratory
Names Haller, Merrick C. (creator)
Catalan, P. A. (creator)
Date Issued 2009-07-22 (iso8601)
Note Copyrighted by American Geophysical Union.
Abstract The optical intensity signals from surf zone waves in a laboratory flume are analyzed
using several different phase-averaging techniques, and a methodology is developed for
estimating wave roller lengths and local wave dissipation. The intensity signals (i.e.,
phase-averaged intensity profiles) of individual breaking waves are compared with the
wave profiles measured by in situ wave gauges, and the optical signal of the wave roller is
shown to ramp up from the toe of the wave roller on the front face of the wave to a
maximum intensity at the wave crest. The remote sensing observations capture the growth,
equilibrium, and decay phases of the roller as it propagates over a fixed bed arranged in a
bar/trough morphology. Next, for the regular wave conditions considered here, the local
maxima of the phase-averaged intensities are shown to better indicate the initial onset of
wave breaking and the occurrence of wave breaking in the bar trough, as compared to
the more commonly used time-averaged mean intensity. In addition, the phase-averaged
profiles are used to measure the size of the roller, and these measurements are compared
to previous observations of smaller-scale rollers in equilibrium. The observed roller
lengths are shown to agree with predictions from a wave roller model and to provide a
new physical link between the remotely sensed signal and roller dissipation. Finally, as
an example application of these new data, a simple wave height inversion model is
presented that allows an estimation of surf zone wave heights from the remotely sensed
roller lengths.
Genre Article
Identifier Haller, M. C., and P. A. Catalán (2009), Remote sensing of wave roller lengths in the laboratory, J. Geophys. Res., 114, C07022.

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