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Shear instabilities of the mean longshore current : 1. theory

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Title Shear instabilities of the mean longshore current : 1. theory
Names Bowen, A. J. (creator)
Holman, Robert A. (creator)
Date Issued 1989-12-15 (iso8601)
Note copyrighted by American Geophysical Union
Abstract A new class of nearshore waves based on the shear instability of a steady longshore current is discussed. The
dynamics depend on the conservation of potential vorticity but with the background vorticity field, traditionally
the role of Coriolis in larger scale flows, supplIed by the shear structure of the longshore current. The resulting
vorticity waves are longshore-progressive with celerities roughly equal to V₀/3, where V₀ is the peak longshore
current velocity. A natural frequency scaling for the problem is fs, the shear of the seaward face of the
longshore current. While the instability can span a range of frequencies and wavenumbers, a representative
frequency is given by 0.07 fs, typically in the range of 10¯³-10¯² Hz (called the Far Infragravity, or FIG, band
because frequencies are just below those of the infragravity band). Wavelengths are of the order of 2x₀, where X₀
is the width of the longshore current. Growth is exponential with an e-folding time that is typically half of a
wave period. Field data, presented in the companion paper [Oltman-Shay et al., this issue], demonstrate the
presence of energetic motions from a natural beach whose behavior matches the theory in many aspects.
Results from the model suggest that shear instability will be more important on barred, rather than monotonic
beach profiles, a result of the stronger shears expected over the bar crest. Since vorticity waves will probably
have a profound effect on cross-shore mixing as well as longshore current dissipation, we expect the dynamics
of barred and monotonic beaches to show fundamental differences.
Genre Article
Identifier Bowen, R. A., and Holman, R. A., (1989). Shear instabilities of the mean longshore current : 1. Theory. J. Geophys. Res., 94, C12.

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