Record Details
Nonlinear shear instabilities of alongshore currents over barred beaches
ScholarsArchive at Oregon State University
| Field | Value |
|---|---|
| Title | Nonlinear shear instabilities of alongshore currents over barred beaches |
| Names |
Slinn, Donald N.
(creator) Allen, J. S. (creator) Newberger, P. A. (creator) Holman, Robert A. (creator) |
| Date Issued | 1998-08-15 (iso8601) |
| Note | copyrighted by American Geophysical Union |
| Abstract | The nonlinear dynamics of finite amplitude shear instabilities of alongshore currents in the nearshore surf zone over barred beach topography are studied using numerical experiments. These experiments extend the recent study of Allen et al. [1996], which utilized plane beach (constant slope) topography by including shore-parallel sandbars. The model involves finite-difference solutions to the nonlinear shallow water equations for forced, dissipative, initial-value problems and employs periodic boundary conditions in the alongshore direction. Effects of dissipation are modeled by linear bottom friction. Forcing for the alongshore currents is specified using a model formulated by Thornton and Guza [1986] (T-G). Distinct classes of flows develop depending on the dimensionless parameter Q, the ratio of an advective to a frictional timescale. For Q greater than a critical value Qc the flows are linearly stable. For ∆Q = Qc - Q > 0 the flow is unstable. For small values of ∆Q, equilibrated shear waves develop that propagate alongshore at phase speeds and wavelengths that are in agreement with predictions from linear theory for the most unstable mode. At intermediate values of ∆Q, unsteady vortices form and exhibit nonlinear interactions as they propagate alongshore, occasionally merging, pairing, or being shed seaward of the sandbar. At the largest values of ∆Q examined, the resulting flow field resembles a turbulent shear flow. A net effect of the instabilities at large ∆Q is to distribute the time-averaged alongshore momentum from local maxima of the T-G forcing, located over the sandbar and near the shore, into the region of the trough. The across-shore structure of the time-averaged alongshore current is in substantially better qualitative agreement with observations than that given by a steady frictional balance with T-G forcing. The results point to the possible existence in the nearshore surf zone of an energetic eddy field associated with instabilities of the alongshore current. |
| Genre | Article |
| Identifier | Allen, J. S., Holman, R. A., Newberger, P. A., Slinn, D. N., Nonlinear shear instabilities of alongshore currents over barred beaches, J. Geophys. Res., 103, C9, 1998. |
