Experimental study of nearshore dynamics on a barred beach with rip channels

[1] Wave and current measurements are presented from a set of laboratory experiments performed on a fixed barred beach with periodically spaced rip channels using a range of incident wave conditions. The data demonstrate that the presence of gaps in otherwise longshore uniform bars dominates the nearshore circulation system for the incident wave conditions considered. For example, nonzero cross-shore flow and the presence of longshore pressure gradients, both resulting from the presence of rip channels, are not restricted to the immediate vicinity of the channels but instead are found to span almost the entire length of the longshore bars. In addition, the combination of breaker type and location is the dominant driving mechanism of the nearshore flow, and both are found to be strongly influenced by the variable bathymetry and the presence of a strong rip current. The depth-averaged currents are calculated from the measured velocities assuming conservation of mass across the measurement grid. The terms in both the cross-shore and longshore momentum balances are calculated, and their relative magnitudes are quantified. The cross-shore balance is shown to be dominated by the cross-shore pressure and radiation stress gradients in general agreement with previous results, however, the rip current is shown to influence the wave breaking and the wave-induced setup in the rip channel. Analysis of the longshore balance shows that the overall strength of the longshore feeder currents is governed by a balance between longshore pressure gradient forcing and an opposing radiation stress gradient. In addition, the longshore feeder currents show maxima in the bar trough region, providing experimental evidence that longshore pressure gradients can shift longshore current maxima shoreward from the bar crest. Finally, since the longshore radiation stress gradient in the surf zone is governed by the amount of wave dissipation on the rip current, there exists a positive feedback mechanism whereby a strong rip current can weaken the radiation stress gradient opposing the feeder currents and lead to even stronger feeder currents and rips.

[1]  R. Dalrymple,et al.  Rip current instabilities , 2001, Journal of Fluid Mechanics.

[2]  I. A. Svendsen,et al.  Analysis of Rip Current Systems , 2001 .

[3]  S. Elgar,et al.  Field observations of wave‐driven setdown and setup , 2001 .

[4]  E. Thornton,et al.  Undertow over a barred beach , 2000 .

[5]  Alongshore currents over variable beach topography , 2000 .

[6]  R. Brander,et al.  Morphodynamics of a large-scale rip current system at Muriwai Beach, New Zealand , 2000 .

[7]  A note on hydrodynamic instabilities and horizontal circulation in the surf zone , 1999 .

[8]  Robert W. Brander Field observations on the morphodynamic evolution of a low-energy rip current system , 1999 .

[9]  K. Haas,et al.  NUMERICAL MODELING OF NEARSHORE CIRCULATION ON A BARRED BEACH WITH RIP CURRENTS , 1999 .

[10]  R. Deigaard,et al.  The circulation over a longshore bar with rip channels , 1999 .

[11]  T. Aagaard,et al.  Mean currents and sediment transport in a rip channel , 1997 .

[12]  Jurjen A. Battjes,et al.  A laboratory study of longshore currents over barred and non-barred beaches , 1997 .

[13]  E. Thornton,et al.  Longshore Currents Over Barred Beaches , 1996 .

[14]  I. A. Svendsen,et al.  Longshore Nonuniformities of Nearshore Currents , 1996 .

[15]  Joan Oltman-Shay,et al.  Effect of alongshore nonuniformities on longshore current predictions , 1995 .

[16]  Ib A. Svendsen,et al.  Nearshore mixing and dispersion , 1994, Proceedings of the Royal Society of London. Series A: Mathematical and Physical Sciences.

[17]  Nicholas C. Kraus,et al.  Longshore Current on a Barred Beach: Field Measurements and Calculation , 1993 .

[18]  Luc Hamm DIRECTIONAL NEARSHORE WAVE PROPAGATION OVER A RIP CHANNEL: AN EXPERIMENT , 1993 .

[19]  D. Huntley,et al.  On the spacing between observed rip currents , 1992 .

[20]  R. Dalrymple,et al.  WAVE GROUP FORCED NEARSHORE CIRCULATION , 1991 .

[21]  Robert A. Dalrymple,et al.  Directional wavemaker theory with sidewall reflection , 1989 .

[22]  E. Kit,et al.  Flow characteristics along the rip current system under low-energy conditions , 1988 .

[23]  E. Kit,et al.  Flow characteristics at the rip current neck under low energy conditions , 1988 .

[24]  D. Sherman,et al.  LONGSHORE CURRENT PROFILES AND LATERAL MIXING ACROSS THE SURF ZONE OF A BARRED NEARSHORE , 1986 .

[25]  I. A. Svendsen,et al.  THE INTERACTION OF WAVES AND CURRENTS OVER A LONGSHORE BAR , 1986 .

[26]  Robert G. Dean,et al.  Wave height variation across beaches of arbitrary profile , 1985 .

[27]  L. Wright,et al.  Morphodynamic variability of surf zones and beaches: A synthesis , 1984 .

[28]  I. A. Svendsen Wave Heights and Set-up in a Surf Zone , 1983 .

[29]  Robert A. Dalrymple,et al.  Wave-current interaction models for rip currents , 1978 .

[30]  Robert A. Dalrymple,et al.  Rip Currents and Their Causes , 1978 .

[31]  Chiang C. Mei,et al.  Effects of topography on the circulation in and near the surf zone—Linear theory , 1977 .

[32]  Robert A. Dalrymple,et al.  A MECHANISM FOR RIP CURRENT GENERATION ON AN OPEN COAST. , 1975 .

[33]  Choule J. Sonu,et al.  Field observation of nearshore circulation and meandering currents , 1972 .

[34]  D. Cook The occurrence and geologic work of rip currents off southern California , 1970 .

[35]  Douglas L. Inman,et al.  Rip currents: 2. Laboratory and field observations , 1969 .

[36]  Anthony J. Bowen,et al.  Rip currents: 1. Theoretical investigations , 1969 .

[37]  P. Bruun Longshore currents and longshore troughs , 1963 .

[38]  M. Longuet-Higgins,et al.  Radiation stress and mass transport in gravity waves, with application to ‘surf beats’ , 1962, Journal of Fluid Mechanics.

[39]  P. McKenzie Rip-Current Systems , 1958, The Journal of Geology.

[40]  Thorndike Saville,et al.  Model study of sand transport along an infinitely long, straight beach , 1950 .

[41]  Francis P. Shepard,et al.  Nearshore water circulation related to bottom topography and wave refraction , 1950 .

[42]  K. O. Emery,et al.  Rip Currents: A Process of Geological Importance , 1941, The Journal of Geology.