1987
DOI: 10.1007/978-1-4612-1058-0_6
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Interaction of Shallow-Water Waves and Bottom Topography

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Cited by 15 publications
(14 citation statements)
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“…Davidson-Arnott and McDonald (1989) present field evidence which suggests that the presence of an undertow very close to the bed is an important control in maintaining the equilibrium of nearshore bars. Boczar-Karakiewicz et al (1986) showed theoretically that longperiod, incident surface gravity waves in shallow water will be subject to reflective trapping by bottom undulations and a nonlinear resonance will yield positive feedback between the wave form and the growing bar forms. There are limitations to all bar genesis models, and the controversy concerning bar origin remains unresolved because the manner in which nearshore forms evolve in the field has not yet been fully documented, and since scaling problems preclude their complete examination in the laboratory.…”
Section: Introductionmentioning
confidence: 99%
“…Davidson-Arnott and McDonald (1989) present field evidence which suggests that the presence of an undertow very close to the bed is an important control in maintaining the equilibrium of nearshore bars. Boczar-Karakiewicz et al (1986) showed theoretically that longperiod, incident surface gravity waves in shallow water will be subject to reflective trapping by bottom undulations and a nonlinear resonance will yield positive feedback between the wave form and the growing bar forms. There are limitations to all bar genesis models, and the controversy concerning bar origin remains unresolved because the manner in which nearshore forms evolve in the field has not yet been fully documented, and since scaling problems preclude their complete examination in the laboratory.…”
Section: Introductionmentioning
confidence: 99%
“…In [11 they conjecture that longshore sand ridges are the result of energetic interactiuis between shallow water waves and the underlying bottom topography, and propose a simple model, which in [2] was shown to be in qualitative agreement with oceanic data. While the present study owes much to the previous work.…”
Section: Report Documentation Pagementioning
confidence: 83%
“…For internal waves, the issue of dissipation is relatively more straightforward: As the density stratification collapses in the shallower reaches of the shelf, the water column is no longer able to support an internal wave. Incidentally, Boczar-Karakiewicz et al [2] have found that the area in which stratification collapses agrees with the limit to which sand ridge fields appear.…”
Section: General Commentsmentioning
confidence: 83%
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