The issue of hydrodynamics causing cross-shore sediment transport is e
xamined analytically. Undertow is represented based on recent experime
ntal evidence. A relatively complete physics-based cross-shore sedimen
t transport model, including mechanisms for suspended and bedload tran
sport, is developed with the capacity for onshore and offshore transpo
rt. Effects of turbulence, momentum transfer, and augmented volumetric
flux in the surf zone, horizontal wave asymmetry, bottom boundary lay
er, intermittent suspension, overtopping water levels, and gravity are
included. The model is tested against data from laboratory experiment
s involving regular and irregular waves, and overtopping conditions; i
t is fairly successful in predicting prominent patterns of erosion and
deposition, sediment overwash, and longshore bars. The model lacks lo
ng-term stability.