Directional spreading of waves in the nearshore

Observations of surface gravity waves shoaling between 8-m water depth and the shoreline on a barred beach indicate that breaking results in an increa se in the directional spread of wave energy, in contrast to the directional narrowing with decreasing depth predicted by refraction theory (Snell's la w). During low-energy wave conditions, when breaking-induced wave energy lo sses over the instrumented transect are small, the observed mean propagatio n direction and spread about the mean both decrease with decreasing depth, consistent with the expected effects of refraction. Nonlinearity causes hig h-frequency components of the spectrum to become directionally aligned with the dominant incident waves. During high-energy wave conditions with signi ficant wave breaking on the sand bar, the observed mean directions still de crease with decreasing depth. However, the observed directional spreads inc rease sharply (nominally a factor of 2 for values integrated over the swell -sea frequency range) between the outer edge of the surf zone and the crest of the sand bar, followed by a decrease toward the shoreline. Observations on a nonbarred beach also show directional broadening, with spreads increa sing monotonically from the outer edge of the surf zone to a maximum value near the shoreline. Although the mechanism is not understood, these spatial patterns of directional broadening suggest that wave breaking causes signi ficant scattering of incident wave energy into obliquely propagating compon ents.