The transformation of ocean swell across a wide, shallow (nominal depths 25--50 m) continental shelf is examined with data from a 100 km long transect of bottom pressure recorders extending from the shelf break to the beach at Duck, North Carolina. The analysis is restricted to periods with light winds when surface boundary layer processes (e.g., wave generation by wind and wave breaking in the form of whitecaps) are expected to be relatively unimportant. The majority of the observations with low-energy incident swell conditions (significant wave heights <1 m) shows weak variations in swell energy across the shelf, in qualitative agreement with predictions of a spectral refraction model. Although the predicted ray trajectories of waves propagating over the irregular shelf bathymetry are quite sensitive to the deep water incident wave directions, the predicted spatial energy variations for broadbanded wave fields are small and relatively insensitive to incident wave conditions, consistent with the observations. Whereas swell dissipation on the shelf appears to be insignificant in low-energy conditions, strong attenuation of swell energy levels (a factor 4 between the shelf break and nearshore sites) was observed in high-energy conditions (significant wave height 2.5 m). This decay, not predicted by the energy-conserving refraction model, indicates that dissipative bottom boundary layer processes can play an important role in the transformation of swell across wide continental shelves. ¿ 2000 American Geophysical Union