Shoaling
D2. Hydrography, tides, waves, bathymetry and marine geologyDefinition
Increase in wave height as a wave moves into shallower water.
Shoaling is the increase in wave height as a wave moves into water shallow enough to feel the bottom, where the group speed slows and wave energy concentrates into a shorter, steeper profile. It precedes and combines with refraction and, ultimately, breaking. Shoaling focuses energy on headlands and amplifies long waves such as tsunamis at the coast; the shoaling coefficient quantifies the height change from deep to shallow water.