Published online by Cambridge University Press: 21 April 2006
Various flow processes resulting from the breaking of ocean surface waves are examined in order to determine their relative efficiencies as sources of sound. Momentum fluctuation arising from splashing water sprays is identified as the major contributor to the underwater sound. It is shown that the splashing is more efficient in radiating sound than other processes, such as unsteady foaming that entrains air bubbles into water, and turbulent motions in the surface layer associated with compressibility of the entrained bubbles. A model is presented to estimate the sound power radiated in terms of parameters of the wind and surface wave field. Comparison of theory with measurements is made and good agreement is discovered.