Measurements of the horizontal directivity of the underwater sound made beh
ind individual breaking waves in the surf zone are presented. To an observe
r behind a breaking wave, the breaking noise appears to radiate from acoust
ic hot-spots, which are compact sources at the ends of the breaking wavecre
st. The hot-spots move through the surf zone as the length of breaking wave
crest increases, leading to systematic temporal variations in the wave nois
e directionality. Measurements of the acoustical properties of the mixture
of water and bubbles left behind the breaking wave are presented. Sound spe
eds as low as 500 m/s and acoustic absorption up to 50 dB per mere; occur i
n the bubbly region. Based on these measurements and a propagation model fo
r the surf noise, it is proposed that the observed horizontal directivity i
s caused by the interaction between the noise radiated by the breaking wave
crest and the residue of bubbly water left behind the wave. (C) 1999 Acoust
ical Society of America. [S0001-4966(99)02206-7].