Pressure-rime series from breathing-mode oscillation of large (centimeter s
cale or larger) underwater bubbles reveal much higher decay rates than can
be explained using viscous, thermal, or radiative mechanisms which apply to
microbubbles. It is shown that if one assumes energy transfer to shape osc
illations (surface capillary waves) of large amplitude in subharmonic reson
ance with the breathing mode [M. S. Longuet-Higgins, J. Acoust. Sec. Am. 91
, 1414 (1992)], then the shape oscillations can drive fluid motions outside
the bubble capable of exciting turbulent instabilities. Application of an
appropriate eddy viscosity from mixing-length theory to the viscous decay m
echanism appears to offer a credible explanation for the observed large dec
ay rates. An analysis is given to show that energy is transferred from the
breathing mode to surface capillaries fast enough to make the proposed deca
y mechanism viable. [S0001-4966(00)01405-3].