Ambient and transient bubble spectral densities in quiescent seas and under spilling breakers

Recently published observations, using laser holography near the ocean surface, have shown that the densities of 10 to 15 micron radius bubbles can be as high as 106 (per cubic meter per micron radius increment) within 3 m of the surface of quiescent seas, thereby supporting the acoustically derived values of two decades ago. The accumulated evidence suggests that these quiescent microbubble densities off the coast of California are proportional to a−4 for radius range 10 < a < 60 microns and a−2.5 for larger bubbles. A calibrated, floating, multi-frequency, acoustical resonator has now been used to obtain the bubble spectrum for 9 radii from 30 to 240 microns, 25 cm under breaking waves in the open sea. At this depth, bubbles larger than 60 microns have a radius dependence approximately a−2.5 and smaller bubble densities vary approximately as a a−4. Our densities are in good agreement with recently published laboratory studies of bubbles, using laser scattering under wind-blown surfaces with about the same surface frictional velocity U*. Older, photographically derived densities at ocean depth 75 cm are close to the new data only over the limited range 50 to 100 microns. Past inconsistencies between acoustical results and optical results were apparently due to an inability of some optical techniques to identify small bubbles in the difficult ocean environment.

[1]  Herman Medwin,et al.  In situ acoustic measurements of bubble populations in coastal ocean waters , 1970 .

[2]  Herman Medwin,et al.  In situ acoustic measurements of microbubbles at sea , 1977 .

[3]  Herman Medwin,et al.  Acoustical determinations of bubble‐size spectra , 1977 .

[4]  R. C. Cooke,et al.  Bubble populations and spectra in coastal waters: A photographic approach , 1979 .

[5]  A. Lovik Acoustic Measurements of the Gas Bubble Spectrum in Water , 1980 .

[6]  Jin Wu,et al.  Bubble populations and spectra in near‐surface ocean: Summary and review of field measurements , 1981 .

[7]  S. Thorpe,et al.  On the clouds of bubbles formed by breaking wind-waves in deep water, and their role in air-sea gas transfer , 1982, Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences.

[8]  T. Blanc Variation of Bulk-Derived Surface Flux, Stability, and Roughness Results Due to the Use of Different Transfer Coefficient Schemes , 1985 .

[9]  Ferren Magintyre,et al.  On Reconciling Optical and Acoustical Bubble Spectra in the Mixed Layer , 1986 .

[10]  V. A. Akulichev,et al.  The Study of Sound Backscattering From Microinhomogeneities in Sea Water , 1987 .

[11]  S. Baldy,et al.  Bubbles in the close vicinity of breaking waves: Statistical characteristics of the generation and dispersion mechanism , 1988 .

[12]  Luca d'Agostino,et al.  Comparison of Holographic and Coulter Counter Measurements of Cavitation Nuclei in the Ocean , 1988 .

[13]  S. Ling,et al.  Optical Microbubble Measurements in the North Sea , 1988 .

[14]  Herman Medwin,et al.  Instrumentation for in situ acoustical measurements of bubble spectra under breaking waves , 1989 .