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Simultaneous acoustic and microwave backscattering from the sea surface

 

作者: Peter H. Dahl,   William J. Plant,   Bernd Nützel,   Anke Schmidt,   Heinz Herwig,   Eugene A. Terray,  

 

期刊: The Journal of the Acoustical Society of America  (AIP Available online 1997)
卷期: Volume 101, issue 5  

页码: 2583-2595

 

ISSN:0001-4966

 

年代: 1997

 

DOI:10.1121/1.418500

 

出版商: Acoustical Society of America

 

数据来源: AIP

 

摘要:

Simultaneous and coincident measurements of acoustic and microwave backscatter from the air/sea interface were obtained during Phase II of the SAXON-FPN experiment in December 1992 and again in March 1993. The acoustic and microwave grazing angles were both set to 17°, and the wavelengths were matched, being set to 2.14, 3.00, and 5.66 cm, corresponding to, respectively, acoustic frequencies of 26.5, 50, and 70 kHz and microwave frequencies of 5.3, 10, and 14 GHz. Backscattering cross sections normalized by ensonified area for the acoustic(σ0a)and microwave(σ0m)returns were determined, and their dependence on wind speed was investigated. The acoustic scattering strength is defined as10 log10(σ0a)and the microwave scattering strength is defined as10 log10(σ0m)−10 log10(4π).The results of these experiments show that the two scattering strengths are comparable at wind speeds below about 3 m/s but that the acoustic scattering strength increases much faster than the microwave scattering strength with increasing wind speed until reaching saturation. If these wind-speed dependencies are represented by a power law,Un,thennis 5–6 forσ0aand 2–4 forσ0mfor wind speeds between 2 and 7 m/s. This difference is ascribed to the effect of bubbles on the acoustic backscatter. The more rapid increase ofσ0acompared toσ0mimplies that for our 17° grazing angle acoustic scattering from the surface is negligible at all but the lowest wind speeds. Therefore a simple model is used for bubble scattering to fit the acoustic data as a function of wind speed for all three acoustic frequencies. The bubble densities required to fit the data agree well with previous measurements of near-surface bubble distributions. The model predicts an overshoot of the acoustic scattering strength (above the saturation level) at moderate wind speeds which is clearly seen in the data at 26.5 and 70 kHz. Finally, a composite surface scattering model is utilized for the pure surface scattering component along with the bubble model to predict the wind-speed dependence of the acoustic scattering strength at a 45° grazing angle and compare the results with earlier measurements.

 

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