SIMULTANEOUS ACOUSTIC AND MICROWAVE BACKSCATTERING FROM THE SEA-SURFACE

Citation
Ph. Dahl et al., SIMULTANEOUS ACOUSTIC AND MICROWAVE BACKSCATTERING FROM THE SEA-SURFACE, The Journal of the Acoustical Society of America, 101(5), 1997, pp. 2583-2595
Citations number
51
Categorie Soggetti
Acoustics
ISSN journal
00014966
Volume
101
Issue
5
Year of publication
1997
Part
1
Pages
2583 - 2595
Database
ISI
SICI code
0001-4966(1997)101:5<2583:SAAMBF>2.0.ZU;2-2
Abstract
Simultaneous and coincident measurements of acoustic and microwave bac kscatter from the air/sea interface were obtained during Phase II of t he SAXON-FPN experiment in December 1992 and again in March 1993. The acoustic and microwave grazing angles were both set to 17 degrees, and the wavelengths were matched, being set to 2.14, 3.00, and 5.66 cm, c orresponding to, respectively, acoustic frequencies of 26.5, 50, and 7 0 kHz and microwave frequencies of 5.3, 10, and 14 GHz. Backscattering cross sections normalized by ensonified area for the acoustic (sigma( 0)(a)) and microwave (sigma(0)(m)) returns were determined, and their dependence on wind speed was investigated. The acoustic scattering str ength is defined as 10 log(10)(sigma(0)(a)) and the microwave scatteri ng strength is defined as 10 log(10)(sigma(0)(m))-10 log(10)(4 pi). Th e 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 Scatterin g strength with increasing wind speed until reaching saturation. If th ese wind-speed dependencies are represented by a power law, U-n, then n is 5-6 for sigma(0)(m) and 2-4 for sigma(0)(m) for wind speeds betwe en 2 and 7 m/s. This difference is ascribed to the effect of bubbles o n the acoustic backscatter. The more rapid increase of sigma(0)(a) com pared to sigma(0)(m) implies that for our 17 degrees grazing angle aco ustic 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 acous tic frequencies. The bubble densities required to fit the data agree w ell with previous measurements of near-surface bubble distributions. T he model predicts an overshoot of the acoustic scattering strength (ab ove the saturation level) at moderate wind speeds which is clearly see n in the data at 26.5 and 70 kHz. Finally, a composite surface scatter ing model is utilized for the pure surface scattering component along with the bubble model to predict the wind-speed dependence of the acou stic scattering strength at a 45 degrees grazing angle and compare the results with earlier measurements. (C) 1997 Acoustical Society of Ame rica.