Abstract
The problem of acoustic radiation propagation through a lower 500-m plane-stratified turbulent atmospheric layer has been solved by the Monte Carlo method. Statistical estimates of the contribution of multiply scattered radiation to the transmitted acoustic radiation intensity are obtained. A point omnidirectional source of monochromatic acoustic radiation was placed at a height of 35 m above the absorbing Earth’s surface. Statistical estimates of the contribution of multiply scattered radiation to the transmitted radiation intensity have shown that it does not exceed 15% for the outer scale of atmospheric turbulence L0 = 10 m and sound frequency F = 1700 Hz, reaches 30% for L0 = 20 m, and increases to 90% for L0 = 80 m. A comparison of the calculated results with the available experimental data demonstrates their satisfactory agreement.
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Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Fizika, No. 12, pp. 72–79, December, 2004.
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Shamanaeva, L.G., Burkatovskaya, Y.B. Statistical estimates of the contribution of multiply scattered radiation to the intensity of acoustic radiation transmitted through a lower 500-m atmospheric layer. Russ Phys J 47, 1297–1306 (2004). https://doi.org/10.1007/s11182-005-0070-9
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DOI: https://doi.org/10.1007/s11182-005-0070-9