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首页> 外文期刊>The Journal of the Acoustical Society of America >Scattering of sonic booms by anisotropic turbulence in the atmosphere
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Scattering of sonic booms by anisotropic turbulence in the atmosphere

机译:大气中各向异性湍流对音爆的散射

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摘要

An earlier paper [J. Acoust. Soc. Am. 98, 3412-3417 (1995)] reported on the comparison of rise times and overpressures of sonic booms calculated with a scattering center model of turbulence to measurements of sonic boom propagation through a well-characterized turbulent layer under moderately turbulent conditions. This detailed simulation used spherically symmetric scatterers to calculate the percentage of occurrence histograms of received overpressures and rise times. In this paper the calculation is extended to include distorted ellipsoidal turbules as scatterers and more accurately incorporates the meteorological data into a determination of the number of scatterers per unit volume. The scattering center calculation overpredicts the shifts in rise times for weak turbulence, and still underpredicts the shift under more turbulent conditions. This indicates that a single-scatter center-based model cannot completely describe sonic boom propagation through atmospheric turbulence.
机译:较早的论文[J. co Soc。上午。 98,3412-3417(1995)]报道了用湍流的散射中心模型计算的声波臂的上升时间和超压与在中等湍流条件下通过良好表征的湍流层传播的声波臂的测量的比较。这个详细的模拟使用球对称散射体来计算接收到的超压和上升时间的出现直方图的百分比。在本文中,将计算范围扩展到包括变形的椭圆形湍流作为散射体,并更准确地将气象数据纳入确定每单位体积散射体的数量。散射中心的计算过高地预测了弱湍流上升时间的变化,而在较湍流的条件下仍低估了该变化。这表明基于单散射中心的模型不能完全描述声波通过大气湍流的传播。

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