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Effect of atmospheric variability and aircraft flight parameters on the refraction of sonic booms

机译:大气变化和飞机飞行参数对音爆波折射的影响

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This study deals with the potential audibility of sonic booms from supersonic aircraft at the ground as a consequence of the aircraft flight parameters and the atmospheric variability. A ray tracing model is used to decide whether a sonic boom emitted downwards by a high flying supersonic aircraft hits the ground or is refracted upwards before it reaches the ground. Aircraft altitude, speed, and flight direction are systematically changed within realistic ranges. The meteorological data rely on a homogeneous reanalysis dataset for eleven years over the domain of Europe with a very high vertical resolution. The cases of sonic booms hitting or not hitting the ground are identified for various situations and respective frequency distributions are derived. In addition, the angle of incidence of rays arriving at the ground and the turning-level height of rays not reaching the ground are studied as the intensity of sonic booms also depends on these parameters. It turned out that sonic-boom rays are refracted such that they do not reach the ground if the flight altitude is rather high (long propagation path) and the aircraft speed remains between Mach numbers of 1.05 and 1.25. Sonic-boom rays not reaching the ground are furthermore possible if the aircraft heading is mainly upwind, the temperature mostly increases along the propagation direction of the ray, and a wind speed maximum exists below flight level. The probability of sonic-boom rays not reaching the ground generally increases from north to south, but also depends on the season.
机译:这项研究处理了由于飞机飞行参数和大气多变性而导致的地面超音速飞机的声爆声的潜在可听性。射线追踪模型用于确定高空飞行的超音速飞机向下方发射的声波是撞击地面还是在到达地面之前向上折射。飞机的高度,速度和飞行方向会在实际范围内系统更改。气象数据依赖于欧洲范围内具有很高垂直分辨率的11年的均质再分析数据集。确定各种情况下的音爆臂撞击或不撞击地面的情况,并得出相应的频率分布。另外,由于声波强度也取决于这些参数,因此研究了到达地面的光线的入射角和未到达地面的光线的转弯高度。事实证明,如果飞行高度很高(较长的传播路径)并且飞机速度保持在1.05到1.25马赫数之间,则声波射线会折射,使得它们不会到达地面。如果飞机的飞行方向主要是逆风,则声波射线可能不会到达地面,温度大部分会沿着射线的传播方向增加,并且在飞行高度以下存在最大风速。声波射线未到达地面的可能性通常从北向南增加,但还取决于季节。

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