scholarly journals Stability of sonic boom metrics regarding signature distortions from atmospheric turbulence

2017 ◽  
Vol 141 (6) ◽  
pp. EL592-EL597 ◽  
Author(s):  
William J. Doebler ◽  
Victor W. Sparrow
Keyword(s):  
Atmospheric Turbulence ◽  
Sonic Boom

Evaluation of numerical predictions of sonic boom level variability due to atmospheric turbulence

2021 ◽  
Vol 149 (5) ◽  
pp. 3250-3260
Author(s):  
Trevor A. Stout ◽  
Victor W. Sparrow ◽  
Philippe Blanc-Benon
Keyword(s):  
Atmospheric Turbulence ◽  
Sonic Boom ◽  
Numerical Predictions

Numerical Evauation of Effect of Atmospheric Turbulence on Sonic Boom Observed in D-SEND#2 Flight Test

2017 ◽  
Author(s):  
Masashi Kanamori ◽  
Takashi Takahashi ◽  
Yusuke Naka ◽  
Yoshikazu Makino ◽  
Hidemi Takahashi ◽  
...  
Keyword(s):  
Atmospheric Turbulence ◽  
Flight Test ◽  
Sonic Boom

Modeling atmospheric turbulence as a filter for sonic boom propagation

2007 ◽  
Vol 55 (6) ◽  
pp. 495 ◽  
Author(s):  
Lance L. Locey ◽  
Victor W. Sparrow
Keyword(s):  
Atmospheric Turbulence ◽  
Sonic Boom

On the possibility of turbulent thickening of weak shock waves

1973 ◽  
Vol 58 (3) ◽  
pp. 461-480 ◽  
Author(s):  
J. E. Ffowcs Williams ◽  
M. S. Howe
Keyword(s):  
Shock Waves ◽  
Wave Packet ◽  
Wave Front ◽  
Atmospheric Turbulence ◽  
Upper Bound ◽  
Weak Shock ◽  
Sonic Boom ◽  
Wave Fronts ◽  
Sharp Wave ◽  
Nominal Position

This paper examines the possible thickening of an initially sharp sonic boom by the turbulence it encounters in passing to the ground. Three apparently different viewpoints, all indicating substantial thickening, are shown to be actually identical and to give an irrelevant upper bound on wave thickness. All three approaches describe only the apparent mean diffusion induced by random convection of a sharp wave about its nominal position. Although a wave-front folding mechanism ultimately accounts for an apparent thickening as individual rays are weakened and tangled by turbulence, this process is too slow to be effective in the practical boom situation. The paper then considers what linear thickening of a wave packet results from propagation trough atmospheric turbulence and concludes that, in the relevant limit, a wave may be thickened by a factor of about 2 at the most. The conclusion is therefore reached that atmospheric turbulence cannot be the cause of the thousandfold discrepancy between the measured wave fronts and their Taylor thickness.

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