Coordinated observations of a ~45 g earthgrazing fireball localize thermospheric shock generation to volatile-enhanced hydrodynamic shielding that enables continuum-like flow and detectable infrasound.
The Journal of the Acoustical Society of America 141, 2681- 2692,10.1121/1.4980096
2 Pith papers cite this work, alongside 48 external citations. Polarity classification is still indexing.
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Sakurai blast radius formulation matches observed infrasound periods from OSIRIS-REx reentry with 9% median absolute percentage residual, outperforming Mach-diameter approximation by factor of three.
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Shock wave formation in the thermosphere by an earthgrazing fireball: Empirical evidence for volatile-enhanced hydrodynamic shielding
Coordinated observations of a ~45 g earthgrazing fireball localize thermospheric shock generation to volatile-enhanced hydrodynamic shielding that enables continuum-like flow and detectable infrasound.
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Benchmarking Cylindrical Blast Wave Theory Against the OSIRIS-REx Sample Return Capsule Reentry
Sakurai blast radius formulation matches observed infrasound periods from OSIRIS-REx reentry with 9% median absolute percentage residual, outperforming Mach-diameter approximation by factor of three.