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.
Theory of sputtering
2 Pith papers cite this work. Polarity classification is still indexing.
2
Pith papers citing it
years
2026 2representative citing papers
BCA codes fail to reproduce both sputter yields and angular distributions for He-irradiated minerals, revealing a structural limitation when modeling rough or porous planetary surfaces.
citing papers explorer
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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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Limitations of Using BCA Codes for Modeling the Sputtering Behavior of Planetary Surfaces
BCA codes fail to reproduce both sputter yields and angular distributions for He-irradiated minerals, revealing a structural limitation when modeling rough or porous planetary surfaces.