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arxiv: 1404.6458 · v1 · pith:C3FQ74ELnew · submitted 2014-04-25 · 🌌 astro-ph.EP

The Flux of Kilogram-Sized Meteoroids from Lunar Impact Monitoring

classification 🌌 astro-ph.EP
keywords fluxenergyflashesimpactlunarsizeimpactorsimpacts
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The flashes from meteoroid impacts on the Moon are useful in determining the flux of impactors with masses as low as a few tens of grams. A routine monitoring program at NASA's Marshall Space Flight Center has recorded over 300 impacts since 2006. A selection of 126 flashes recorded during periods of photometric skies was analyzed, creating the largest and most homogeneous dataset of lunar impact flashes to date. Standard CCD photometric techniques were applied to the video and the luminous energy, kinetic energy, and mass are estimated for each impactor. Shower associations were determined for most of the impactors and a range of luminous efficiencies was considered. The flux to a limiting energy of 2.5E-6 kT TNT or 1.05E7 J is 1.03E-7 km-2 hr-1 and the flux to a limiting mass of 30 g is 6.14E-10 m-2 yr-1 at the Moon. Comparisons made with measurements and models of the meteoroid population indicate that the flux of objects in this size range is slightly lower (but within error bars) than flux at this size from the near Earth object and fireball population by Brown et al. 2002. Size estimates for the crater detected by Lunar Reconnaissance Orbiter from a large impact observed on March 17, 2013 are also briefly discussed.

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Cited by 2 Pith papers

Reviewed papers in the Pith corpus that reference this work. Sorted by Pith novelty score.

  1. Mare versus highland lunar impact flash light curve dichotomy

    astro-ph.EP 2026-05 unverdicted novelty 5.0

    Lunar impact flashes on highlands exhibit shallower, longer-lasting decay than on mare terrain, driven by fine ejecta in dual-size cooling models and indicating lithology-dependent early cratering.

  2. Mare versus highland lunar impact flash light curve dichotomy

    astro-ph.EP 2026-05 unverdicted novelty 5.0

    Lunar impact flashes on highlands exhibit longer and shallower decay than on maria, with the dual-size ejecta model attributing the difference mainly to fine droplets and indicating lithology dependence in early cratering.