Lunar impact flashes from Geminids, analysis of luminous efficiencies and the flux of large meteoroids on Earth
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We analyze lunar impact flashes recorded by our team during runs in December 2007, 2011, 2013 and 2014. In total, 12 impact flashes with magnitudes ranging between 7.1 and 9.3 in V band were identified. From these, 9 events could be linked to the Geminid stream. Using these observations the ratio of luminous energy emitted in the flashes with respect to the kinetic energy of the impactors for meteoroids of the Geminid stream is estimated. By making use of the known Geminids meteoroid flux on Earth we found this ratio to be 2.1x10$^{-3}$ on average. We compare this luminous efficiency with other estimations derived in the past for other meteoroid streams and also compare it with other estimations that we present here for the first time by making use of crater diameter measurements. We think that the luminous efficiency has to be revised downward, not upward, at least for sporadic impacts. This implies an increase in the influx of kilogram-sized and larger bodies on Earth that has been derived thus far through the lunar impact flash monitoring technique.
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Cited by 2 Pith papers
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Mare versus highland lunar impact flash light curve dichotomy
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.
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Mare versus highland lunar impact flash light curve dichotomy
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.
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