Analysis of Moon impact flashes detected during the 2012 and 2013 Perseids
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We present the results of our Moon impact flashes detection campaigns performed around the maximum activity period of the Perseid meteor shower in 2012 and 2013. Just one flash produced by a Perseid meteoroid was detected in 2012 because of very unfavourable geometric conditions, but 12 of these were confirmed in 2013. The visual magnitude of the flashes ranged between 6.6 and 9.3. A luminous efficiency of 1.8 $\times$ 10$^{-3}$ has been estimated for meteoroids from this stream. According to this value, impactor masses would range between 1.9 and 190 g. In addition, we propose a criterion to establish, from a statistical point of view, the likely origin of impact flashes recorded on the lunar surface.
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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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