Detection of sporadic impact flashes on the Moon: Implications for the luminous efficiency of hypervelocity impacts and derived terrestrial impact rates |
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Authors: | J.L. Ortiz,F.J. Aceituno,J. Aceituno,P. Santos-Sanz,J. Llorca,F.J. Martí n-Torres,E. Pallé |
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Affiliation: | a Instituto de Astrofísica de Andalucía, CSIC, Apt. 3004, Camino Bajo de Huetor 50, 18080 Granada, Spain b Huétor Santillán Observatory, Avda Puente Nuevo 27, 18183 Huétor-Santillán, Granada, Spain c Centro Astronómico Hispano-Alemán de Calar Alto, Almería, Apt. 04004, Almería, Spain d Institut de Ciències de l'Espai (CSIC) Campus UAB, Facultat de Ciencies, 08193 Bellaterra (Barcelona), Spain e Institut d'Estudis Espacials de Catalunya (IEEC), Campus UAB, Facultat de Ciencies, 08193 Bellaterra (Barcelona), Spain f Institut de Tècniques Energètiques, Univ. Politècnica de Catalunya, 08028 Barcelona, Spain g Analytical Services and Materials, Inc., 107 Research Drive, Hampton, VA 23666, USA h Big Bear Solar Observatory, New Jersey Institute of Technology, Big Bear City, CA 92314-9672, USA |
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Abstract: | We present the first redundant detection of sporadic impact flashes on the Moon from a systematic survey performed between 2001 and 2004. Our wide-field lunar monitoring allows us to estimate the impact rate of large meteoroids on the Moon as a function of the luminous energy received on Earth. It also shows that some historical well-documented mysterious lunar events fit in a clear impact context. Using these data and traditional values of the luminous efficiency for this kind of event we obtain that the impact rate on Earth of large meteoroids (0.1-10 m) would be at least one order of magnitude larger than currently thought. This discrepancy indicates that the luminous efficiency of the hypervelocity impacts is higher than 10−2, much larger than the common belief, or the latest impact fluxes are somewhat too low, or, most likely, a combination of both. Our nominal analysis implies that on Earth, collisions of bodies with masses larger than 1 kg can be as frequent as 80,000 per year and blasts larger than 15-kton could be as frequent as one per year, but this is highly dependent on the exact choice of the luminous efficiency value. As a direct application of our results, we expect that the impact flash of the SMART-1 spacecraft should be detectable from Earth with medium-sized telescopes. |
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Keywords: | Impact processes Moon Collisional physics Cratering |
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