On 11 September 2013, an unusually long and bright impact flash was observed on the Moon. Its peak luminosity was equivalent to a stellar magnitude of around 2.9.
What happened? A meteorite with a mass of around 400 kg hit the lunar surface at a speed of over 61,000 kilometres per hour.
Rocks often collide with the lunar surface at high speed (tens of thousands of kilometres per hour) and are instantaneously vaporised at the impact site. This gives rise to a thermal glow that can be detected by telescopes from Earth as short duration flashes. These flashes, in general, last just a fraction of a second.
The extraordinary flash in September was recorded from Spain by two telescopes operating in the framework of the Moon Impacts Detection and Analysis System (MIDAS). These devices were aimed to the same area in the night side of the Moon. With a duration of over eight seconds, this is the brightest and longest confirmed impact flash ever recorded on the Moon.
Our calculations show that the impact, which took place at 20:07 GMT, created a new crater with a diameter of around 40 meters in Mare Nubium. This rock had a size raging between 0.6 and 1.4 metres. The impact energy was equivalent to over 15 tons of TNT under the assumption of a luminous efficiency of 0.002 (the fraction of kinetic energy converted into visible radiation as a consequence of the hypervelocity impact).
The detection of impact flashes is one of the techniques suitable to analyze the flux of incoming bodies to the Earth. One of the characteristics of the lunar impacts monitoring technique is that it is not possible to unambiguously associate an impact flash with a given meteoroid stream. Nevertheless, our analysis shows that the most likely scenario is that the impactor had a sporadic origin (i.e., was not associated to any known meteoroid stream). From the analysis of this event we have learnt that that one metre-sized objects may strike our planet about ten times as often as previously thought.
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