“…With the advent of new ground‐based and space‐borne observations of the Moon there exists new interest in understanding the differences between the lunar and terrestrial meteoroid environments. Like for the case of Mercury (Pokorný et al, , ), modeling the meteoroid flux on the Moon is critical for understanding the importance of impact vaporization as a source for the lunar exosphere (Bruno et al, ; Cremonese et al, ; Morgan et al, ; Morgan & Killen, ; Sarantos et al, ), as meteoroids in the size range of 5–200 μm are considered relevant to the daily resupply of the lunar atmosphere. The importance of impacts for the exosphere was demonstrated by the brightening of its sodium and potassium component during meteor showers (Barbieri et al, ; Colaprete et al, ; Smith et al, ; Szalay et al, ).…”