A region of non-terrestrial sodium emission seen in the sky on the nights o
f November 18-20, 1998, has been interpreted as the Moon's distant sodium t
ail, possibly enhanced by micrometeor impact vaporization of the lunar rego
lith by the Leonid meteor shower. We show, that the location and morphology
of the spot can be explained by standard steady-state models of the Moon's
sodium atmosphere. Moreover, using a new time-dependent simulation of the
lunar atmosphere, we find that the Na escape rate from the Moon increased t
o 2 or 3 times its normal level during the most intense period of the 1998
Leonid meteor shower on November 16th and 17th.