A new Monte Carlo type model of the lunar sodium atmosphere has been d
eveloped and applied to recent ground-based imaging observations. The
model assumes a steady state atmosphere with production of sodium due
to a spatially uniform source (e.g., meteor impact vaporization) or a
solar zenith angle dependent source (e.g., solar wind sputtering or ph
otodesorption). The loss processes included in the model are surface a
dsorption and photoionization. Solar radiation pressure is also accoun
ted for. The model output is analyzed for overall spatial structure an
d compared with recent observations and theory. The results indicate t
hat a sodium release mechanism that decreases in source rate with incr
easing solar zenith angle is best able to reproduce imaging data taken
on September 30, 1991.