A global three-dimensional model of the dynamics and chemistry of the
mesosphere-lower thermosphere region (30-150 km) has been developed. T
his model is used to calculate the distributions of the most important
minor and plasma constituents. Additionally, the mass fluxes of those
constituents subjected to transport and the chemical heating rates ha
ve been computed. In view of the connection between the stratospheric
and mesospheric odd-oxygen distribution, we concentrate here on discus
sing the mesospheric ozone chemistry at the equinox. (C) 1998 Elsevier
Science Ltd. All rights reserved.