作者: G. Sonnemann , Ch. Kremp , A. Ebel , U. Berger
DOI: 10.1016/S1352-2310(98)00113-7
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摘要: Abstract A global three-dimensional model of the dynamics and chemistry mesosphere—lower thermosphere region (30–150 km) has been developed. This is used to calculate distributions most important minor plasma constituents. Additionally, mass fluxes those constituents subjected transport chemical heating rates have computed. In view connection between stratospheric mesospheric odd-oxygen distribution, we concentrate here on discussing ozone at equinox.