Abstract A non-steady one-dimensional model for middle latitude of the Earth's mesosphere and lower thermosphere at equinox condition specially adapted for twilight conditions is developed to obtain the temporal dependence of the photodissociation coefficients and the concentration of the different compounds. The temporal variations obtained are used to explain the diurnal behaviour of some atmospheric O2 and OH emissions.
Atmospheric composition during twilight
Advances in Space Research ; 13 , 1 ; 339-342
1992-01-01
4 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
TIBKAT | 1972
|Online Contents | 1993
|Elsevier | 1986
TIBKAT | 1978
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