Abstract The PMR ch. 3000 radiance data are correlated with temperatures from a reference atmosphere at 85 and 90 km to obtain mean temperature fields at these heights. Another technique for this purpose is to extrapolate upwards temperature fields given by the Barnett-Corney model for the stratosphere and mesosphere. The results of the two techniques agree well. The temperature fields in the lower thermosphere are briefly analysed.
Mean temperature fields in the lower thermosphere
Advances in Space Research ; 10 , 6 ; 13-16
1989-01-01
4 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
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