Abstract Mesopause temperatures were derived from ground measurements of the near infrared OH∗ spectrum. Preliminary data are presented. Seasonal variations at Wuppertal (51° N, 7° E) are well represented if the Cole and Kantor (1978) model [1] is raised by 10 K and shifted by about 18 days. Latitudinal variations from 68° N to 51° N are found much smaller than the model variations. During a stratospheric warming, mesopause and stratosphere temperatures were found to be in anticorrelation only if a substantial longitudinal shift is introduced.
Variations of mesopause temperatures in Europe
Advances in Space Research ; 3 , 1 ; 21-23
1983-01-01
3 pages
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
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