A method of measuring the temperature of the lower thermosphere

Details A method of measuring the temperature of the lower thermosphere A method of measuring the temperature of the lower thermosphere

Jun 1993

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1993jgr....98.9437b&link_type=abstract

Journal of Geophysical Research (ISSN 0148-0227), vol. 98, no. A6, p. 9437-9441.

Physics

7

Atmospheric Temperature, Nitric Oxide, Rotational Spectra, Temperature Measurement, Thermosphere, Airglow, Spectrum Analysis, Ultraviolet Spectra

Scientific paper

The temperature of the lower thermosphere between 110 and 140 km has been measured from the analysis of the rotational structure of the (1,1) nitric oxide gamma band in the ultraviolet dayglow. The ultraviolet spectra were obtained on a rocket experiment at Poker Flat, Alaska, at local noon on March 7, 1989. The temperatures were determined by generating synthetic spectra of the nitric oxide gamma bands and performing a multiple linear regression analysis of the rocket and synthetic spectra.

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