Temperature measurements in the earth's stratosphere using a limb scanning visible light spectrometer

Details Temperature measurements in the earth's stratosphere using a limb scanning visible light spectrometer Temperature measurements in the earth's stratosphere using a limb scanning visible light spectrometer

Apr 1983

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1983georl..10..261r&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 10, April 1983, p. 261-264.

Physics

7

Atmospheric Temperature, Ebert Spectrometers, Solar Mesosphere Explorer, Stratosphere, Temperature Measurement, Latitude, Light Scattering, Root-Mean-Square Errors, Temperature Profiles, Visible Spectrum

Scientific paper

The temperature of the earth's atmosphere between 40 and 50 km is inferred from measurements of Rayleigh scattered sunlight by a visible-light spectrometer on the Solar Mesosphere Explorer spacecraft. The RMS deviation of the satellite measurements from conventional rocket measurements is 5 K above 45 km and 2-3 K below 45 km. The satellite data are compared to the model temperatures for March 1982.

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