O3 and NO2 ground-based measurements by visible spectrometry during Arctic winter and spring 1988

Details O3 and NO2 ground-based measurements by visible spectrometry during Arctic winter and spring 1988 O3 and NO2 ground-based measurements by visible spectrometry during Arctic winter and spring 1988

Aug 1988

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1988georl..15..891p&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 15, Aug. 1988, p. 891-894. Research supported by the Terres Australes et Ant

Physics

63

Atmospheric Temperature, Nitrogen Dioxide, Ozone, Photochemical Reactions, Stratosphere, Visible Spectrum, Arctic Regions, Diurnal Variations, Spring (Season), Wind Velocity, Winter

Scientific paper

Ozone and nitrogen dioxide were monitored using ground-based visible spectrometry from the Esrange base at Kiruna (Sweden) during January to April, 1988. The springtime radiative warming was found to begin in early March. On the average, ozone increased from 400 DU in January to 450 DU in March. The data indicate that diurnal and seasonal NO2 variations are closely associated with stratospheric temperature.

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