The measurement of ozone concentrations at high latitude during the twilight

Details The measurement of ozone concentrations at high latitude during the twilight The measurement of ozone concentrations at high latitude during the twilight

Feb 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977p%26ss...25..165l&link_type=abstract

Planetary and Space Science, vol. 25, Feb. 1977, p. 165-172.

Computer Science

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7

Arctic Regions, Atmospheric Composition, Night Sky, Ozone, Upper Atmosphere, Atmospheric Heating, Balloon Sounding, Gas Composition, Mesosphere, Photometry, Stratosphere, Stratospheric Warming, Winter

Scientific paper

The ozone height profile in the Arctic at the end of winter has been measured up to an altitude of 100 km using a combined solar-occultation and 1.27-micron oxygen-emission technique. The typical two-layer structure has been observed with a high-altitude minimum near 80 km and a maximum at 86 km. The measured concentration in this ozone bulge was 51 million per cu cm, typical of that measured at 52 deg N for the summer months. It is suggested that this reduced ozone concentration may have been associated with a stratospheric warming event that was in progress at the time of the measurement.

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