Changes in aerosol content and temperature in the antarctic spring stratosphere - Lidar measurement at Syowa station (69 deg 00 min S, 39 deg 35 min E) in 1983, 1984 and 1985

Details Changes in aerosol content and temperature in the antarctic spring stratosphere - Lidar measurement at Syowa station (69 deg 00 min S, 39 deg 35 min E) in 1983, 1984 and 1985 Changes in aerosol content and temperature in the antarctic spring stratosphere - Lidar measurement at Syowa station (69 deg 00 min S, 39 deg 35 min E) in 1983, 1984 and 1985

Dec 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986georl..13.1407i&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 13, Dec. 1986, p. 1407-1410.

Physics

12

Aerosols, Antarctic Regions, Atmospheric Temperature, Optical Radar, Stratosphere, Ozone, Ozone Depletion, Radar Measurement, Spring (Season), Volcanoes

Scientific paper

Measurements on stratosheric aerosols at Syowa Station in 1983, 1984 and 1985 are described. The year-to-year changes in aerosol content were influenced by volcanic eruption of El Chichon (spring 1982, Mexico) and variations of stratospheric temperature. The aerosol load in winter of 1983 was about five times larger than the load of 1985. The particle content of spring 1985 was larger than that of spring 1983 even though the effect of the volcanic eruption was more severe in 1983. This may be a result of the decrease in average stratospheric temperature in spring. If heterogeneous reactions including the particles are indeed important for Antarctic oxone depletion, the rate of ozone depletion from heterogeneous reactions in the Antarctic spring must have increased from 1983 to 1985.

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