Indication of increasing solar ultraviolet-B radiation flux in alpine regions

Details Indication of increasing solar ultraviolet-B radiation flux in alpine regions Indication of increasing solar ultraviolet-B radiation flux in alpine regions

Apr 1990

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1990sci...248..206b&link_type=abstract

Science (ISSN 0036-8075), vol. 248, April 13, 1990, p. 206-208. Research supported by the Oesterreichische Akademie der Wissensc

Physics

44

Alps Mountains (Europe), Ozone Depletion, Solar Radiation, Ultraviolet Radiation, Annual Variations, Ozonometry, Radiation Effects

Scientific paper

Measurements at the Jungfraujoch High Mountain Station (Swiss Alps, 47 deg N, 3576 meters above sea level) indicate that there has been a slight increase of about 1 percent per year in the flux of solar ultraviolet-B radiation (290 to 330 nanometers) since 1981. A Robertson-Berger detector was used to measure solar erythemal radiation. The increase can be related to a long-term ozone depletion.

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