[Effect of the atmospheric ozone layer on the biologically active ultraviolet radiation on the earth's surface].
Based on measurements of the spectral irradiation intensity of UV-B global radiation by Bener (1960) and on the curve of spectral skin erythema effects newly measured by Urbach and Berger (1972), the biologically active UV-radiation at earth's surface has been calculated as a function of sun's altitude and atmospheric ozone content in so-called "Biological Units": BE = mWh cm-2 times erythema efficacy. On the basis of these data, the total daily, monthly, and yearly amounts of biologically active UV-radiation have been determined for the different geographical latitudes and various ozone contents. Approximately two thirds of BU hit the equatorial zone from 35 degrees south to 35 degrees north. Provided that the stratospheric ozone layer would be reduced by ten per cent from the exhaust gases of supersonic planes flying at high-altitude, an increase of BU would result amounting to 18% at the equator, to 19% in middle latitudes, and to 22% at the poles.
D000393:Air Pollutants; D000401:Aircraft; D000531:Altitude; D001272:Atmosphere; D004890:Erythema / Q000209:etiology; D005843:Geography; D006801:Humans; D009381:Neoplasms, Radiation-Induced; D010126:Ozone; D011829:Radiation Dosage; D011830:Radiation Effects; D012621:Seasons; D012878:Skin Neoplasms / Q000209:etiology; D013472:Sunlight; D014466:Ultraviolet Rays; D014894:Weights and Measures
D000393:Air Pollutants; D010126:Ozone
Der Einfluss der Ozonschicht der Atmosphäre auf die biologisch wirksame Ultraviolettstrahlung an der Erdoberfläche