The relationship between erythemal UV and ozone, derived from spectral irradiance measurements

Details The relationship between erythemal UV and ozone, derived from spectral irradiance measurements The relationship between erythemal UV and ozone, derived from spectral irradiance measurements

Dec 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991georl..18.2269m&link_type=abstract

Geophysical Research Letters (ISSN 0094-8276), vol. 18, Dec. 1991, p. 2269-2272.

Physics

56

Atmospheric Attenuation, Ozonometry, Solar Radiation, Ultraviolet Radiation, Ultraviolet Spectroscopy, Cloud Cover, Solar Position, Total Ozone Mapping Spectrometer

Scientific paper

Spectral measurements of solar UV radiation received at the ground at Lauder, New Zealand (45 deg S) during 1990 are used in conjunction with ozone total column measurements to investigate the relative importance to erythemally active UV radiation of variations in solar zenith angle, ozone, and cloud cover. At this site solar zenith angle variations are the dominant factor, but clouds frequently attenuate the clear sky irradiances by more than 50 percent. Ozone reductions of 1 percent typically cause an increase in erythemally active UV irradiance of 1.25 +/- 0.20 percent.

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