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The effect of clouds and surface albedo on UV irradiances at a high latitude site
Author(s) -
Kylling A.,
Dahlback A.,
Mayer B.
Publication year - 2000
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/1999gl011015
Subject(s) - snow , albedo (alchemy) , environmental science , total ozone mapping spectrometer , irradiance , atmospheric sciences , latitude , cloud cover , snow cover , ozone , climatology , meteorology , ozone layer , geology , cloud computing , physics , stratosphere , optics , art , geodesy , performance art , computer science , art history , operating system
At high latitudes the Earth's surface is covered by snow large parts of the year. In spring the snow cover significantly increases UV radiation for cloudless as well as cloudy situations. In Tromsø (69.65° N, 18.95° E), Norway, independent measurements have been made of the effective regional spectral surface albedo, the total ozone column, the effective cloud optical depth, and the surface UV irradiance. These measurements are used together with model simulations to study the effect of snow and clouds on surface erythemal radiation doses. Snow on the surface increases the monthly erythemal doses by more than 20%. Relative to cloudless sky, the clouds reduce the monthly erythemal doses by 20–40%. During snow free conditions monthly doses derived from Earth Probe/Total Ozone Mapping Spectrometer (EP‐TOMS) total ozone and cloud reflectivity agree with the measurements within the experimental uncertainties. In presence of snow, however, the EP‐TOMS derived data are too low by 30–40% due to snow covered surfaces being misinterpreted as clouds.