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Observed storminess patterns and trends in the circum-Arctic coastal regime
Authors:David E. Atkinson
Affiliation:(1) Bedford Institute of Oceanography, Geological Survey of Canada (Atlantic), 1 Challenger Drive, Dartmouth, NS, B3G 1E9, Canada;(2) Present address: Dept. of Atmospheric Sciences, International Arctic Research Center, University of Alaska Fairbanks, 930 Koyukuk Drive, Fairbank, AK 99775, USA
Abstract:Storm event statistics for the open-water season (June–October) were extracted from the terrestrial-based observational record throughout the circumpolar coastal regime over the period 1950–2000. The Barents/Norwegian and Kara regions exhibited an active spring/quiet summer signature typical of the mid-latitudes. The Kara and Laptev Sea regions had a strong June peak possibly associated with early sea ice breakup. The Chukchi sector exhibited large storm power values (defined as speed2*duration). Storm counts declined from 1950 to 1970, shifted rapidly from 1970 to 1974 to a level of greater mean activity and greater inter-annual variability, and declined after 1988.
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