Wet snow icing upstream of mountains
Haraldur Ólafsson, University of Iceland, IS 150 Reykjavík, Iceland; and Á. J. Elíasson
A case of wet snow icing upstream of mountains is studied. A numerical simulation reveals that local effect of the mountains such as low level inversion upstream of the mountain, a corner wind and locally increased precipitation contribute to the severe icing. The simulation is successful in reproducing the local atmospheric conditions for the icing, suggesting that real-time local icing forecasts are within a reach.
Poster Session 1, Conference Posters
Monday, 1 August 2005, 5:30 PM-7:00 PM, Regency Ballroom
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