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Long-wavelength Cloud Rolls Over the Arctic Ice
Authors:George Chimonas
Institution:(1) School of Earth and Atmospheric Sciences, Georgia Institute of Technology, Atlanta, Georgia, 30332-0340, U.S.A.
Abstract:Cloud bands observed over the Arctic sea ice are interpreted in terms of long-wavelength gravity-wave modes trapped between the ground and a vertically-thin over-reflecting layer in the mid-troposphere. The over-reflecting layer is neutrally-stratified and lies between the counter-streaming upper troposphere and lower troposphere in a strong high-pressure system. The Arctic cloud bands appear to share many features with the long-wavelength roll waves observed in more temperate latitudes.
Keywords:Atmospheric layering  Atmospheric waves  Cloud bands  Over reflection  Roll waves
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