caa a22 4500 475777360 CHVBK 20180406123634.0 cr unu---uuuuu 170329e20000101xx s 000 0 eng 10.1023/A:1002494229431 doi (NATIONALLICENCE)springer-10.1023/A:1002494229431 Chimonas George School of Earth and Atmospheric Sciences, Georgia Institute of Technology, 30332-0340, Atlanta, Georgia, U.S.A. aut Long-wavelength Cloud Rolls Over the Arctic Ice [Elektronische Daten] [George Chimonas] 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. Kluwer Academic Publishers, 2000 Atmospheric layering nationallicence Atmospheric waves nationallicence Cloud bands nationallicence Over reflection nationallicence Roll waves nationallicence Boundary-Layer Meteorology Kluwer Academic Publishers 94/1(2000-01-01), 89-113 0006-8314 94:1<89 2000 94 10546 https://doi.org/10.1023/A:1002494229431 text/html Onlinezugriff via DOI 1 research-article jats NATIONALLICENCE 856 40 https://doi.org/10.1023/A:1002494229431 text/html Onlinezugriff via DOI NATIONALLICENCE 100 1- Chimonas George School of Earth and Atmospheric Sciences, Georgia Institute of Technology, 30332-0340, Atlanta, Georgia, U.S.A aut NATIONALLICENCE 773 0- Boundary-Layer Meteorology Kluwer Academic Publishers 94/1(2000-01-01), 89-113 0006-8314 94:1<89 2000 94 10546 Metadata rights reserved Springer special CC-BY-NC licence nationallicence BK010053 XK010053 XK010000 NATIONALLICENCE NATIONALLICENCE NL-springer