Frontal Undulations
Frontal Undulations is a meteorological phenomenon characterized as a mesoscale distortion or wavelike deformation along a density front in the atmosphere, distinguished by localized variations in frontal slope and curvature that can initiate cyclogenesis or enhance horizontal moisture transport.
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219
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16
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8
Institutions
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2017–2026
0
Variants
Frontal Waves
Parents
4
E. M. Dewan, R. H. Picard · Journal of Geophysical Research Atmospheres · 1998 · 106 citations · Full text
Jeremy Leggett, Yutaka Aoki, T. Toba · Marine and Petroleum Geology · 1985 · 48 citations
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Don Carlo Gnocchi Foundation
Milan, Italy
1 h-index
6 publications
120 citations

University of Milan
Milan, Italy
1 h-index
5 publications
100 citations
Japan Petroleum Energy Center
Tokyo, Japan
1 h-index
1 publications
48 citations
GEOMAR Technologie GmbH - GTG
Kiel, Germany
1 h-index
5 publications
225 citations
Inpex (Japan)
Tokyo, Japan
1 h-index
1 publications
48 citations

Hanscom Air Force Base
Bedford, United States
1 h-index
2 publications
212 citations

Imperial College London
London, United Kingdom
1 h-index
1 publications
48 citations
Luigi Sacco Hospital
Milan, Italy
1 h-index
5 publications
100 citations
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1 publications · 20 citations
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JGR · 1 publications · 106 citations
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1 publications · 45 citations
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1 publications · 48 citations
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