Frontal Cyclones
Frontal Cyclone is a synoptic-scale extratropical cyclone characterized by the presence of distinct frontal boundaries between air masses, which drive its development and precipitation patterns through baroclinic instability within the midlatitude westerlies.
143
Publications
7.8K
Citations
328
Authors
141
Institutions
Publications per year
2017–2026
15
Variants
Frontal Cyclone
143
Orographic effects on precipitating clouds
Robert A. Houze · Reviews of Geophysics · 2011 · 951 citations · Full text
1–5 of 143
328
University at Albany, State University of New York, United States
5 publications · 287 citations
5
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4
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3
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European Centre for Medium-Range Weather Forecasts, United Kingdom
3 publications · 96 citations
3
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3
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1–5 of 328
141
University of Reading
Reading, United Kingdom
11 h-index
21 publications
980 citations
University of Washington
Seattle, United States
8 h-index
14 publications
1.3K citations
University at Albany, State University of New York
Albany, United States
6 h-index
12 publications
736 citations
ETH Zurich
Zurich, Switzerland
6 h-index
14 publications
866 citations
Jet Propulsion Laboratory
Pasadena, United States
5 h-index
7 publications
236 citations
Meteorological Research Institute
Tsukuba, Japan
5 h-index
6 publications
246 citations

NSF National Center for Atmospheric Research
Boulder, United States
5 h-index
8 publications
231 citations
Columbia University
New York, United States
5 h-index
8 publications
839 citations
1–8 of 141
32 publications · 1.1K citations
18
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21 publications · 1.3K citations
18
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10 publications · 453 citations
10
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8 publications · 196 citations
8
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6 publications · 519 citations
6
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1–5