Synoptic-scale Wind Extremes
Synoptic-Scale Wind Extremes is a meteorological phenomenon characterized by intense wind events that arise from large-scale atmospheric pressure gradients associated with migratory extratropical cyclones and frontal systems, distinguishing it from convective or mesoscale wind extremes by its origin in baroclinic weather systems spanning hundreds to thousands of kilometers.
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3K
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182
Authors
112
Institutions
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2017–2026
12
Parents
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CLIMATOLOGY OF THE LOW LEVEL JET
William D. Bonner · Monthly Weather Review · 1968 · 683 citations · Full text
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Cooperative Institute for Research in Environmental Sciences, United States
2 publications · 106 citations
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1–5 of 182
112
NOAA National Severe Storms Laboratory
Norman, United States
3 h-index
3 publications
163 citations
University of Trás-os-Montes and Alto Douro
Vila Real, Portugal
3 h-index
4 publications
323 citations
University of Lisbon
Lisbon, Portugal
3 h-index
7 publications
539 citations

Agencia Estatal de Meteorología
Madrid, Spain
3 h-index
12 publications
250 citations
National Research Council
Rome, Italy
3 h-index
10 publications
1.1K citations

University of East Anglia
Norwich, United Kingdom
2 h-index
6 publications
264 citations
University of Colorado Boulder
Boulder, United States
2 h-index
4 publications
212 citations

The University of Melbourne
Melbourne, Australia
2 h-index
3 publications
144 citations
1–8 of 112
5 publications · 902 citations
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5 publications · 244 citations
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JGR · 4 publications · 437 citations
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3 publications · 53 citations
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3 publications · 202 citations
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