Cyclonic Vortex Formation
Cyclonic Vortex Formation is a mesoscale atmospheric process characterized by the development of a rotating low-pressure system in which the Coriolis effect induces counterclockwise (in the Northern Hemisphere) or clockwise (in the Southern Hemisphere) wind circulations that intensify through convergent inflow and vertical motion within synoptic or convective weather systems.
221
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11.6K
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541
Authors
237
Institutions
Publications per year
2017–2026
34
Parents
221
A Vortical Hot Tower Route to Tropical Cyclogenesis
Michael T. Montgomery, Melville E. Nicholls, Thomas Cram et al. · Journal of the Atmospheric Sciences · 2006 · 574 citations · Full text
Ocean convergence and the dispersion of flotsam
Eric A. D’Asaro, Andrey Shcherbina, Jody Klymak et al. · Proceedings of the National Academy of Sciences · 2018 · 301 citations · Full text
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Institute of Atmospheric Physics
Beijing, China
10 h-index
32 publications
1.2K citations

Chinese Academy of Sciences
Beijing, China
10 h-index
32 publications
1.2K citations

NSF National Center for Atmospheric Research
Boulder, United States
9 h-index
16 publications
1.4K citations
Woods Hole Oceanographic Institution
Falmouth, United States
9 h-index
12 publications
716 citations

Instituto Nacional de Pesquisas Espaciais
São José dos Campos, Brazil
8 h-index
19 publications
559 citations
University of Washington
Seattle, United States
7 h-index
14 publications
2.5K citations

Centre National de la Recherche Scientifique
Paris, France
7 h-index
18 publications
710 citations
University at Albany, State University of New York
Albany, United States
7 h-index
10 publications
645 citations
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40 publications · 2.9K citations
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20 publications · 1.6K citations
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JGR · 12 publications · 722 citations
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11 publications · 832 citations
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11 publications · 414 citations
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