Low-level Jet Dynamics
Low-Level Jet Dynamics is a meteorological phenomenon characterized by a localized maximum in the vertical profile of horizontal wind speed within the atmospheric boundary layer, distinguished from other boundary-layer flows by its strong vertical wind shear, diurnal variability, and association with stable nocturnal conditions over land or coastal regions.
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Authors
486
Institutions
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2017–2026
144
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579
CLIMATOLOGY OF THE LOW LEVEL JET
William D. Bonner · Monthly Weather Review · 1968 · 683 citations · Full text
Summer Monsoon Rainfalls in China
Yihui Ding · Journal of the Meteorological Society of Japan Ser II · 1992 · 663 citations · Full text
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Cooperative Institute for Research in Environmental Sciences, United States
10 publications · 1.4K citations
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NSF National Center for Atmospheric Research
Boulder, United States
28 h-index
73 publications
5.7K citations
University of Oklahoma
Norman, United States
21 h-index
77 publications
5.3K citations

Pennsylvania State University
State College, United States
15 h-index
30 publications
1.7K citations

Centre National de la Recherche Scientifique
Paris, France
14 h-index
32 publications
1.6K citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
14 h-index
30 publications
3.3K citations
University of Colorado Boulder
Boulder, United States
14 h-index
28 publications
2.2K citations

National Taiwan University
Taipei, Taiwan
13 h-index
22 publications
1.3K citations
Iowa State University
Ames, United States
13 h-index
33 publications
2.3K citations
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132 publications · 10.8K citations
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67 publications · 5.2K citations
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39 publications · 3.9K citations
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25 publications · 1.9K citations
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23 publications · 1.6K citations
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