Low-level Wind Shear
Low-Level Wind Shear is a meteorological phenomenon characterized by a sudden, localized change in wind speed and/or direction within the lower altitudes of the atmosphere, typically below 2,000 feet above ground level, that poses significant hazards to aircraft during takeoff and landing.
145
Publications
8.9K
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401
Authors
155
Institutions
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2017–2026
46
145
GLOBAL VIEW OF THE ORIGIN OF TROPICAL DISTURBANCES AND STORMS
William M. Gray · Monthly Weather Review · 1968 · 1.9K citations · Full text
Vertical Structure of Thunderstorm Outflows
R. Craig Goff · Monthly Weather Review · 1976 · 363 citations · Full text
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NSF National Center for Atmospheric Research, United States
3 publications · 240 citations
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Pennsylvania State University
State College, United States
12 h-index
29 publications
2K citations

NSF National Center for Atmospheric Research
Boulder, United States
12 h-index
27 publications
1.5K citations
University of Oklahoma
Norman, United States
7 h-index
14 publications
1.4K citations
North Carolina State University
Raleigh, United States
6 h-index
15 publications
591 citations
NOAA National Severe Storms Laboratory
Norman, United States
6 h-index
12 publications
1.4K citations
Colorado State University
Fort Collins, United States
5 h-index
8 publications
459 citations
Hong Kong Observatory
Hong Kong, China
5 h-index
6 publications
177 citations
Massachusetts Institute of Technology
Cambridge, United States
5 h-index
22 publications
782 citations
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38 publications · 4.3K citations
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23 publications · 1.3K citations
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8 publications · 496 citations
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6 publications · 441 citations
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5 publications · 112 citations
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