Upper-level Jet Streams
Upper-Level Jet Streams is a type of atmospheric circulation characterized as a narrow, high-altitude band of strong, predominantly zonal winds occurring in the upper troposphere or lower stratosphere, distinguished by its association with large vertical and horizontal wind shear and its role in shaping synoptic-scale weather patterns.
84
Publications
4.2K
Citations
209
Authors
101
Institutions
Publications per year
2017–2026
25
Parents
84
1–5 of 84
209
5
h-index
University at Albany, State University of New York, United States
4 publications · 152 citations
4
h-index
University at Albany, State University of New York, United States
4 publications · 147 citations
4
h-index
National Institute of Water and Atmospheric Research, New Zealand
3 publications · 113 citations
3
h-index
National Oceanic and Atmospheric Administration, United States
3 publications · 259 citations
3
h-index
1–5 of 209
101
ETH Zurich
Zurich, Switzerland
6 h-index
20 publications
1.4K citations

NSF National Center for Atmospheric Research
Boulder, United States
6 h-index
7 publications
288 citations

Chinese Academy of Sciences
Beijing, China
6 h-index
10 publications
330 citations
University of Reading
Reading, United Kingdom
5 h-index
11 publications
986 citations
Albany State University
Albany, United States
5 h-index
10 publications
498 citations
University at Albany, State University of New York
Albany, United States
5 h-index
14 publications
610 citations
Chinese Academy of Meteorological Sciences
Beijing, China
4 h-index
14 publications
835 citations
Karlsruhe Institute of Technology
Karlsruhe, Germany
3 h-index
3 publications
188 citations
1–8 of 101
21 publications · 1.1K citations
17
h-index
11 publications · 1.2K citations
11
h-index
10 publications · 365 citations
10
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4 publications · 115 citations
4
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4 publications · 130 citations
4
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1–5