Upper-level Trough Dynamics
Upper-Level Trough Dynamics is a theoretical framework within atmospheric dynamics that characterizes the evolution, propagation, and associated baroclinic instability of large-scale cyclonic curvature in the upper-tropospheric flow, distinguishing it by its emphasis on the vertical coupling between potential vorticity anomalies and synoptic-scale wave development.
111
Publications
6.2K
Citations
306
Authors
159
Institutions
Publications per year
2017–2026
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159

NSF National Center for Atmospheric Research
Boulder, United States
4 h-index
7 publications
304 citations
Seoul National University
Seoul, South Korea
4 h-index
9 publications
758 citations
University of Washington
Seattle, United States
4 h-index
10 publications
942 citations
Johannes Gutenberg University Mainz
Mainz, Germany
4 h-index
6 publications
195 citations
University of Maryland, College Park
College Park, United States
4 h-index
8 publications
367 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
11 publications
390 citations
Ludwig-Maximilians-Universität München
Munich, Germany
3 h-index
4 publications
76 citations
National Institute of Meteorology
Tunis, Tunisia
3 h-index
4 publications
173 citations
1–8 of 159
38 publications · 2.8K citations
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10 publications · 470 citations
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6 publications · 252 citations
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5 publications · 246 citations
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3 publications · 352 citations
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