Planetary Wave Dynamics
Planetary Wave Dynamics is a theoretical framework within atmospheric dynamics that describes the propagation and evolution of large-scale, low-frequency Rossby waves in the presence of mean flow and topographic forcing, distinguishing it from other wave models by its explicit incorporation of β-plane approximation and quasigeostrophic potential vorticity conservation to explain teleconnections in mid-latitude synoptic-scale systems.
1.3K
Publications
88.2K
Citations
2.1K
Authors
618
Institutions
Publications per year
2017–2026
183
1.3K
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NSF National Center for Atmospheric Research, United States
26 publications · 2.1K citations
22
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618

NSF National Center for Atmospheric Research
Boulder, United States
55 h-index
186 publications
14.3K citations
University of Colorado Boulder
Boulder, United States
41 h-index
157 publications
9.4K citations
NSF NCAR High Altitude Observatory
Boulder, United States
34 h-index
88 publications
6.8K citations
Goddard Space Flight Center
Greenbelt, United States
32 h-index
118 publications
6.3K citations
University of Washington
Seattle, United States
31 h-index
59 publications
18.4K citations

United States Naval Research Laboratory
Washington, United States
26 h-index
60 publications
3K citations
University of Cambridge
Cambridge, United Kingdom
24 h-index
40 publications
10.9K citations
Cooperative Institute for Research in Environmental Sciences
Boulder, United States
23 h-index
56 publications
3.8K citations
1–8 of 618
261 publications · 19.9K citations
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JGR · 157 publications · 11.7K citations
64
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130 publications · 7.2K citations
51
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54 publications · 5.9K citations
41
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51 publications · 7K citations
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