Wave-Mean Flow Interaction is a dynamical process in atmospheric dynamics and dynamic meteorology whereby atmospheric waves (such as planetary or gravity waves) systematically exchange momentum, energy, and potential vorticity with the large-scale, typically zonally averaged, mean flow through wave-induced fluxes and nonlinear correlations, thereby modifying both the mean circulation and the wave field.
655
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37.8K
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1.1K
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453
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Publications per year
2017–2026
72
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655
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1.1K
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13
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453
University of Washington
Seattle, United States
21 h-index
35 publications
4.2K citations
NSF National Center for Atmospheric Research
Boulder, United States
20 h-index
32 publications
2.4K citations
University of Cambridge
Cambridge, United Kingdom
19 h-index
30 publications
3.6K citations
Massachusetts Institute of Technology
Cambridge, United States
18 h-index
29 publications
2.3K citations
Centre National de la Recherche Scientifique
Paris, France
17 h-index
49 publications
2.1K citations
Princeton University
Princeton, United States
15 h-index
19 publications
1K citations
Goddard Space Flight Center
Greenbelt, United States
12 h-index
15 publications
1K citations
University of Chicago
Chicago, United States
12 h-index
20 publications
2.2K citations
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Venues
- Journal of the Atmospheric Sciences
155 publications · 9.8K citations
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- Journal of Fluid Mechanics
90 publications · 6.2K citations
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- Journal of Geophysical Research Atmospheres
JGR · 39 publications · 2.4K citations
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- Journal of Physical Oceanography
48 publications · 2.8K citations
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- Coastal Engineering
24 publications · 1.1K citations
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