Rossby Wave Forcing
Rossby Wave Forcing is a theoretical construct in atmospheric and oceanic dynamics that denotes the large-scale redistribution of momentum and energy by Rossby waves, distinguishing it from other forcing mechanisms through its dependence on planetary vorticity gradients and potential vorticity anomalies.
201
Publications
11K
Citations
487
Authors
224
Institutions
Publications per year
2017–2026
52
Parents
201
The Influence of Nonlinear Mesoscale Eddies on Near-Surface Oceanic Chlorophyll
Dudley B. Chelton, Peter Gaube, Michael G. Schlax et al. · Science · 2011 · 693 citations
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Chinese Academy of Sciences
Beijing, China
10 h-index
30 publications
1.2K citations

NSF National Center for Atmospheric Research
Boulder, United States
9 h-index
12 publications
1K citations
University of Washington
Seattle, United States
9 h-index
16 publications
1.4K citations

Nanjing University of Information Science and Technology
Nanjing, China
8 h-index
17 publications
499 citations
Institute of Atmospheric Physics
Beijing, China
8 h-index
22 publications
1.1K citations

Scripps Institution of Oceanography
La Jolla, United States
6 h-index
10 publications
934 citations
Woods Hole Oceanographic Institution
Falmouth, United States
6 h-index
11 publications
263 citations

Ocean University of China
Qingdao, China
6 h-index
12 publications
237 citations
1–8 of 224
29 publications · 1.6K citations
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23 publications · 1K citations
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17 publications · 1K citations
15
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13 publications · 990 citations
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JGR · 11 publications · 862 citations
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