Transient Eddy Forcing
Transient Eddy Forcing is a dynamical process in atmospheric and oceanic fluid dynamics wherein the convergence of momentum and heat by time-varying eddies exerts a forcing on the mean flow, distinct from steady or radiative forcings, thereby modulating the growth and evolution of baroclinic instabilities.
111
Publications
8.3K
Citations
237
Authors
103
Institutions
Publications per year
2017–2026
21
Parents
111
1–5 of 111
237
7
h-index
Laboratoire d’Études en Géophysique et Océanographie Spatiales, France
5 publications · 394 citations
5
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Cooperative Institute for Research in Environmental Sciences, United States
4 publications · 126 citations
4
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4
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4
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1–5 of 237
103
Nanjing University
Nanjing, China
12 h-index
34 publications
1.2K citations

Chinese Academy of Sciences
Beijing, China
8 h-index
13 publications
903 citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
7 h-index
10 publications
1K citations

NSF National Center for Atmospheric Research
Boulder, United States
6 h-index
6 publications
780 citations
Princeton University
Princeton, United States
6 h-index
7 publications
1K citations
University of Reading
Reading, United Kingdom
6 h-index
15 publications
1.4K citations

Nanjing University of Information Science and Technology
Nanjing, China
5 h-index
10 publications
293 citations

Lamont-Doherty Earth Observatory
Sparkill, United States
5 h-index
14 publications
1.4K citations
1–8 of 103
30 publications · 2.3K citations
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33 publications · 2.4K citations
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7 publications · 353 citations
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6 publications · 540 citations
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4 publications · 279 citations
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