Charney-stern Criterion
The Charney-Stern Criterion is a theoretical condition in geophysical fluid dynamics that provides a necessary criterion for the onset of barotropic instability in a zonal flow by establishing bounds on the spatial gradients of absolute vorticity, thereby distinguishing stable from unstable configurations in the context of large-scale atmospheric and oceanic motions.
21
Publications
1.2K
Citations
34
Authors
21
Institutions
Publications per year
2017–2026
1
Variants
Charney-stern Theorem
Parents
21
Momentum Transport by Quasi-Geostrophic Eddies
Isaac M. Held · Journal of the Atmospheric Sciences · 1975 · 161 citations · Full text
1–5 of 21
34
3
h-index
3
h-index
2
h-index
2
h-index
University at Albany, State University of New York, United States
1 publications · 175 citations
1
h-index
1–5 of 34
21
Massachusetts Institute of Technology
Cambridge, United States
4 h-index
5 publications
109 citations
Colorado State University
Fort Collins, United States
2 h-index
6 publications
494 citations

University of Louisville
Louisville, United States
2 h-index
2 publications
33 citations

University of Toronto
Toronto, Canada
1 h-index
2 publications
52 citations

University of Oslo
Oslo, Norway
1 h-index
1 publications
49 citations
Texas Tech University
Lubbock, United States
1 h-index
1 publications
34 citations
NOAA Geophysical Fluid Dynamics Laboratory
Princeton, United States
1 h-index
2 publications
126 citations
New Mexico Institute of Mining and Technology
Socorro, United States
1 h-index
1 publications
18 citations
1–8 of 21
11 publications · 620 citations
11
h-index
3 publications · 365 citations
3
h-index
1 publications · 19 citations
1
h-index
1 publications · 26 citations
1
h-index
1 publications · 39 citations
1
h-index
1–5