Vorticity Shearing is a kinematic process in atmospheric dynamics, within the broader class of vorticity generation mechanisms, distinguished by the differential advection of vorticity due to spatial gradients in the horizontal wind field, leading to the deformation and stretching of air parcels that modulates the local vorticity distribution.
60
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2017–2026
13
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Publications
60
The instability of precessing flow
Rich R. Kerswell · Geophysical & Astrophysical Fluid Dynamics · 1993 · 145 citations
1–5 of 60
Authors
160
- RZ
2
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- LDL. Dell'Osso
European Centre for Medium-Range Weather Forecasts, United Kingdom
2 publications · 69 citations
2
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- MW
2
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- LL
2
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- XL
1
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1–5 of 160
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104
NSF National Center for Atmospheric Research
Boulder, United States
4 h-index
5 publications
385 citations
Chinese Academy of Meteorological Sciences
Beijing, China
3 h-index
7 publications
144 citations
Naval Postgraduate School
Monterey, United States
3 h-index
5 publications
235 citations
University of California San Diego
San Diego, United States
2 h-index
4 publications
60 citations
Newcastle University
Newcastle upon Tyne, United Kingdom
2 h-index
2 publications
173 citations
Columbia University
New York, United States
2 h-index
4 publications
57 citations
University of California, Los Angeles
Los Angeles, United States
2 h-index
6 publications
362 citations
Scripps Institution of Oceanography
La Jolla, United States
2 h-index
4 publications
60 citations
1–8 of 104
Venues
- Journal of the Atmospheric Sciences
4 publications · 251 citations
4
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- Journal of Structural Geology
3 publications · 101 citations
3
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- Monthly Weather Review
3 publications · 121 citations
3
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- Journal of Geophysical Research Atmospheres
JGR · 3 publications · 182 citations
3
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- Journal of Physical Oceanography
3 publications · 106 citations
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