Lateral Stirring is a submesoscale oceanographic process that refers to the horizontal redistribution of tracers and momentum by transient eddies and fronts, distinguished from larger-scale advection and vertical mixing by its role in enhancing cross-frontal exchange and sharpening lateral gradients in density and velocity.
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1.2K
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92
Authors
44
Institutions
Publications per year
2017–2026
6
Parents
Publications
17
1–5 of 17
Authors
92
- KSK. Shafer Smith
Courant Institute of Mathematical Sciences, United States
2 publications · 187 citations
2
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- JM
2
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- JR
2
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- JK
2
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- JR
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1–5 of 92
Institutions
44
University of Washington Applied Physics Laboratory
Seattle, United States
2 h-index
2 publications
59 citations
Scripps Institution of Oceanography
La Jolla, United States
2 h-index
7 publications
160 citations
University of California San Diego
San Diego, United States
2 h-index
7 publications
160 citations
Laboratoire d’Études en Géophysique et Océanographie Spatiales
Toulouse, France
2 h-index
7 publications
344 citations
University of Victoria
Victoria, Canada
2 h-index
2 publications
175 citations
Woods Hole Oceanographic Institution
Falmouth, United States
2 h-index
7 publications
678 citations
Massachusetts Institute of Technology
Cambridge, United States
2 h-index
3 publications
274 citations
New York University
New York, United States
2 h-index
3 publications
244 citations
1–8 of 44
Venues
- Journal of Geophysical Research Oceans
2 publications · 71 citations
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- Journal of Physical Oceanography
2 publications · 71 citations
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- Journal of the Marine Biological Association of the United Kingdom
JMBA · 1 publications · 153 citations
1
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- Journal of Crystal Growth
1 publications · 25 citations
1
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- Journal of Geophysical Research Atmospheres
JGR · 1 publications · 90 citations
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