Equatorial Current Instability is a hydrodynamic phenomenon characterized by the spontaneous perturbation and breakdown of zonal equatorial ocean currents due to baroclinic or shear-induced instabilities arising from meridional gradients in potential vorticity and background flow asymmetry relative to the equator.
57
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2.8K
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117
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53
Institutions
Publications per year
2017–2026
4
Parents
Publications
57
1–5 of 57
Authors
117
- SG
4
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3
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1–5 of 117
Institutions
53
Chinese Academy of Sciences
Beijing, China
4 h-index
9 publications
317 citations
Institute of Oceanology
Qingdao, China
4 h-index
11 publications
359 citations
Massachusetts Institute of Technology
Cambridge, United States
3 h-index
3 publications
141 citations
Scripps Institution of Oceanography
La Jolla, United States
3 h-index
4 publications
201 citations
National Oceanic and Atmospheric Administration
Washington, United States
3 h-index
4 publications
151 citations
Qingdao National Laboratory for Marine Science and Technology
Qingdao, China
3 h-index
6 publications
100 citations
Physical Research Laboratory
Ahmedabad, India
3 h-index
13 publications
394 citations
CSIRO Oceans and Atmosphere
Canberra, Australia
2 h-index
3 publications
261 citations
1–8 of 53
Venues
- Journal of Geophysical Research Atmospheres
JGR · 15 publications · 926 citations
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- Journal of Physical Oceanography
6 publications · 439 citations
6
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- Journal of Atmospheric and Terrestrial Physics
5 publications · 238 citations
5
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- Geophysical Research Letters
4 publications · 188 citations
4
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- Deep Sea Research (1953)
3 publications · 56 citations
3
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1–5