Current Divergence
Current Divergance is a geophysical phenomenon characterized as a vector field property in ocean surface currents where the horizontal outflow of water from a given region exceeds the inflow, resulting in a net displacement of surface water masses and often inducing upwelling or downwelling effects in the marine boundary layer.
65
Publications
5K
Citations
166
Authors
109
Institutions
Publications per year
2017–2026
5
Parents
65
Axial Vector Current Conservation in Weak Interactions
Y. Nambu · Physical Review Letters · 1960 · 1.1K citations · Full text
Self-potential modeling from primary flows
W.R. Sill · Geophysics · 1983 · 330 citations
1–5 of 65
166
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Space Environment Corporation (United States), United States
2 publications · 398 citations
2
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Max Planck Institute for Extraterrestrial Physics, Germany
2 publications · 398 citations
2
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2
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1
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1–5 of 166
109
University of Utah
Salt Lake City, United States
3 h-index
5 publications
384 citations
Nagoya University
Nagoya, Japan
3 h-index
4 publications
89 citations
University of Colorado Boulder
Boulder, United States
3 h-index
6 publications
172 citations

Centre National de la Recherche Scientifique
Paris, France
3 h-index
3 publications
102 citations
Stanford University
Stanford, United States
2 h-index
2 publications
311 citations
Max Planck Institute for Physics
Munich, Germany
2 h-index
4 publications
264 citations
National Oceanic and Atmospheric Administration
Washington, United States
2 h-index
3 publications
97 citations

University of Alberta
Edmonton, Canada
2 h-index
4 publications
78 citations
1–8 of 109
JGR · 5 publications · 519 citations
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4 publications · 144 citations
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PRL · 4 publications · 1.8K citations
4
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4 publications · 612 citations
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3 publications · 163 citations
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