Buoyancy-driven Convection
Buoyancy-Driven Convection is a physical process in which fluid motion in shelf seas is generated by density differences arising from temperature or salinity gradients, leading to vertical mixing as a result of gravitational instability.
426
Publications
21.3K
Citations
952
Authors
439
Institutions
Publications per year
2017–2026
77
Parents
426
Open‐ocean convection: Observations, theory, and models
John Marshall, Friedrich Schott · Reviews of Geophysics · 1999 · 1.3K citations
On thermohaline convection with linear gradients
Peter G. Baines, A. E. Gill · Journal of Fluid Mechanics · 1969 · 380 citations
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439
Université Libre de Bruxelles
Brussels, Belgium
17 h-index
47 publications
2.7K citations
University of Cambridge
Cambridge, United Kingdom
17 h-index
32 publications
2.5K citations

Centre National de la Recherche Scientifique
Paris, France
14 h-index
36 publications
2.3K citations

Chinese Academy of Sciences
Beijing, China
12 h-index
34 publications
827 citations
Seoul National University
Seoul, South Korea
12 h-index
19 publications
345 citations
Cheju Halla University
Jeju City, South Korea
11 h-index
17 publications
263 citations
Stanford University
Stanford, United States
10 h-index
24 publications
1.7K citations
Institute of Mechanics
Beijing, China
10 h-index
31 publications
790 citations
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47 publications · 3.6K citations
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55 publications · 2.7K citations
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17 publications · 736 citations
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17 publications · 554 citations
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PRE · 14 publications · 622 citations
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