Mixing By Double Diffusion
Mixing By Double Diffusion is a physical oceanographic process denoting the vertical transport of heat and salt in stratified fluids, where the differential molecular diffusion rates of temperature and salinity generate localized instabilities that drive turbulent mixing, distinct from mechanical or convective mechanisms.
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3.3K
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2017–2026
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Double Diffusion in Oceanography
Raymond W. Schmitt · Annual Review of Fluid Mechanics · 1994 · 530 citations
Two Years in the Life of a Mediterranean Salt Lens
Laurence Armi, Dave Hebert, Neil S. Oakey et al. · Journal of Physical Oceanography · 1989 · 296 citations · Full text
The East Greenland Polar Front in autumn
Robert G. Paquette, Robert H. Bourke, John F. Newton et al. · Journal of Geophysical Research Atmospheres · 1985 · 130 citations
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Columbia University
New York, United States
6 h-index
7 publications
169 citations

Goddard Institute for Space Studies
New York, United States
6 h-index
8 publications
192 citations

Scripps Institution of Oceanography
La Jolla, United States
5 h-index
6 publications
554 citations
Fisheries and Oceans Canada
Ottawa, Canada
3 h-index
3 publications
444 citations
University of California San Diego
San Diego, United States
3 h-index
4 publications
107 citations
Massachusetts Institute of Technology
Cambridge, United States
2 h-index
2 publications
66 citations

University of Hawaii System
Honolulu, United States
2 h-index
2 publications
83 citations

Helmholtz Centre for Environmental Research
Leipzig, Germany
2 h-index
4 publications
143 citations
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JGR · 11 publications · 493 citations
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8 publications · 607 citations
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6 publications · 160 citations
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5 publications · 123 citations
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5 publications · 183 citations
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