A mechanism for layer formation in a double-diffusive fluid
By T. Radko. Journal of Fluid Mechanics, 2003
163 citations recorded by the source corpus.
Subfields: Earth-Surface Processes, Mechanics of Materials, Oceanography
View Paper: https://www.semanticscholar.org/paper/971e938345bbe78dcdce25d5cb1a7cecc62a740c
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In Earth-Surface Processes
In Mechanics of Materials
In Oceanography
Citations in the corpus
- A new vision of giant planet interiors: Impact of double diffusive convection (2012, background): “R−1min corresponds to the point where the solute to heat buoyancy flux ratio (≡ γ−1) stops decreasing when R−1ρ increases (see Radko 2003 for details).”