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- W1980079897 abstract "As an idealization of convection near an ice boundary, flows in both salt-stratified and non-stratified liquids generated by a cooled slab of solid material are considered through direct numerical simulation. When the liquid far from the slab is homogeneous, significant convection occurs below the ice and apart from a small boundary layer, hardly no flow appears next to the ice. On the contrary, when the background liquid is stratified through a constant salt gradient, a layered flow appears next to the ice if the thickness of the slab is large enough. The latter flows are of double diffusive origin and have a significant effect on the transport of heat and salt near the ice." @default.
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- W1980079897 date "1998-07-01" @default.
- W1980079897 modified "2023-09-23" @default.
- W1980079897 title "Double diffusive layer formation near a cooled liquid-solid boundary" @default.
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- W1980079897 doi "https://doi.org/10.1016/s0017-9310(97)00355-4" @default.
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