To the theory of underwater ice evolution, or nonlinear dynamics of ``false bottoms

DOI10.1016/j.ijheatmasstransfer.2007.11.061zbMath1154.80363OpenAlexW2087353621MaRDI QIDQ955545

I. G. Nizovtseva, Dmitri V. Alexandrov

Publication date: 20 November 2008

Published in: International Journal of Heat and Mass Transfer (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1016/j.ijheatmasstransfer.2007.11.061

zbMATH Keywords

sea iceheat fluxesmushy layerfalse bottommelt pond

Mathematics Subject Classification ID

Stefan problems, phase changes, etc. (80A22) Multiphase and multicomponent flows (76T99)

Related Items (8)

Thermo-solutal and kinetic modes of stable dendritic growth with different symmetries of crystalline anisotropy in the presence of convection ⋮ Nonlinear dynamics of mushy layers induced by external stochastic fluctuations ⋮ Analytical solutions of mushy layer equations describing directional solidification in the presence of nucleation ⋮ A complete analytical solution of the Fokker–Planck and balance equations for nucleation and growth of crystals ⋮ Mathematical modeling of dendrite growth in an Al–Ge alloy with convective flow ⋮ Влияние ложного дна на нелинейную динамику процесса замерзания воды;An influence of the false bottom on the nonlinear dynamics of the water freezing process ⋮ Solidification of a ternary melt from a cooled boundary, or nonlinear dynamics of mushy layers ⋮ The effect of density changes on crystallization with a mushy layer

Cites Work

• A THERMODYNAMICALLY CONSISTENT MODEL OF A MUSHY ZONE
• Heat and mass transfer between a rough wall and turbulent fluid flow at high Reynolds and Péclet numbers
• Heat transfer across rough surfaces

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