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On hadley flow in a porous layer with vertical heterogeneity - MaRDI portal

On hadley flow in a porous layer with vertical heterogeneity (Q2863406)

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Please use this page instead for the normal view: On hadley flow in a porous layer with vertical heterogeneity

scientific article; zbMATH DE number 6231837

Language	Label	Description	Also known as
English	On hadley flow in a porous layer with vertical heterogeneity	scientific article; zbMATH DE number 6231837

Statements

scholarly article

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Journal of Fluid Mechanics

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publication date

21 November 2013

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zbMATH Keywords

Bénard convection

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buoyancy-driven instability

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convection in porous media

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MaRDI profile type

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full work available at URL

https://doi.org/10.1017/jfm.2012.365

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The effects of combined horizontal and vertical heterogeneity on the onset of convection in a porous medium with horizontal throughflow

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Convection induced by inclined thermal and solutal gradients in a shallow horizontal layer of a porous medium

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Convection in Porous Media

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Convection in a porous medium with inclined temperature gradient and vertical throughflow

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Convection in a porous medium with inclined temperature gradient

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The method of weighted residuals and variational principles. With application in fluid mechanics, heat and mass transfer

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Absolute/convective instability dichotomy at the onset of convection in a porous layer with either horizontal or vertical solutal and inclined thermal gradients, and horizontal throughflow

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Soret-driven thermosolutal convection induced by inclined thermal and solutal gradients in a shallow horizontal layer of a porous medium

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Convection induced by inclined thermal and solutal gradients, with horizontal mass flow, in a shallow horizontal layer of a porous medium

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Numerical simulations of supercritical Hadley circulation, within a porous layer, induced by inclined temperature gradients

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Nonlinear stability of convection in a porous medium with inclined temperature gradient

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Three-dimensional absolute and convective instabilities at the onset of convection in a porous medium with inclined temperature gradient and vertical throughflow

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Local thermal non-equilibrium effects in the Darcy-Bénard instability with isoflux boundary conditions

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Convection in a porous medium with horizontal and vertical temperature gradients

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Stability and Wave Motion in Porous Media

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The effects of combined horizontal and vertical heterogeneity on the onset of convection in a porous medium

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On hadley flow in a porous layer with vertical heterogeneity (English)

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Identifiers

zbMATH Open document ID

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Mathematics Subject Classification ID

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zbMATH DE Number

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10.1017/JFM.2012.365

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Sitelinks

Mathematics(1 entry)

mardi Publication:2863406

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