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Convection driven by differential heating at a horizontal boundary

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dc.contributor.authorMullarney, J
dc.contributor.authorGriffiths, Ross
dc.contributor.authorHughes, Graham
dc.date.accessioned2015-12-13T23:09:59Z
dc.date.issued2004
dc.date.updated2016-02-24T09:47:55Z
dc.description.abstractWe report laboratory and numerical experiments with the convective circulation that develops in a long channel driven by heating and cooling through opposite halves of the horizontal base. The problem is similar to that posed by Stommel (Proc. Natl Acad.
dc.identifier.issn0022-1120
dc.identifier.urihttp://hdl.handle.net/1885/87260
dc.publisherCambridge University Press
dc.sourceJournal of Fluid Mechanics
dc.subjectKeywords: Boundary conditions; Density (specific gravity); Heat flux; Numerical methods; Problem solving; Thermal effects; Turbulence; Velocity measurement; Convective circulation; Differential heating; Rayleigh numbers; Thermocline depth; Heat convection; boundary
dc.titleConvection driven by differential heating at a horizontal boundary
dc.typeJournal article
local.bibliographicCitation.lastpage209
local.bibliographicCitation.startpage181
local.contributor.affiliationMullarney, J, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationGriffiths, Ross, College of Physical and Mathematical Sciences, ANU
local.contributor.affiliationHughes, Graham, College of Physical and Mathematical Sciences, ANU
local.contributor.authoruidMullarney, J, u4024764
local.contributor.authoruidGriffiths, Ross, u8300081
local.contributor.authoruidHughes, Graham, u8912812
local.description.embargo2037-12-31
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.absfor040403 - Geophysical Fluid Dynamics
local.identifier.ariespublicationMigratedxPub16473
local.identifier.citationvolume516
local.identifier.doi10.1017/S0022112004000485
local.identifier.scopusID2-s2.0-6044266064
local.type.statusPublished Version

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