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Sandstrom's experiments revisited

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Coman, Melissa; Griffiths, Ross; Hughes, Graham

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Sandström's (1908, 1916) pioneering experiments led to the conclusion, later referred to as Sandström's 'theorem', that differential heating and cooling cannot drive a sustained circulation when the source of heating is at or above the level of the cool

dc.contributor.authorComan, Melissa
dc.contributor.authorGriffiths, Ross
dc.contributor.authorHughes, Graham
dc.date.accessioned2015-12-10T22:29:34Z
dc.identifier.issn0022-2402
dc.identifier.urihttp://hdl.handle.net/1885/54967
dc.description.abstractSandström's (1908, 1916) pioneering experiments led to the conclusion, later referred to as Sandström's 'theorem', that differential heating and cooling cannot drive a sustained circulation when the source of heating is at or above the level of the cool
dc.publisherSears Foundation for Marine Research
dc.sourceJournal of Marine Research
dc.subjectKeywords: buoyancy; heat source; meridional circulation; overturn; sea surface temperature; thermal convection
dc.titleSandstrom's experiments revisited
dc.typeJournal article
local.description.notesImported from ARIES
local.identifier.citationvolume64
dc.date.issued2006
local.identifier.absfor040403 - Geophysical Fluid Dynamics
local.identifier.absfor040503 - Physical Oceanography
local.identifier.ariespublicationu4105084xPUB315
local.type.statusPublished Version
local.contributor.affiliationComan, Melissa, 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.description.embargo2037-12-31
local.bibliographicCitation.issue6
local.bibliographicCitation.startpage783
local.bibliographicCitation.lastpage796
local.identifier.doi10.1357/002224006779698413
dc.date.updated2015-12-09T09:57:11Z
local.identifier.scopusID2-s2.0-33847070312
CollectionsANU Research Publications

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