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A modified quasigeostrophic formulation for weakly nonlinear barotropic flow with large-amplitude depth variations

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Kiss, Andrew

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When the β effect is weak, rapidly rotating weakly nonlinear barotropic flow is subject to the "strong" Taylor-Proudman theorem, which severely restricts the horizontal divergence. This constraint is independent of the boundary conditions, and applies ev

dc.contributor.authorKiss, Andrew
dc.date.accessioned2015-12-13T23:23:01Z
dc.date.available2015-12-13T23:23:01Z
dc.identifier.issn1463-5003
dc.identifier.urihttp://hdl.handle.net/1885/91714
dc.description.abstractWhen the β effect is weak, rapidly rotating weakly nonlinear barotropic flow is subject to the "strong" Taylor-Proudman theorem, which severely restricts the horizontal divergence. This constraint is independent of the boundary conditions, and applies ev
dc.publisherElsevier
dc.sourceOcean Modelling
dc.subjectKeywords: barotropic motion; Ekman pumping; modeling; quasi-geostrophic flow; wind-driven circulation Barotropic flow; Laboratory modelling; Large-amplitude topography; Quasigeostrophic theory; Wind-driven circulation
dc.titleA modified quasigeostrophic formulation for weakly nonlinear barotropic flow with large-amplitude depth variations
dc.typeJournal article
local.description.notesImported from ARIES
local.description.refereedYes
local.identifier.citationvolume5
dc.date.issued2003
local.identifier.absfor040503 - Physical Oceanography
local.identifier.ariespublicationMigratedxPub22561
local.type.statusPublished Version
local.contributor.affiliationKiss, Andrew, College of Physical and Mathematical Sciences, ANU
local.bibliographicCitation.startpage171
local.bibliographicCitation.lastpage191
local.identifier.doi10.1016/S1463-5003(02)00038-0
dc.date.updated2015-12-12T09:13:40Z
local.identifier.scopusID2-s2.0-0037064633
CollectionsANU Research Publications

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