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Nonhydrostatic wave generation at strained fronts

dc.contributor.authorShakespeare, Callum J.en
dc.date.accessioned2026-01-01T12:42:03Z
dc.date.available2026-01-01T12:42:03Z
dc.date.issued2016en
dc.description.abstractA simple analytical model is developed to describe wave generation during frontogenesis forced by a horizontal strain field. In contrast to previous models, neither geostrophic nor hydrostatic balance is assumed. The generated waves are trapped in the strain field and form steady bands of enhanced vertical flow on either side of the surface front on scales from 1 to 100 km. The predictions of the analytical model are confirmed by comparison with fully nonlinear numerical simulations.en
dc.description.statusPeer-revieweden
dc.format.extent14en
dc.identifier.issn0022-4928en
dc.identifier.scopus84977547063en
dc.identifier.urihttps://hdl.handle.net/1885/733800381
dc.language.isoenen
dc.rightsPublisher Copyright: © 2016 American Meteorological Society.en
dc.sourceJournal of the Atmospheric Sciencesen
dc.titleNonhydrostatic wave generation at strained frontsen
dc.typeJournal articleen
dspace.entity.typePublicationen
local.bibliographicCitation.lastpage2850en
local.bibliographicCitation.startpage2837en
local.contributor.affiliationShakespeare, Callum J.; University of Cambridgeen
local.identifier.citationvolume73en
local.identifier.doi10.1175/JAS-D-14-0294.1en
local.identifier.pure6bb44ca1-63e1-4279-a041-c94d99a4a82aen
local.identifier.urlhttps://www.scopus.com/pages/publications/84977547063en
local.type.statusPublisheden

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