A note on boundary-layer friction in baroclinic cyclones

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dc.creatorBoutle, I. A.
dc.creatorBeare, R. J.
dc.creatorBelcher, S. E.
dc.creatorPlant, R. S.
dc.date2008-01-30
dc.date.accessioned2026-07-07T08:57:17Z
dc.date.available2026-07-07T08:57:17Z
dc.descriptionThe interaction between extratropical cyclones and the underlying boundary layer has been a topic of recent discussion in papers by Adamson et. al. (2006) and Beare (2007). Their results emphasise different mechanisms through which the boundary layer dynamics may modify the growth of a baroclinic cyclone. By using different sea-surface temperature distributions and comparing the low-level winds, the differences are exposed and both of the proposed mechanisms appear to be acting within a single simulation.
dc.description5 pages, 3 figures
dc.identifierhttps://arxiv.org/abs/0801.4648
dc.identifierhttp://arxiv.org/abs/0801.4648
dc.identifierQuarterly Journal of the Royal Meteorological Society, 133, 2137-2141 (2007)
dc.identifierdoi:10.1002/qj.179
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/146906
dc.subjectAtmospheric and Oceanic Physics
dc.subjectFluid Dynamics
dc.titleA note on boundary-layer friction in baroclinic cyclones
dc.typetext

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