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dc.contributor.authorDritschel, David Gerard
dc.contributor.authorViudez, A
dc.identifier.citationDritschel , D G & Viudez , A 2007 , ' The persistence of balance in geophysical flows ' , Journal of Fluid Mechanics , vol. 570 , pp. 365-383 .
dc.identifier.otherPURE: 329627
dc.identifier.otherPURE UUID: 81a9f3bb-be43-4d87-8289-c0ea0b2273a2
dc.identifier.otherWOS: 000243671300015
dc.identifier.otherScopus: 33845966765
dc.identifier.otherORCID: /0000-0001-6489-3395/work/64697751
dc.descriptionThis paper introduces a novel, powerful way to understand the why geophysical flows are largely under the control of a single scalar field, the potential vorticity, a materially conserved dynamical tracer in the absence of viscous and diabatic effects.en
dc.description.abstractRotating stably stratified geophysical flows can exhibit a near 'balanced' evolution controlled by the conservative advection of a single scalar quantity, the potential vorticity (PV). This occurs frequently in the Earth's atmosphere and oceans where motions tend to be weak compared with the background planetary rotation and where stratification greatly inhibits vertical motion. Under these circumstances, both high-frequency acoustic waves and lower-frequency inertia-gravity waves (IGWs) contribute little to the flow evolution compared with the even-lower-frequency advection of PV. Moreover, this 'slow' PV-controlled balanced evolution appears unable to excite these higher-frequency waves in any significant way-i.e. balance persists. The present work pushes the limits of balance by systematically exploring the evolution of a range of highly nonlinear flows in which motions are comparable with the background rotation. These flows do not possess a frequency separation between PV advection and IGWs. Nonetheless, the flows exhibit a remarkable persistence of balance. Even when flows are not initialized to minimize the amount of IGWs initially present, and indeed even when flows are deliberately seeded with significant IGW amplitudes, the flow evolution-over many inertial periods (days)-remains strongly controlled by PV advection.
dc.relation.ispartofJournal of Fluid Mechanicsen
dc.rights(c)2007 Cambridge University Pressen
dc.subjectPotential vorticity inversionen
dc.subjectGravity-wave generationen
dc.subjectQA Mathematicsen
dc.titleThe persistence of balance in geophysical flowsen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews. Applied Mathematicsen
dc.description.statusPeer revieweden

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