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dc.contributor.authorDritschel, David Gerard
dc.contributor.authorViúdez, Alvaro
dc.date.accessioned2010-11-29T16:35:12Z
dc.date.available2010-11-29T16:35:12Z
dc.date.issued2003-08-10
dc.identifier.citationDritschel , D G & Viúdez , A 2003 , ' A balanced approach to modelling rotating stably stratified geophysical flows ' , Journal of Fluid Mechanics , vol. 488 , pp. 123-150 . https://doi.org/10.1017/S0022112003004920en
dc.identifier.issn0022-1120
dc.identifier.otherPURE: 253248
dc.identifier.otherPURE UUID: 37b641f1-2764-4f7c-a2c4-a3c251b69f8e
dc.identifier.otherWOS: 000185258000004
dc.identifier.otherScopus: 0038804645
dc.identifier.otherORCID: /0000-0001-6489-3395/work/64697777
dc.identifier.urihttp://hdl.handle.net/10023/1493
dc.descriptionThis work was the first to show how one can rewrite the equations for a rotating stratified fluid in a way which makes potential vorticity conservation explicit. Potential vorticity is linked closely to balance, a state void of high-frequency gravity waves. The mathematical transformation reveals a deep underlying mathematical structure, including explicit conditions for inertial and static stability as well as a new double Monge-Ampere equation. This work forms the cornerstone of much subsequent research into the fundamental nature of rotating stratified fluids.en
dc.description.abstractWe describe a new approach to modelling three-dimensional rotating stratified flows under the Boussinesq approximation. This approach is based on the explicit conservation of potential vorticity, and exploits the underlying leading-order geostrophic and hydrostratic balances inherent in these equations in the limit of small Froude and Rossby numbers. These balances are not imposed, but instead are used to motivate the use of a pair of new variables expressing the departure from geostrophic and hydrostratic balance. These new variables are the ageostrophic horizontal vorticity components, i.e. the vorticity not directly associated with the displacement of isopycnal surfaces. The use of potential vorticity and ageostrophic horizontal vorticity, rather than the usual primitive variables of velocity and density, reveals a deep mathematical structure and appears to have advantages numerically. This change of variables results in a diagnostic equation, of Monge-Amp re type, for one component of a vector potential phi, and two Poisson equations for the other two components. The curl of phi gives the velocity field while the divergence of phi is proportional to the displacement of isopycnal surfaces. This diagnostic equation makes transparent the conditions for both static and inertial stability, and may change form from (spatially) elliptic to (spatially) hyperbolic even when the flow is statically and inertially stable. A numerical method based on these new variables is developed and used to examine the instability of a horizontal elliptical shear zone (modelling a jet streak). The basic-state flow is in exact geostrophic and hydrostratic balance. Given a small perturbation however, the shear zone destabilizes by rolling up into a street of vortices and radiating inertia-gravity waves.
dc.format.extent28
dc.language.isoeng
dc.relation.ispartofJournal of Fluid Mechanicsen
dc.rights(c)2003 Cambridge University Pressen
dc.subjectPotential-vorticityen
dc.subject2-Dimensional Flowsen
dc.subjectGravity-wavesen
dc.subjectTurbulenceen
dc.subjectDynamicsen
dc.subjectSurgeryen
dc.subjectQA Mathematicsen
dc.subject.lccQAen
dc.titleA balanced approach to modelling rotating stably stratified geophysical flowsen
dc.typeJournal articleen
dc.description.versionPublisher PDFen
dc.contributor.institutionUniversity of St Andrews.Applied Mathematicsen
dc.identifier.doihttps://doi.org/10.1017/S0022112003004920
dc.description.statusPeer revieweden
dc.identifier.urlhttp://www.scopus.com/inward/record.url?scp=0038804645&partnerID=8YFLogxKen
dc.identifier.urlhttp://dx.doi.org/DOI 10.1017/S0022112003004920en


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