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dc.contributor.authorFlierl, Glenn R
dc.contributor.authorMorrison, Philip J
dc.contributor.authorVilasur Swaminathan, Rohith
dc.date.accessioned2021-10-27T20:09:16Z
dc.date.available2021-10-27T20:09:16Z
dc.date.issued2019
dc.identifier.urihttps://hdl.handle.net/1721.1/134804
dc.description.abstract© 2019 MDPI AG. All rights reserved. We explore the theory of isolated vortices in strongly sheared, deep zonal flows and the stability of these banded jets, as occur in Jupiter's atmosphere This is done using the standard 2-layer quasigeostrophic model with the lower layer depth becoming infinite; however, this model differs from the usual layer model because the lower layer is not assumed to be motionless but has a steady configuration of alternating zonal flows. Steady state vortices are obtained by a simulated annealing computational method as generalized to fluid problems with constraints and also used in the used in the context of magnetohydrodynamics. Various cases of vortices with a constant potential vorticity anomaly atop zonal winds and the stability of the underlying winds are considered using a mix of computational and analytical techniques.
dc.language.isoen
dc.publisherMDPI AG
dc.relation.isversionof10.3390/fluids4020104
dc.rightsCreative Commons Attribution 4.0 International license
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.sourceMDPI
dc.titleJovian Vortices and Jets
dc.typeArticle
dc.contributor.departmentMassachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
dc.relation.journalFluids
dc.eprint.versionFinal published version
dc.type.urihttp://purl.org/eprint/type/JournalArticle
eprint.statushttp://purl.org/eprint/status/PeerReviewed
dc.date.updated2019-10-18T11:04:40Z
dspace.orderedauthorsFlierl, GR; Morrison, PJ; Vilasur Swaminathan, R
dspace.date.submission2019-10-18T11:04:43Z
mit.journal.volume4
mit.journal.issue2
mit.metadata.statusAuthority Work and Publication Information Needed


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