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dc.contributor.authorISHIOKA, Keiichien
dc.contributor.alternative石岡, 圭一ja
dc.date.accessioned2015-02-12T07:11:05Z-
dc.date.available2015-02-12T07:11:05Z-
dc.date.issued2013-
dc.identifier.issn0026-1165-
dc.identifier.urihttp://hdl.handle.net/2433/193663-
dc.description.abstractA previous study proposed two methods for calculating the upper bound of the growth of disturbances from barotropic instability of a zonal flow in a two-dimensional incompressible fluid on a rotating sphere. The study conjectured that these two upper bounds are equivalent. One method was based on the conservation of the domain-averaged pseudomomentum density, and the other solved a minimization problem under the constraints of the conservations of all Casimir invariants and the total absolute angular momentum. In this study, this conjecture is verified, i.e., a proof is presented for their equivalence by developing an annealing-like procedure to reach the absolute vorticity profile that corresponds to the upper bound. The procedure also provides a more efficient method to calculate the upper bound.en
dc.format.mimetypeapplication/pdf-
dc.language.isoeng-
dc.publisherMeteorological Society of Japanen
dc.publisher.alternative日本気象学会ja
dc.rights© 2013 by Meteorological Society of Japanen
dc.subjectbarotropic instabilityen
dc.subjectnonlinear stabilityen
dc.subjectpseudomomentumen
dc.subjectupper bound for disturbance growthen
dc.subjectoptimization problemen
dc.titleA Proof for the Equivalence of Two Upper Bounds for the Growth of Disturbances from Barotropic Instabilityen
dc.typejournal article-
dc.type.niitypeJournal Article-
dc.identifier.ncidAA00702524-
dc.identifier.jtitleJournal of the Meteorological Society of Japan. Ser. IIen
dc.identifier.volume91-
dc.identifier.issue6-
dc.identifier.spage843-
dc.identifier.epage850-
dc.relation.doi10.2151/jmsj.2013-609-
dc.textversionpublisher-
dcterms.accessRightsopen access-
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