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Article: Decay of Fourier modes of solutions to the dissipative surface quasi-geostrophic equations on a finite domain

TitleDecay of Fourier modes of solutions to the dissipative surface quasi-geostrophic equations on a finite domain
Authors
Issue Date2012
Citation
Chaos, Solitons and Fractals, 2012, v. 45, n. 9-10, p. 1192-1200 How to Cite?
AbstractWe consider the two dimensional dissipative surface quasi-geostrophic equation on the unit square with mixed boundary conditions. Under some suitable assumptions on the initial stream function, we obtain existence and uniqueness of solutions in the form of a fast converging trigonometric series. We prove that the Fourier coefficients of solutions have a non-uniform decay: in one direction the decay is exponential and along the other direction it is only power like. We establish global wellposedness for arbitrary large initial data. © 2012 Elsevier Ltd. All rights reserved.
Persistent Identifierhttp://hdl.handle.net/10722/326900
ISSN
2023 Impact Factor: 5.3
2023 SCImago Journal Rankings: 1.349
ISI Accession Number ID

 

DC FieldValueLanguage
dc.contributor.authorChernov, Nikolai-
dc.contributor.authorLi, Dong-
dc.date.accessioned2023-03-31T05:27:21Z-
dc.date.available2023-03-31T05:27:21Z-
dc.date.issued2012-
dc.identifier.citationChaos, Solitons and Fractals, 2012, v. 45, n. 9-10, p. 1192-1200-
dc.identifier.issn0960-0779-
dc.identifier.urihttp://hdl.handle.net/10722/326900-
dc.description.abstractWe consider the two dimensional dissipative surface quasi-geostrophic equation on the unit square with mixed boundary conditions. Under some suitable assumptions on the initial stream function, we obtain existence and uniqueness of solutions in the form of a fast converging trigonometric series. We prove that the Fourier coefficients of solutions have a non-uniform decay: in one direction the decay is exponential and along the other direction it is only power like. We establish global wellposedness for arbitrary large initial data. © 2012 Elsevier Ltd. All rights reserved.-
dc.languageeng-
dc.relation.ispartofChaos, Solitons and Fractals-
dc.titleDecay of Fourier modes of solutions to the dissipative surface quasi-geostrophic equations on a finite domain-
dc.typeArticle-
dc.description.naturelink_to_subscribed_fulltext-
dc.identifier.doi10.1016/j.chaos.2012.06.002-
dc.identifier.scopuseid_2-s2.0-84864105655-
dc.identifier.volume45-
dc.identifier.issue9-10-
dc.identifier.spage1192-
dc.identifier.epage1200-
dc.identifier.isiWOS:000309315800014-

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