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Please use this identifier to cite or link to this item: https://physrep.ff.bg.ac.rs/handle/123456789/1122
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dc.contributor.authorGavrilov, Milivoj B.en
dc.contributor.authorTošić, Ivanaen
dc.date.accessioned2022-07-12T18:19:36Z-
dc.date.available2022-07-12T18:19:36Z-
dc.date.issued1999-01-01en
dc.identifier.issn0027-0644en
dc.identifier.urihttps://physrep.ff.bg.ac.rs/handle/123456789/1122-
dc.description.abstractDispersion characteristics of the shallow water quasigeostrophic modes are discussed for the rectangular grids. It is shown that the propagation of the quasigeostrophic modes is affected by the orientation of the semistaggered grids. Also, it is found that the A and E Arakawa grids produce frequencies of the Rossby waves with the wrong sign, that is, positive instead of negative. The B grid gives better propagation of the quasigeostrophic modes than any of the Arakawa grids. Finally, it appears that the B grid has certain advantages over the Z grid.en
dc.relation.ispartofMonthly Weather Reviewen
dc.titleDispersion characteristics of discrete quasigeostrophic modesen
dc.typeArticleen
dc.identifier.doi10.1175/1520-0493(1999)127<2197:DCODQM>2.0.CO;2en
dc.identifier.scopus2-s2.0-0343415738en
dc.identifier.urlhttps://api.elsevier.com/content/abstract/scopus_id/0343415738en
dc.relation.issue9en
dc.relation.volume127en
dc.relation.firstpage2197en
dc.relation.lastpage2203en
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.grantfulltextnone-
item.cerifentitytypePublications-
item.openairetypeArticle-
item.fulltextNo Fulltext-
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