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dc.contributor.authorWurtele, M. G.
dc.date.accessioned2017-06-09T14:12:29Z
dc.date.available2017-06-09T14:12:29Z
dc.date.copyright1960/12/01
dc.date.issued1960
dc.identifier.issn0095-9634
dc.identifier.otherams-14681.pdf
dc.identifier.urihttp://onlinelibrary.yabesh.ir/handle/yetl/4150269
dc.description.abstractThe Lagrangian ?parcel method? of stability analysis is systematically presented and rendered rigorous in its application to nondivergent flow on a plane with constant Coriolis parameter. The method is applied in detail to two familiar models. (1) Zonal geostrophic current with linear horizontal shear. Here the parcel method is valid only for uniform initial disturbance (?infinite wave-length?), in which case the usual stability criterion applies, ??g <f. Another particular solution has been given by Lord Kelvin. (2) Anticyclonic vortex with concentric circular contours. Here, the parcel-method stability criterion is ??g < f/2 (as suggested by the balance equation) and is valid for any initial disturbance with balanced velocity field. So far, no non-symmetric solution to the balance equation for this pressure field has been discovered.
dc.publisherAmerican Meteorological Society
dc.titleLAGRANGIAN DYNAMICS AND THE PARCEL METHOD IN ATMOSPHERIC MODELS
dc.typeJournal Paper
dc.journal.volume17
dc.journal.issue6
dc.journal.titleJournal of Meteorology
dc.identifier.doi10.1175/1520-0469(1960)017<0661:LDATPM>2.0.CO;2
dc.journal.fristpage661
dc.journal.lastpage669
dc.treeJournal of Meteorology:;1960:;volume( 017 ):;issue: 006
dc.contenttypeFulltext


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