Linear waves and baroclinic instability in an inhomogeneous-density layered primitive-equation ocean model

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dc.creatorBeron-Vera, F. J.
dc.creatorOlascoaga, M. J.
dc.creatorZavala-Garay, J.
dc.date2004-01-16
dc.date2004-06-11
dc.date.accessioned2026-07-07T05:50:57Z
dc.date.available2026-07-07T05:50:57Z
dc.descriptionWe consider a multilayer generalization of Ripa's inhomogeneous-density single-layer primitive-equation model. In addition to vary arbitrarily in horizontal position and time, the horizontal velocity and buoyancy fields are allowed to vary linearly with depth within each layer of the model. Preliminary results on linear waves and baroclinic instability suggest that a configuration involving a few layers may set the basis for a quite accurate and numerically efficient ocean model.
dc.descriptionTo appear in ICTAM04 Abstract Book and CD-ROM Proceedings, ISBN 83-89687-01-1, IPPT PAN, Warsaw
dc.identifierhttps://arxiv.org/abs/physics/0401078
dc.identifierhttp://arxiv.org/abs/physics/0401078
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/85875
dc.subjectAtmospheric and Oceanic Physics
dc.titleLinear waves and baroclinic instability in an inhomogeneous-density layered primitive-equation ocean model
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