Persistence in a Simple Model for the Earth's Atmosphere Temperature Fluctuations

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dc.creatorBerrones, Arturo
dc.date2005-06-13
dc.date2005-08-30
dc.date.accessioned2026-07-07T05:55:07Z
dc.date.available2026-07-07T05:55:07Z
dc.descriptionThe effect caused by the presence of a number of distinct time scales in a simple stochastic model for the Earth's atmosphere temperature fluctuations is studied. The model is described by a dissipative dynamics consisting of a set of coupled stochastic evolution equations. The system shows features that resemble recent observations. In contrast to other approaches, like autoregressive models, the fluctuations of the atmosphere's temperature depend on parameters with clear physical meaning. A reduced version of the model is constructed and its temporal autocovariance function is explicitly written.
dc.description14 pages, 7 figures, final version
dc.identifierhttps://arxiv.org/abs/physics/0506116
dc.identifierhttp://arxiv.org/abs/physics/0506116
dc.identifierFluctuation and Noise Letters, Vol. 5, No. 3 (2005) L365 -- L374
dc.identifier.urihttp://salesiana.dossiersoluciones.com/handle/123456789/87191
dc.subjectAtmospheric and Oceanic Physics
dc.subjectOther Condensed Matter
dc.subjectData Analysis, Statistics and Probability
dc.titlePersistence in a Simple Model for the Earth's Atmosphere Temperature Fluctuations
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