New toppling dynamics for the self-organized critical rainfall model

dc.creatorAndrade, Roberto Fernandes Silva
dc.creatorPinho, Suani Tavares Rubim de
dc.creatorFraga, Sandro C
dc.creatorTanajura, Ana P. M.
dc.creatorAndrade, Roberto Fernandes Silva
dc.creatorPinho, Suani Tavares Rubim de
dc.creatorFraga, Sandro C
dc.creatorTanajura, Ana P. M.
dc.date.accessioned2022-10-07T15:54:26Z
dc.date.available2022-10-07T15:54:26Z
dc.date.issued2002-11
dc.identifier0378-4371
dc.identifierhttp://www.repositorio.ufba.br/ri/handle/ri/7443
dc.identifierv. 314, n. 1-4
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/4006224
dc.description.abstractIn this paper we introduce two new dynamical features of rainfall phenomena into the self-organized critical rainfall model. The new dynamics lead to the constrained random and the complete toppling versions, both of which lose the abelian character of the original model. The constrained random rainfall model is also a self-organized criticality model, but it belongs to another universal class. The complete toppling rainfall model presents two different regimes related to small and large avalanches, respectively.
dc.languageen
dc.sourcehttp://dx.doi.org/10.1016/S0378-4371(02)01071-3
dc.subjectRainfall model
dc.subjectWater avalanche
dc.subjectSelf-organized criticality
dc.titleNew toppling dynamics for the self-organized critical rainfall model
dc.typeArtigo de Periódico


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