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Titlebook: Nonlinear Dynamics in Geosciences; Anastasios A. Tsonis,James B. Elsner Conference proceedings 2007 Springer-Verlag New York 2007 Atmosphe

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25 Years of Nonlinearity in Oceanography from the Lagrangian Perspective,hyperbolic and elliptic regions in flow fields along with finite time and scale Lyapunov exponents and particle dispersion statistics. Here we identify elliptic and hyperbolic regions to study the life cycle of a large anticyclonic eddy in the Gulf of Mexico. Hyperbolic regions develop simultaneousl
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Self-Scaling of the Statistical Properties of a Minimal Model of the Atmospheric Circulation,n and barotropic convergence processes. The model undergoes baroclinic forcing towards a given latitudinal temperature profile controlled by the forced equator-to-pole temperature difference T.. As T. increases, a transition takes place from a stationary regime - Hadley equilibrium - to a periodic r
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Hindcast AGCM Experiments on the Predictability of Stratospheric Sudden Warming,ugawa, Sakai, and Hirooka (2005) is confirmed by conducting a series of hindcast experiments using an atmospheric general circulation model (MRI/JMA-GCM). Similar precursory circulation anomaly in the troposphere for the occurrence of the SSW is also obtained through a regression analysis on the GCM
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Analysis of Nonlinear Biophysical Time Series in Aquatic Environments: Scaling Properties and Empircing coming from seasonal or annual meteorological and climatic cycles. In this work we are interested in the characterization of these properties, using different statistical tools, borrowed from the field of turbulence, or of nonlinear time series analysis. We first present the analysis of a long
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Scale, Scaling and Multifractals in Geophysics: Twenty Years on,tifractal processes, b) the self-organized critical (SOC) generation of extremes via multifractal phase transitions c) the generalization from isotropic scale invariance (self-similar fractals, multifractals) to (anisotropic) generalized scale invariance. We argue that these innovations are generall
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