It has been shown that forced Lorenz models generally maintain their two-lobe structure, just giving rise to changes in the occurrence of their regimes. Here, using the richness of a unified formalism for Kolmogorov-Lorenz systems, we show that introducing oscillating forcings can lead to the birth of new regimes and to a four-lobe attractor. Analogies within a climate dynamics framework are mentioned. © Author(s) 2012.
CITATION STYLE
Pelino, V., Maimone, F., & Pasini, A. (2012). Oscillating forcings and new regimes in the Lorenz system: A four-lobe attractor. Nonlinear Processes in Geophysics, 19(3), 315–322. https://doi.org/10.5194/npg-19-315-2012
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