2012
DOI: 10.1088/0951-7715/26/1/1
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Abundance of attracting, repelling and elliptic periodic orbits in two-dimensional reversible maps

Abstract: Abstract. We study dynamics and bifurcations of two-dimensional reversible maps having non-transversal heteroclinic cycles containing symmetric saddle periodic points. We consider one-parameter families of reversible maps unfolding generally the initial heteroclinic tangency and prove that there are infinitely sequences (cascades) of bifurcations of birth of asymptotically stable and unstable as well as elliptic periodic orbits.

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Cited by 46 publications
(78 citation statements)
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References 33 publications
(88 reference statements)
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“…Chaos in dissipative systems is quite different and is associated with strange attractors. Our goal in this paper is to attract attention to one more type of chaos, the third one, which was called "mixed dynamics" in [1,2]. This type of behavior is characterized by inseparability of attractors, repellers, and conservative elements in the phase space [3].…”
Section: Introductionmentioning
confidence: 99%
“…Chaos in dissipative systems is quite different and is associated with strange attractors. Our goal in this paper is to attract attention to one more type of chaos, the third one, which was called "mixed dynamics" in [1,2]. This type of behavior is characterized by inseparability of attractors, repellers, and conservative elements in the phase space [3].…”
Section: Introductionmentioning
confidence: 99%
“…In this section we describe two stochastic lattice models, the simplest tropical climate model developed in [15,30,33] and the stochastic skeleton model for the MJO developed and applied in [34,35,41,42]. They both consist of an ODE system U t , which describes the dry dynamics based on continuum thermal-dynamical PDEs, and a stochastic jump process Á t , which describes the intermittent tropical variability.…”
Section: Stochastic Lattice Models For the Tropicsmentioning
confidence: 99%
“…In [15,30,33], the simplest tropical climate model is derived to capture the impact of tropical moisture variability. Here we discuss a simplified setup of flows above the equator, which follows a PDE:…”
Section: The Simplest Tropical Climate Model Deterministic Modelmentioning
confidence: 99%
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