When are projections also embeddings?

We study an autonomous four-dimensional dynamical system used to model certain geophysical processes.This system generates a chaotic attractor that is strongly contracting, with four Lyapunov exponents $\lambda_i$ that satisfy $\lambda_1+ \lambda_2+\lambda_3<0$, so the Lyapunov dimension is $...

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Main Authors: Moroz, I, Letellier, C, Gilmore, R
Format: Journal article
Published: 2007
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author Moroz, I
Letellier, C
Gilmore, R
author_facet Moroz, I
Letellier, C
Gilmore, R
author_sort Moroz, I
collection OXFORD
description We study an autonomous four-dimensional dynamical system used to model certain geophysical processes.This system generates a chaotic attractor that is strongly contracting, with four Lyapunov exponents $\lambda_i$ that satisfy $\lambda_1+ \lambda_2+\lambda_3<0$, so the Lyapunov dimension is $D_L=2+|\lambda_3|/\lambda_1 < 3$ in the range of coupling parameter values studied. As a result, it should be possible to find three-dimensional spaces in which the attractors can be embedded so that topological analyses can be carried out to determine which stretching and squeezing mechanisms generate chaotic behavior. We study mappings into $R^3$ to determine which can be used as embeddings to reconstruct the dynamics. We find dramatically different behavior in the two simplest mappings: projections from $R^4$ to $R^3$. In one case the one-parameter family of attractors studied remains topologically unchanged for all coupling parameter values. In the other case, during an intermediate range of parameter values the projection undergoes self-intersections, while the embedded attractors at the two ends of this range are topologically mirror images of each other.
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spelling oxford-uuid:dd286265-1ebc-414e-8eeb-93fe02d186732022-03-27T09:23:13ZWhen are projections also embeddings?Journal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:dd286265-1ebc-414e-8eeb-93fe02d18673Mathematical Institute - ePrints2007Moroz, ILetellier, CGilmore, RWe study an autonomous four-dimensional dynamical system used to model certain geophysical processes.This system generates a chaotic attractor that is strongly contracting, with four Lyapunov exponents $\lambda_i$ that satisfy $\lambda_1+ \lambda_2+\lambda_3<0$, so the Lyapunov dimension is $D_L=2+|\lambda_3|/\lambda_1 < 3$ in the range of coupling parameter values studied. As a result, it should be possible to find three-dimensional spaces in which the attractors can be embedded so that topological analyses can be carried out to determine which stretching and squeezing mechanisms generate chaotic behavior. We study mappings into $R^3$ to determine which can be used as embeddings to reconstruct the dynamics. We find dramatically different behavior in the two simplest mappings: projections from $R^4$ to $R^3$. In one case the one-parameter family of attractors studied remains topologically unchanged for all coupling parameter values. In the other case, during an intermediate range of parameter values the projection undergoes self-intersections, while the embedded attractors at the two ends of this range are topologically mirror images of each other.
spellingShingle Moroz, I
Letellier, C
Gilmore, R
When are projections also embeddings?
title When are projections also embeddings?
title_full When are projections also embeddings?
title_fullStr When are projections also embeddings?
title_full_unstemmed When are projections also embeddings?
title_short When are projections also embeddings?
title_sort when are projections also embeddings
work_keys_str_mv AT morozi whenareprojectionsalsoembeddings
AT letellierc whenareprojectionsalsoembeddings
AT gilmorer whenareprojectionsalsoembeddings