2009
DOI: 10.1016/j.physd.2009.05.003
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Capturing deviation from ergodicity at different scales

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Cited by 23 publications
(23 citation statements)
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“…Other options include the combined function g • b being the instantaneous eigenvector field of the variational equation [41], or a set of indicator functions over spatial boxes in order to define trajectory's "correlation dimension" or "ergodicity defect" [64,50]. Averages of the form (4) are also relevant to determining dispersion statistics [65], which are expected to be different in different coherent regions of a fluid.…”
Section: Lcs Diagnostic Methodsmentioning
confidence: 99%
“…Other options include the combined function g • b being the instantaneous eigenvector field of the variational equation [41], or a set of indicator functions over spatial boxes in order to define trajectory's "correlation dimension" or "ergodicity defect" [64,50]. Averages of the form (4) are also relevant to determining dispersion statistics [65], which are expected to be different in different coherent regions of a fluid.…”
Section: Lcs Diagnostic Methodsmentioning
confidence: 99%
“…Our results confirm the importance of studying coherent structures in zones in addition to focusing on finding the location of the barriers. Applying the recent results of geodesic LCS theory [19] or using the probabilistic approach based on transfer operators [20] to improve the objectivity in domain partitions may bring further insights on the statistics we obtain here. Such studies will be reported elsewhere.…”
mentioning
confidence: 85%
“…The second complexity measure considered here is the ergodicity defect d that was recently introduced by Scott et al (2009). d measures the extent to which the dynamical system and the corresponding map falls short of being ergodic using the "time average equals space average" view of ergodicity (Petersen, 1983;Lasota and Mackey, 1994).…”
Section: Two Complexity Measures and The Relationship Between Themmentioning
confidence: 99%
“…d measures the extent to which the dynamical system and the corresponding map falls short of being ergodic using the "time average equals space average" view of ergodicity (Petersen, 1983;Lasota and Mackey, 1994). The ergodicity defect was originally introduced in the context of illustrative (mathematical) maps in Scott et al (2009) and the theory behind it is further developed in (Scott, 2010(Scott, , 2011b. Here we extend the notion of ergodicity defect to fluid particle trajectories in geophysical fluid flows.…”
Section: Two Complexity Measures and The Relationship Between Themmentioning
confidence: 99%