Relation between kinematic boundaries, stirring, and barriers for the Antarctic polar vortex
By Binson Joseph, Bernard Legras. 2002
178 citations recorded by the source corpus.
Subfields: Astronomy and Astrophysics, Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/4e5ff32b2cc45e991e2d5a93171364f6660054e9
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Astronomy and Astrophysics
In Atmospheric Science
- E. García-Ladona
- E. Hernández‐García
- J. Isern‐Fontanet
- Jerrold E. Marsden
- Francois Lekien
- Shawn C. Shadden
- G. Haller
Citations in the corpus
- Definition and properties of Lagrangian coherent structures from finite-time Lyapunov exponents in two-dimensional aperiodic flows (2005, unknown): “The works of [20] [19] demonstrate the use of FSLE for locating LCSs in atmospheric data.”
- Frontiers of chaotic advection (2014, methodology): “Because this simplified computation, LCS were often approximated by ridges of Finite Time Lyapunov Exponent (FTLE) and Finite Size Lyapunov Exponent (FSLE) fields, which were assumed to exist near true LCS; see Haller and Sapsis (2011); Joseph and Legras (2002); Shadden et al. (2005).”
- Lagrangian Coherent Structures (2015, background): “…2000, Jones & Winkler 2002), finite-time Lyapunov exponents (FTLEs; see Section 4), finite-size Lyapunov exponents (FSLEs; see Aurell et al. 1997, Joseph & Legras 2002, d’Ovidio et al. 2004), effective diffusivity (Nakamura 1996, Haynes & Shuckburgh 2000, Shuckburgh & Haynes 2003), stretching in…”
- Lagrangian coherent structures in n-dimensional systems (2007, methodology): “Using FTLE is, however, not necessary and ridges can be computed from other measures of hyperbolicity, such as hyperbolicity time Haller 2000, 2001 , finite strain Jones and Winkler 2002 , or finite-size Lyapunov exponents FSLE Koh and Legras 2002 ; Joseph and Legras 2002 .”
- Comparison between Eulerian diagnostics and finite-size Lyapunov exponents computed from altimetry in the Algerian basin (2008, background): “…tion -either backward or forward in time- respectively as the unstable and stable manifolds205 of the hyperbolic points in the flow (Haller and Yuan, 2000; Boffetta et al., 2001; Haller,206 2001; Koh and Legras, 2002; Joseph and Legras, 2002; d’Ovidio et al., 2004; Mancho et al.,207 2006).”