Objective Detection of Oceanic Eddies and the Agulhas Leakage
By Francisco J. Beron-Vera, Yan Wang, Maria J. Olascoaga, G. Goñi, G. Haller. 2013
155 citations recorded by the source corpus.
Subfields: Global and Planetary Change, Oceanography
View Paper: https://www.semanticscholar.org/paper/681e0dbfd19f9f3ccd47c3f3b68a22fdb8354bdd
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Global and Planetary Change
- G. Haller
- E. van Sebille
- L. Zanna
- P. Berloff
- S. Griffies
- Francisco J. Beron-Vera
- Claire B Paris-Limouzy
- N. Gruber
In Oceanography
- G. Haller
- Claire B Paris-Limouzy
- L. Zanna
- P. Berloff
- S. Griffies
- Francisco J. Beron-Vera
- N. Gruber
- Robert Marsh
Citations in the corpus
- Southern Ocean eddy phenomenology (2015, background): “The contribution of this effect to the (monopole) SST pattern versus the contribution of waters stemming from the eddies nursery is difficult to quantify even in models, even though a few approaches to assess the permeability of an eddy exist [Williams et al., 2012; Beron-Vera et al., 2013].”
- Defining coherent vortices objectively from the vorticity (2015, methodology): “Recent two-dimensional Lagrangian studies of the Agulhas leakage have used geodesic LCS theory to locate perfectly non-filamenting (black-hole-type) material eddies (Beron-Vera et al. 2013; Haller & Beron-Vera 2013).”
- Coherent Lagrangian vortices: the black holes of turbulence (2013, background): “As shown by Beron-Vera et al. (2013), eddy tracking from instantaneous altimetric Sea-Surface-Height (SSH) measurements (Chelton et al. 2011) would substantially overestimate the coherent part of this transport.”
- Lagrangian Coherent Structures (2015, methodology): “…data (Voth et al. 2002; Mathur et al. 2007; Raben et al. 2014a,b); coherent Lagrangian eddy transport in ocean models can readily be quantified (Beron-Vera et al. 2013); detailed Lagrangian now-casting for the ocean and atmosphere is within reach (Tang et al. 2011a,b; Shuckburgh 2012;…”
- Lagrangian ocean analysis: Fundamentals and practices (2018, methodology): “(25) We can relate the Fokker-Planck equation (24) to the Boussinesq form of the 566 tracer equation (16), so that(13) 567 bij = Kij ai = v † i + ∂jKij P = C.”
- Frontiers of chaotic advection (2014, methodology): “The resulting computational procedure is more involved than the detection of FTLE/FSLE ridges, but it addresses the issue of false positives, and was successfully applied by Beron-Vera et al. (2013) to the detection of Agulhas ring eddies in the Atlantic (Fig.”