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2013•Geophysical Research LettersOpen access

Drifter motion in the Gulf of Mexico constrained by altimetric Lagrangian coherent structures

M. J. Olascoaga, F. J. Beron‐Vera, George Haller, Joaquín Triñanes, Mohamed Iskandarani, Emanuel Coelho, Brian K. Haus, Helga S. Huntley, Gregg Jacobs, A. D. Kirwan, B. L. Lipphardt, Tamay M. Özgökmen, Ad Reniers, Arnoldo Valle‐Levinson

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Abstract

Application of recent geometric tools for Lagrangian coherent structures (LCS) shows that material attraction in geostrophic velocities derived from altimetry data imposed an important constraint to the motion of drifters from the Grand Lagrangian Deployment (GLAD) in the Gulf of Mexico. This material attraction is largely transparent to traditional Eulerian analysis. Attracting LCS acted as approximate centerpieces for mesoscale patterns formed by the drifters. Persistently attracting LCS cores emerged 1 week before the development of a filament resembling the “tiger tail” of the Deepwater Horizon oil slick, thereby anticipating its formation. Our results suggest that the mesoscale circulation plays a significant role in shaping near‐surface transport in the Gulf of Mexico.

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What this paper is about

Application of recent geometric tools for Lagrangian coherent structures (LCS) shows that material attraction in geostrophic velocities derived from altimetry data imposed an important constraint to the motion of drifters from the Grand Lagrangian Deployment (GLAD) in the Gulf of Mexico. This material attraction is largely transparent to traditional Eulerian analysis. Attracting LCS acted as approximate centerpieces for mesoscale patterns formed by the drifters. Persistently attracting LCS cores emerged 1 week before the development of a filament resembling the “tiger tail” of the Deepwater Horizon oil slick, thereby anticipating its formation. Our results suggest that the mesoscale circulation plays a significant role in shaping near‐surface transport in the Gulf of Mexico.

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Available abstract

Application of recent geometric tools for Lagrangian coherent structures (LCS) shows that material attraction in geostrophic velocities derived from altimetry data imposed an important constraint to the motion of drifters from the Grand Lagrangian Deployment (GLAD) in the Gulf of Mexico. This material attraction is largely transparent to traditional Eulerian analysis. Attracting LCS acted as approximate centerpieces for mesoscale patterns formed by the drifters. Persistently attracting LCS cores emerged 1 week before the development of a filament resembling the “tiger tail” of the Deepwater Horizon oil slick, thereby anticipating its formation. Our results suggest that the mesoscale circulation plays a significant role in shaping near‐surface transport in the Gulf of Mexico.

Key concepts: Drifter, Mesoscale meteorology, Geostrophic wind, Lagrangian, Geology, Constraint (computer-aided design), Eulerian path, Altimeter

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