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

• Published in: Geophysical research letters Vol. 40; no. 23; pp. 6171 - 6175
• Main Authors: Olascoaga, M. J., Beron-Vera, F. J., Haller, G., Triñanes, J., Iskandarani, M., Coelho, E. F., Haus, B. K., Huntley, H. S., Jacobs, G., Kirwan Jr, A. D., Lipphardt Jr, B. L., Özgökmen, T. M., H. M. Reniers, A. J., Valle-Levinson, A.
• Format: Journal Article
• Language: English
• Published: Washington Blackwell Publishing Ltd 16.12.2013; John Wiley & Sons, Inc
• Subjects: Altimeters; Altimetry; Approximation; Attraction; Coherence; Constraints; Deep water; Drift; Drifters; geodesic LCS; GLAD; Gulf of Mexico; LCS cores; Mesoscale circulation; Mesoscale phenomena; Meteorology; Oil slicks; Transport; Mexico; ASW, Mexico Gulf
• ISSN: 0094-8276; 1944-8007
• DOI: 10.1002/2013GL058624

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 Points Altimetric LCS constrain drifter motion Altimetric LCS form centerpieces of drifter distributions Altimetric LCS cores predate shape changes in drifter distributions