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

被引:91
作者
Olascoaga, M. J. [1 ]
Beron-Vera, F. J. [1 ]
Haller, G. [2 ]
Trinanes, J. [3 ]
Iskandarani, M. [1 ]
Coelho, E. F. [4 ]
Haus, B. K. [1 ]
Huntley, H. S. [5 ]
Jacobs, G. [6 ]
Kirwan, A. D., Jr. [5 ]
Lipphardt, B. L., Jr. [5 ]
Oezgoekmen, T. M. [1 ]
Reniers, A. J. H. M. [1 ]
Valle-Levinson, A. [7 ]
机构
[1] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA
[2] Swiss Fed Inst Technol, Inst Mech Syst, Zurich, Switzerland
[3] Univ Santiago de Compostela, Inst Invest Tecnolox, Santiago, Spain
[4] Univ New Orleans, Dept Phys, New Orleans, LA 70148 USA
[5] Univ Delaware, Sch Marine Sci & Policy, Newark, DE USA
[6] Stennis Space Ctr, Naval Res Lab, Stennis Space Ctr, MS USA
[7] Univ S Florida, Dept Civil & Coastal Engn, Gainesville, FL USA
基金
美国国家科学基金会;
关键词
geodesic LCS; LCS cores; altimetry; Gulf of Mexico; drifters; GLAD; TRANSPORT;
D O I
10.1002/2013GL058624
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
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 1week 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.
引用
收藏
页码:6171 / 6175
页数:5
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