Near-surface transport pathways in the north Atlantic Ocean : looking for throughput from the subtropical to the subpolar gyre

• Published in: Journal of Physical Oceanography
• Main Authors: Rypina, Irina I., Pratt, Lawrence J., Lozier, M. Susan
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Meteorological Society 2011
• Subjects: Atlantic Ocean; Transport; Gyres; Lagrangian circulation/transport; Tracers; Currents; Meridional overturning circulation; North Atlantic
• Online Access: https://hdl.handle.net/1912/4647

Author Posting. © American Meteorological Society, 2011. This article is posted here by permission of American Meteorological Society for personal use, not for redistribution. The definitive version was published in Journal of Physical Oceanography 41 (2011): 911–925, doi:10.1175/2011JPO4498.1. Motivated by discrepancies between Eulerian transport estimates and the behavior of Lagrangian surface drifters, near-surface transport pathways and processes in the North Atlantic are studied using a combination of data, altimetric surface heights, statistical analysis of trajectories, and dynamical systems techniques. Particular attention is paid to the issue of the subtropical-to-subpolar intergyre fluid exchange. The velocity field used in this study is composed of a steady drifter-derived background flow, upon which a time-dependent altimeter-based perturbation is superimposed. This analysis suggests that most of the fluid entering the subpolar gyre from the subtropical gyre within two years comes from a narrow region lying inshore of the Gulf Stream core, whereas fluid on the offshore side of the Gulf Stream is largely prevented from doing so by the Gulf Stream core, which acts as a strong transport barrier, in agreement with past studies. The transport barrier near the Gulf Stream core is robust and persistent from 1992 until 2008. The qualitative behavior is found to be largely independent of the Ekman drift. This work was supported by the National Science Foundation Grants CMG-82469600 and CMG-82579600 and by the Office of Naval Research Grant ONR-13108700.