Abstract
Buoyant, finite-size, or inertial particle motion is fundamentally unlike neutrally buoyant, infinitesimally small, or Lagrangian particle motion. The de-jure fluid mechanics framework for the description of inertial particle dynamics is provided by the Maxey–Riley equation. Derived from first principles—a result of over a century of research since the pioneering work by Sir George Stokes—the Maxey–Riley equation is a Newton-type law with several forces including (mainly) flow, added mass, shear-induced lift, and drag forces. In this paper, we present an overview of recent efforts to transfer the Maxey–Riley framework to oceanography. These involved: (1) including the Coriolis force, which was found to explain behavior of submerged floats near mesoscale eddies; (2) accounting for the combined effects of ocean current and wind drag on inertial particles floating at the air–sea interface, which helped understand the formation of great garbage patches and the role of anticyclonic eddies as plastic debris traps; and (3) incorporating elastic forces, which are needed to simulate the drift of pelagic Sargassum. Insight into the nonlinear dynamics of inertial particles in every case was possible to be achieved by investigating long-time asymptotic behavior in the various Maxey–Riley equation forms, which represent singular perturbation problems involving slow and fast variables.
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Notes
If \(t\in [t_1,t_2]\subset {\mathbb {R}}\), as in applications involving measurements, \(M_0\) will not form, strictly speaking, a manifold since it will necessary include corners. Yet \(M_0\!\setminus \!\partial M_0\) represents a well-defined manifold.
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Acknowledgements
The constructive criticism of two anonymous reviewers led to improvements to this paper. I want to acknowledge the influence exerted by Gustavo Goñi on my career for triggering my interest in nonlinear dynamics while I was an undergraduate student of oceanography, and by Paco Villaverde, Roberto Delellis, the late Pedro Ripa, and Mike Brown for conveying subsequent sustain to it. Doron Nof’s presentation at the 2016 Ocean Science Meeting [63] provided inspiration for the work that led to the derivation of the BOM equation in collaboration with Maria Olascoaga and Philippe Miron, with whom I am in debt for the benefit of many discussions on inertial ocean dynamics. I thank George Haller and Chris Jones for clarifying comments on geometric singular perturbation theory. Remark 14 is due to Mohammad Farazmand. Remark 27 was brought to my attention by Tamás Tél. This work builds on lectures I imparted at the CISM–ECCOMAS International Summer School on “Coherent Structures in Unsteady Flows: Mathematical and Computational Methods,” Udine, Italy, June 3–7, 2019, organized by George Haller. Support for the work overviewed here was provided by CONACyT–SENER (Mexico) grant 201441, the Gulf of Mexico Research Initiative, and the University of Miami’s Cooperative Institute for Marine and Atmospheric Science.
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Beron-Vera, F.J. Nonlinear dynamics of inertial particles in the ocean: from drifters and floats to marine debris and Sargassum. Nonlinear Dyn 103, 1–26 (2021). https://doi.org/10.1007/s11071-020-06053-z
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DOI: https://doi.org/10.1007/s11071-020-06053-z