Transport induced by mean-eddy interaction: I. Theory, and relation to Lagrangian lobe dynamics

被引:5
作者
Ide, Kayo [1 ,2 ]
Wiggins, Stephen [3 ]
机构
[1] Univ Maryland, Inst Phys Sci & Technol, Ctr Sci Computat & Math Modeling, Dept Atmospher & Ocean Sci, College Pk, MD 20742 USA
[2] Univ Maryland, Earth Syst Sci Interdisciplinary Ctr, College Pk, MD 20742 USA
[3] Univ Bristol, Sch Math, Bristol BS8 1TW, Avon, England
关键词
Eulerian transport; Lagrangian transport; Mean-eddy interaction; Dynamical systems approach; Wind-driven ocean circulation; OCEANIC FLOWS; WIND-DRIVEN; DATA SETS; SYSTEMS; CHAOS;
D O I
10.1016/j.cnsns.2014.06.007
中图分类号
O29 [应用数学];
学科分类号
070104 ;
摘要
In this paper we develop a method for the estimation of Transport Induced by the Mean-Eddy interaction (TIME) in two-dimensional unsteady flows. The method is based on the dynamical systems approach to fluid transport and can be viewed as a hybrid combination of Lagrangian and Eulerian methods. The (Eulerian) boundaries across which we consider (Lagrangian) transport are kinematically defined by appropriately chosen streamlines of the mean flow. By evaluating the impact of the mean-eddy interaction on transport, the TIME method can be used as a diagnostic tool for transport processes that occur during a specified time interval along a specified boundary segment. We introduce two types of TIME functions: one that quantifies the accumulation of flow properties and another that measures the displacement of the transport geometry. The spatial geometry of transport is described by the so-called pseudo-lobes, and temporal evolution of transport by their dynamics. In the case where the TIME functions are evaluated along a separatrix, the pseudo-lobes have a relationship to the lobes of Lagrangian transport theory. In fact, one of the TIME functions is identical to the Melnikov function that is used to measure the distance, at leading order in a small parameter, between the two invariant manifolds that define the Lagrangian lobes. We contrast the similarities and differences between the TIME and Lagrangian lobe dynamics in detail. An application of the TIME method is carried out for inter-gyre transport in the wind-driven oceanic circulation model and a comparison with the Lagrangian transport theory is made. (C) 2014 Elsevier B.V. All rights reserved.
引用
收藏
页码:516 / 535
页数:20
相关论文
共 25 条
[1]  
[Anonymous], 2005, Nonlinear Physical Oceanography: A Dynamical Systems Approach to the Large-Scale Ocean Circulation and El Nino
[2]  
Arnold V. I., 2013, Mathematical methods of classical mechanics, V60
[3]   Intergyre transport in a wind-driven, quasigeostrophic double gyre: An application of lobe dynamics [J].
Coulliette, C ;
Wiggins, S .
NONLINEAR PROCESSES IN GEOPHYSICS, 2000, 7 (1-2) :59-85
[4]  
Greenspan B. D., 1983, NONLINEAR DYNAMICS T, P172
[5]  
Guckenheimer J., 2013, Nonlinear Oscillations, Dynamical Systems, and Bifurcations of Vector Fields, V42
[6]   AVERAGING AND CHAOTIC MOTIONS IN FORCED-OSCILLATIONS [J].
HOLMES, PJ .
SIAM JOURNAL ON APPLIED MATHEMATICS, 1980, 38 (01) :65-80
[7]  
Hovmoller E, 1949, TELL, V1, P62, DOI [DOI 10.3402/TELLUSA.V1I2.8498, 10.1111/j.2153-3490.1949.tb01260.x10.3402/tellusa.v1i2.8498, DOI 10.1111/J.2153-3490.1949.TB01260.X10.3402/TELLUSA.V1I2.8498, 10.1111/j.2153-3490.1949.tb01260.x, DOI 10.1111/J.2153-3490.1949.TB01260.X]
[8]   Distinguished hyperbolic trajectories in time-dependent fluid flows: analytical and computational approach for velocity fields defined as data sets [J].
Ide, K ;
Small, D ;
Wiggins, S .
NONLINEAR PROCESSES IN GEOPHYSICS, 2002, 9 (3-4) :237-263
[9]  
Ide K, 2014, COMMUN NONLINEAR SCI
[10]   Geometric structures, lobe dynamics, and Lagrangian transport in flows with aperiodic time-dependence, with applications to Rossby wave flow [J].
Malhotra, N ;
Wiggins, S .
JOURNAL OF NONLINEAR SCIENCE, 1998, 8 (04) :401-456