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蜿蜒射流中的混沌混合与输运。

Chaotic mixing and transport in a meandering jet flow.

作者信息

Prants S V, Budyansky M V, Uleysky M Yu, Zaslavsky G M

机构信息

V.I.Il'ichev Pacific Oceanological Institute of the Russian Academy of Sciences, 43 Baltiiskaya Ulitsa, 690041 Vladivostok, Russia.

出版信息

Chaos. 2006 Sep;16(3):033117. doi: 10.1063/1.2229263.

Abstract

Mixing and transport of passive particles are studied in a simple kinematic model of a meandering jet flow motivated by the problem of lateral mixing and transport in the Gulf Stream. We briefly discuss a model stream function, Hamiltonian advection equations, stationary points, and bifurcations. The phase portrait of the chosen model flow in the moving reference frame consists of a central eastward jet, chains of northern and southern circulations, and peripheral westward currents. Under a periodic perturbation of the meander's amplitude, the topology of the phase space is complicated by the presence of chaotic layers and chains of oscillatory and ballistic islands with sticky boundaries immersed into a stochastic sea. Typical chaotic trajectories of advected particles are shown to demonstrate a complicated behavior with long flights in both the directions of motion intermittent with trapping in the circulation cells being stuck to the boundaries of vortex cores and resonant islands. Transport is asymmetric in the sense that mixing between the circulations and the peripheral currents is, in general, different from mixing between the circulations and the jet. The transport properties are characterized by probability distribution functions (PDFs) of durations and lengths of flights. Both the PDFs exhibit at their tails power-law decay with different values of exponents.

摘要

在一个受墨西哥湾流横向混合与输运问题启发而建立的蜿蜒射流简单运动学模型中,研究了被动粒子的混合与输运。我们简要讨论了一个模型流函数、哈密顿平流方程、驻点和分岔。在移动参考系中所选模型流的相图由一个中心向东的射流、北部和南部环流链以及外围向西的水流组成。在对蜿蜒幅度进行周期性扰动的情况下,相空间的拓扑结构因混沌层以及振荡和弹道岛链的存在而变得复杂,这些岛链具有粘性边界,沉浸在一个随机海中。被平流粒子的典型混沌轨迹显示出一种复杂的行为,在运动的两个方向上都有长距离飞行,其间歇性地被困在环流单元中,被粘在涡核和共振岛的边界上。输运是不对称的,因为环流与外围水流之间的混合通常不同于环流与射流之间的混合。输运特性由飞行持续时间和长度的概率分布函数(PDF)来表征。这两个PDF在其尾部都呈现幂律衰减,但指数值不同。

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