Characterization of coherent structures in three-dimensional turbulent flows using the finite-size Lyapunov exponent

被引:26
作者
Bettencourt, Joao H. [1 ]
Lopez, Cristobal [1 ]
Hernandez-Garcia, Emilio [1 ]
机构
[1] IFISC CSIC UIB, Inst Fis Interdisciplinar & Sistemas Complejos, E-07122 Palma De Mallorca, Spain
关键词
LAGRANGIAN TRANSPORT; CHANNEL FLOW; BARRIERS; IDENTIFICATION; DEFINITION; STATISTICS; DISPERSION; MANIFOLDS; VELOCITY; EDDY;
D O I
10.1088/1751-8113/46/25/254022
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
In this paper, we use the finite-size Lyapunov exponent (FSLE) to characterize Lagrangian coherent structures in three-dimensional (3D) turbulent flows. Lagrangian coherent structures act as the organizers of transport in fluid flows and are crucial to understand their stirring and mixing properties. Generalized maxima (ridges) of the FSLE fields are used to locate these coherent structures. 3D FSLE fields are calculated in two phenomenologically distinct turbulent flows: a wall-bounded flow (channel flow) and a regional oceanic flow obtained by the numerical solution of the primitive equations where two-dimensional (2D) turbulence dominates. In the channel flow, autocorrelations of the FSLE field show that the structure is substantially different from the near wall to the mid-channel region and relates well to the more widely studied Eulerian coherent structure of the turbulent channel flow. The ridges of the FSLE field have complex shapes due to the 3D character of the turbulent fluctuations. In the oceanic flow, strong horizontal stirring is present and the flow regime is similar to that of 2D turbulence where the domain is populated by coherent eddies that interact strongly. This in turn results in the presence of high FSLE lines throughout the domain leading to strong non-local mixing. The ridges of the FSLE field are quasi-vertical surfaces, indicating that the horizontal dynamics dominates the flow. Indeed, due to rotation and stratification, vertical motions in the ocean are much less intense than horizontal ones. This suppression is absent in the channel flow, as the 3D character of the FSLE ridges shows.
引用
收藏
页数:20
相关论文
共 57 条
[1]   Hairpin vortex organization in wall turbulence [J].
Adrian, Ronald J. .
PHYSICS OF FLUIDS, 2007, 19 (04)
[2]  
[Anonymous], 2012, TECHNICAL REPORT
[3]   Dispersion of passive tracers in closed basins: Beyond the diffusion coefficient [J].
Artale, V ;
Boffetta, G ;
Celani, A ;
Cencini, M ;
Vulpiani, A .
PHYSICS OF FLUIDS, 1997, 9 (11) :3162-3171
[4]   Predictability in the large: An extension of the concept of Lyapunov exponent [J].
Aurell, E ;
Boffetta, G ;
Crisanti, A ;
Paladin, G ;
Vulpiani, A .
JOURNAL OF PHYSICS A-MATHEMATICAL AND GENERAL, 1997, 30 (01) :1-26
[5]  
Bakun A., 1996, PATTERNS OCEAN OCEAN
[6]   Invariant-tori-like Lagrangian coherent structures in geophysical flows [J].
Beron-Vera, Francisco J. ;
Olascoaga, Maria J. ;
Brown, Michael G. ;
Kocak, Huseyin ;
Rypina, Irina I. .
CHAOS, 2010, 20 (01)
[7]   Oceanic three-dimensional Lagrangian coherent structures: A study of a mesoscale eddy in the Benguela upwelling region [J].
Bettencourt, Joao H. ;
Lopez, Cristobal ;
Hernandez-Garcia, Emilio .
OCEAN MODELLING, 2012, 51 :73-83
[8]   Detecting barriers to transport: a review of different techniques [J].
Boffetta, G ;
Lacorata, G ;
Radaelli, G ;
Vulpiani, A .
PHYSICA D-NONLINEAR PHENOMENA, 2001, 159 (1-2) :58-70
[9]   Nonasymptotic properties of transport and mixing [J].
Boffetta, G ;
Celani, A ;
Cencini, M ;
Lacorata, G ;
Vulpiani, A .
CHAOS, 2000, 10 (01) :50-60
[10]   Lagrangian structure of flows in the Chesapeake Bay: challenges and perspectives on the analysis of estuarine flows [J].
Branicki, M. ;
Malek-Madani, R. .
NONLINEAR PROCESSES IN GEOPHYSICS, 2010, 17 (02) :149-168