Linear stability analysis of parallel shear flows for an inviscid generalized two-dimensional fluid system

被引:5
作者
Iwayama, T. [1 ]
Sueyoshi, M.
Watanabe, T. [2 ]
机构
[1] Kobe Univ, Grad Sch Sci, Dept Earth & Planetary Sci, Kobe, Hyogo 6578501, Japan
[2] Nagoya Inst Technol, Grad Sch Engn, Dept Sci & Engn Simulat, Showa Ku, Nagoya, Aichi 4668555, Japan
关键词
SCALING LAW; ENERGY; TURBULENCE; DYNAMICS; SPECTRA;
D O I
10.1088/1751-8113/46/6/065501
中图分类号
O4 [物理学];
学科分类号
0702 ;
摘要
The linear stability of parallel shear flows for an inviscid generalized two-dimensional (2D) fluid system, the so-called alpha turbulence system, is studied. This system is characterized by the relation q = -(-Delta)(alpha/2)psi between the advected scalar q and the stream function psi. Here, alpha is a real number not exceeding 3 and q is referred to as the generalized vorticity. In this study, a sufficient condition for linear stability of parallel shear flows is derived using the conservation of wave activity. A stability analysis is then performed for a sheet vortex that violates the stability condition. The instability of a sheet vortex in the 2D Euler system (alpha = 2) is referred to as a Kelvin-Helmholtz (KH) instability; such an instability for the generalized 2D fluid system is investigated for 0 < alpha < 3. The sheet vortex is unstable in the sense that a sinusoidal perturbation applied to it grows exponentially with time. The growth rate is finite and depends on the wavenumber of the perturbation as k(3-alpha) for 1 < alpha < 3, where k is the wavenumber of the perturbation. In contrast, for 0 < alpha <= 1, the growth rate is infinite. In other words, a transition of the growth rate of the perturbation occurs at alpha = 1. A physical model for KH instability in the generalized 2D fluid system, which can explain the transition of the growth rate of the perturbation at alpha = 1, is proposed.
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页数:21
相关论文
共 30 条
[1]  
Batchelor G.K., 1967, An introduction to fluid dynamics
[2]   A new proof on net upscale energy cascade in two-dimensional and quasi-geostrophic turbulence [J].
Gkioulekas, Eleftherios ;
Tung, Ka Kit .
JOURNAL OF FLUID MECHANICS, 2007, 576 (173-189) :173-189
[3]   SURFACE QUASI-GEOSTROPHIC DYNAMICS [J].
HELD, IM ;
PIERREHUMBERT, RT ;
GARNER, ST ;
SWANSON, KL .
JOURNAL OF FLUID MECHANICS, 1995, 282 :1-20
[4]   An 'ideal' form of decaying two-dimensional turbulence [J].
Iwayama, T ;
Shepherd, TG ;
Watanabe, T .
JOURNAL OF FLUID MECHANICS, 2002, 456 :183-198
[5]   Infrared dynamics of decaying two-dimensional turbulence governed by the Charney-Hasegawa-Mima equation [J].
Iwayama, T ;
Watanabe, T ;
Shepherd, TG .
JOURNAL OF THE PHYSICAL SOCIETY OF JAPAN, 2001, 70 (02) :376-386
[6]   Green's function for a generalized two-dimensional fluid [J].
Iwayama, Takahiro ;
Watanabe, Takeshi .
PHYSICAL REVIEW E, 2010, 82 (03)
[7]  
JUCKES M, 1994, J ATMOS SCI, V51, P2756, DOI 10.1175/1520-0469(1994)051<2756:QDOTT>2.0.CO
[8]  
2
[9]   Oceanic restratification forced by surface frontogenesis [J].
Lapeyre, Guillaume ;
Klein, Patrice ;
Hua, Bach Lien .
JOURNAL OF PHYSICAL OCEANOGRAPHY, 2006, 36 (08) :1577-1590
[10]   WEAKLY DECAYING TURBULENCE IN AN EQUIVALENT-BAROTROPIC FLUID [J].
LARICHEV, VD ;
MCWILLIAMS, JC .
PHYSICS OF FLUIDS A-FLUID DYNAMICS, 1991, 3 (05) :938-950