Large-scale effects on the decay of rotating helical and non-helical turbulence

Turbulent mixing in geophysics is often affected by the presence of rotation, which renders the flow anisotropic at large scales. Helicity (correlation between the velocity and its curl) has relevance for atmospheric and astrophysical flows and can also affect mixing. In this paper, decaying three-d...

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Autor principal: Teitelbaum, T.
Otros Autores: Mininni, P.D
Formato: Acta de conferencia Capítulo de libro
Lenguaje:Inglés
Publicado: 2010
Acceso en línea:Registro en Scopus
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100 1 |a Teitelbaum, T. 
245 1 0 |a Large-scale effects on the decay of rotating helical and non-helical turbulence 
260 |c 2010 
270 1 0 |m Teitelbaum, T.; Departamento de Fí Sica, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires and CONICET, 1428 Buenos Aires, Argentina; email: teitelbaum@df.uba.ar 
506 |2 openaire  |e Política editorial 
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504 |a Majda, A.J., Embid, P.F., Averaging over fast gravity waves for geophysics flows with unbalanced initial data (1998) Theor. Comput. Fluid Dyn., 11 (3-4), pp. 155-169 
504 |a Seiwert, J., Morize, C., Moisy, F., On the decrease of intermittency in decaying rotating turbulence (2008) Phys. Fluids, 20 (7), p. 071702 
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504 |a Yang, X., Domaradzki, J.A., Large eddy simulations of decaying rotating turbulence (2004) Phys. Fluids, 16 (11), pp. 4088-4104 
504 |a Teitelbaum, T., Mininni, P.D., Effect of helicity and rotation on the free decay of turbulent flows (2009) Phys. Rev. Lett., 103 (1), p. 014501 
504 |a Morinishi, Y., Nakabayashi, K., Ren, S., Effects of helicity and system rotation on decaying homogeneous turbulence (2001) JSME Int. J. Ser., 44 (3), pp. 410-418 
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504 |a Mininni, P.D., Pouquet, A., Helicity cascades in rotating turbulence (2009) Phys. Rev., 79 (2), p. 026304A4 - International Centre for Theoretical Physics (ICTP); National Science Foundation (NSF); Air Force Office of Scientific Research (AFOSR); Eur. Off. Aerosp. Res. Dev. (EOARD) AFOSR; Department of Energy (DOE) 
520 3 |a Turbulent mixing in geophysics is often affected by the presence of rotation, which renders the flow anisotropic at large scales. Helicity (correlation between the velocity and its curl) has relevance for atmospheric and astrophysical flows and can also affect mixing. In this paper, decaying three-dimensional (3D) turbulence is studied via direct numerical simulations (DNS) for an isotropic non-rotating flow and for rotating flows with and without helicity. We analyze the cases of moderate Rossby number and large Reynolds number, focusing on the behavior of the energy spectrum at large scales and studying its effect on the time evolution of the energy and integral scales for E(k)∼k4 initial conditions. In the non-rotating case, we observe the classical energy decay rate t-10/7 and a growth of the integral length proportional to t2/7 in agreement with the prediction obtained assuming conservation of the Loitsyanski integral. In the presence of rotation we observe a decoupling in the decay of the modes perpendicular to the rotation axis from the remaining 3D modes. These slow modes show a behavior similar to that found in two-dimensional (2D) turbulence, whereas the 3D modes decay as in the isotropic case. We phenomenologically explain the decay considering integral conserved quantities that depend on the large-scale anisotropic spectrum. The decoupling of modes is also observed for a flow with a net amount of helicity. In this case, the 3D modes decay as an isotropic fluid with a constant, constrained integral length and the 2D modes decay as a constrained rotating fluid with maximum helicity. © 2010 The Royal Swedish Academy of Sciences.  |l eng 
593 |a Departamento de Fí Sica, Facultad de Ciencias Exactas y Naturales, Universidad de Buenos Aires and CONICET, 1428 Buenos Aires, Argentina 
593 |a NCAR, PO Box 3000, Boulder, CO 80307-3000, United States 
690 1 0 |a ANISOTROPIC SPECTRA 
690 1 0 |a ASTROPHYSICAL FLOWS 
690 1 0 |a CONSERVED QUANTITY 
690 1 0 |a ENERGY DECAY RATES 
690 1 0 |a ENERGY SPECTRA 
690 1 0 |a HELICAL TURBULENCE 
690 1 0 |a HELICITIES 
690 1 0 |a INITIAL CONDITIONS 
690 1 0 |a ISOTROPIC FLUIDS 
690 1 0 |a LARGE-SCALE EFFECTS 
690 1 0 |a ROSSBY NUMBERS 
690 1 0 |a ROTATING FLOW 
690 1 0 |a ROTATING FLUIDS 
690 1 0 |a ROTATION AXIS 
690 1 0 |a SLOW MODE 
690 1 0 |a THREE-DIMENSIONAL (3D) 
690 1 0 |a TIME EVOLUTIONS 
690 1 0 |a TURBULENT MIXING 
690 1 0 |a TWO-DIMENSIONAL (2D) TURBULENCE 
690 1 0 |a ANISOTROPY 
690 1 0 |a MIXING 
690 1 0 |a REYNOLDS NUMBER 
690 1 0 |a ROTATION 
690 1 0 |a ROTATIONAL FLOW 
690 1 0 |a SPECTROSCOPY 
690 1 0 |a THREE DIMENSIONAL 
690 1 0 |a TURBULENCE 
690 1 0 |a TURBULENT FLOW 
690 1 0 |a DECAY (ORGANIC) 
700 1 |a Mininni, P.D. 
711 2 |c Trieste  |d 27 July 2009 through 7 August 2009  |g Código de la conferencia: 83718 
773 0 |d 2010  |g v. T142  |p Phys Scr T  |n Physica Scripta T  |x 02811847  |t 2nd International Conference and Advanced School on Turbulent Mixing and Beyond, TMB-2009 
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