Not much helicity is needed to drive large-scale dynamos

被引:8
|
作者
Graham, Jonathan Pietarila [1 ]
Blackman, Eric G. [2 ]
Mininni, Pablo D. [3 ,4 ,5 ]
Pouquet, Annick [3 ]
机构
[1] Los Alamos Natl Lab MS B258, Ctr Nonlinear Studies, Los Alamos, NM 87545 USA
[2] Univ Rochester, Dept Phys & Astron, Rochester, NY 14627 USA
[3] Natl Ctr Atmospher Res, Computat & Informat Syst Lab, Boulder, CO 80307 USA
[4] Univ Buenos Aires, Fac Ciencias Exactas & Nat, Dept Fis, RA-1428 Buenos Aires, DF, Argentina
[5] Consejo Nacl Invest Cient & Tecn, Inst Fis Buenos Aires IFIBA, RA-1428 Buenos Aires, DF, Argentina
来源
PHYSICAL REVIEW E | 2012年 / 85卷 / 06期
基金
美国国家科学基金会;
关键词
MAGNETIC-FIELD; SIMULATIONS; TURBULENCE;
D O I
10.1103/PhysRevE.85.066406
中图分类号
O35 [流体力学]; O53 [等离子体物理学];
学科分类号
070204 ; 080103 ; 080704 ;
摘要
Understanding the in situ amplification of large-scale magnetic fields in turbulent astrophysical rotators has been a core subject of dynamo theory. When turbulent velocities are helical, large-scale dynamos that substantially amplify fields on scales that exceed the turbulent forcing scale arise, but the minimum sufficient fractional kinetic helicity f(h,C) has not been previously well quantified. Using direct numerical simulations for a simple helical dynamo, we show that f(h,C) decreases as the ratio of forcing to large-scale wave numbers k(F)/k(min) increases. From the condition that a large-scale helical dynamo must overcome the back reaction from any nonhelical field on the large scales, we develop a theory that can explain the simulations. For k(F)/k(min) >= 8 we find f(h,C) less than or similar to 3%, implying that very small helicity fractions strongly influence magnetic spectra for even moderate-scale separation.
引用
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页数:5
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