2008/04/13 by Paolo Luchini, Luchini, Paolo
Engineering · Environmental Science · Physics and Astronomy · #Fluid Dynamics and Turbulent Flows #Phase Equilibria and Thermodynamics #Plant Water Relations and Carbon Dynamics #physics.flu-dyn
paper · pdf · doi:10.48550/arxiv.0804.2067
arxiv created 2008/04/13 · arxiv updated 2009/12/01
The commonly accepted description of transition to turbulence in shear flows requires the presence of an external source of disturbances that get amplified by an essentially linear mechanism up to the point where breakdown to turbulence occurs. Microscopic fluctuations are shown here to provide just the right amount of initial disturbances to match the predictions of linear stability theory.