1 2D Continuous wavelet transform
1 2D Continuous wavelet transform
1 2D Continuous wavelet transform
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<strong>2D</strong>cwttools.tex Last compiled: Monday 22 nd January, 2007 15:33Signals where I(l, x) = 1 have energy distributed evenly in space. Regions of signalswhere the intermittency factor is much greater than 1 correspond to intermittent features.(presumably these intermittent features will correspond to the coherent structures!)1.3.3 Local Reynolds numberFor a signal that corresponds to a turbulent flow we can construct the Reynolds numberRe as the non-dimensional ratio of the nonlinear advection terms to the linear viscousterms in the Navier-Stokes equations. This gives the level of nonlinearity of the flowand is a measure of the intensity of turbulence (i.e. Re ≫ 1 is generally turbulent,though depending upon the specifics flow, and is indicative of the range of scales ofmotion excited). A global Reynolds number, based upon characteristics of the flow, canbe estimated asRe = UL(28)νwhere U is a characteristic velocity scale (i.e the RMS turbulent velocity), L a characteristiclength scale, and ν the kinematic viscosity of the flow. We can construct theequivalent from the <strong>wavelet</strong> coefficients. A space-scale Reynolds number (Farge et al1990)ṽ(l, x)lRe(l, x) = (29)νwhere ṽ(l, x) is the characteristic RMS velocity that can be calculated by summingover the CWT of the various components of the velocity. i.e. in 3Dṽ(l, x) = [(3C ψ ) −13∑|ṽ n (l, x)| 2 ] −1/2 (30)n=1One can recover a local (in scale) Reynolds number by integrating over space∫Re(l) = Re(l, x)d n x (31)R n...global flow intermittency1.3.4 Local Rossby numbersHere I propose a measure of the local Rossby number for a rotating turbulent flow. TheRossby number Ro is a non-dimensional parameter based upon the ratio of the nonlinearterms to the Coriolis term in the Navier-Stokes equations with rotation. There are twoglobal Rossby numbers that one can construct. One is based upon the advection termRo =U(32)2ΩLwhere U is a characteristic velocity scale, 2Ω is the background vorticity (the rotationof the system), and L is a characteristic length scale of the flow. Another Rossby numbercan be constructed from the nonlinear term containing the time derivative of the velocity.9