12.07.2015 Views

1 2D Continuous wavelet transform

1 2D Continuous wavelet transform

1 2D Continuous wavelet transform

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

<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

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!