Cascade phenomenology

Intermittency quantification

The intermittency can be quantified using the definition of the flatness. To this end, we use a high pass filtered signal defined as :

\begin{eqnarray*} x(t) = \int_{\Re^3} d\omega e^{i \omega t} \hat{x_{\omega}} \\ x_{\Omega}^{>}(t) = \int_{|\omega| > \Omega} d\omega e^{i \omega t} \hat{x_{\omega}} \end{eqnarray*}

We can say that the variable is intermittent at small scales if the flatness grows without bound with the filter frequency .

(red) : Probability density function of temperature increment, (blue) : Gaussian distribution
\begin{equation*} F= \frac{S_4(l)}{\langle S_2(l) \rangle^2} = \frac{\langle (\delta T(l) )^4\rangle}{\langle (\delta T(l))^2 \rangle^2} \end{equation*}

The flatness is useful measure of intermittency for signals having a bursty aspect. Instead of flatness it is possible to use other nondimensional ratios, such as the moment of order 6 divided by the cube of the second moment order.

PreviousPreviousNextNext
HomepageHomepagePrintPrintCreated with Scenari (new window)