J. Szilagyi et al., THE LOCAL EFFECT OF INTERMITTENCY ON THE INERTIAL SUBRANGE ENERGY-SPECTRUM OF THE ATMOSPHERIC SURFACE-LAYER, Boundary - layer meteorology, 79(1-2), 1996, pp. 35-50
Orthonormal wavelet expansions are applied to atmospheric surface laye
r velocity measurements. The effect of intermittent events on the ener
gy spectrum of the inertial subrange is investigated through analysis
of wavelet coefficients. The local nature of the orthonormal wavelet t
ransform in physical space makes it possible to identify a relationshi
p between the inertial subrange slope of the local wavelet spectrum an
d a simple indicator (i.e. the local variance of the signal) of local
intermittency buildup. The slope of the local wavelet energy spectrum
in the inertial subrange is shown to be sensitive to the presence of i
ntermittent events. During well developed intermittent events (coheren
t structures), the slope of the energy spectrum is somewhat steeper th
an -5/3, while in less active regions the slope is found to be flatter
than -5/3. When the slopes of local wavelet spectra are ensemble aver
aged, a slope of -5/3 is recovered for the inertial subrange.