Single-eddy contributions to streamwise velocity variance in turbulent pipe flow. Part 1. The single-eddy intensity function
Jinyul Hwang
Abstract
Townsend's attached-eddy hypothesis explains the asymptotic statistics of wall turbulence through a superposition of self-similar attached eddies. At a given observation location, active portions contribute to momentum transfer, whereas inactive portions retain only wall-parallel fluctuations. Since this distinction depends on the observation height relative to the eddy height yl, we extract single-eddy intensity functions from DNS of turbulent pipe flow at Reτ930--6000. Spectral linear stochastic estimation and differencing isolate wall-coherent contributions at prescribed yl, yielding the streamwise and wall-normal intensity functions Iuu and Ivv. When expressed in y*=y/yl, both collapse across yl and share a peak at ya*, close to the von K'arm'an constant. Near ya*, both components remain significant, whereas for y* ya*, Ivv diminishes while Iuu remains finite, identifying active and inactive portions. Over the self-similar range, both peak intensities scale as yl-1, and Iuu retains this scaling in both portions. Integrating the active portion yields an approximately constant contribution, while the inactive portion recovers the classical near-wall logarithmic variation. An outer logarithmic tendency with a slope close to the Townsend--Perry constant arises from integrating active contributions up to their outer cutoff. At the near-wall peak of uu+, the scaling steepens to Iuu yl-(1+β) with β1/4, yielding a finite asymptote with a Reτ-1/4 defect. The additional exponent is attributed to viscous attenuation of inactive footprints associated with a yl-dependent dissipative scale. Wall-coherent motions also produce a broad outer shoulder, while a localized wall-incoherent residual may contribute to a secondary peak.
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