Estimating intermittency exponent in neutrally stratified atmospheric surface layer flows: A robust framework based on magnitude cumulant and surrogate analyses

Sukanta Basu, Efi Foufoula-Georgiou, Bruno Lashermes, Alain Arnéodo

Research output: Contribution to journalArticlepeer-review

32 Scopus citations

Abstract

This study proposes a novel framework based on magnitude cumulant and surrogate analyses to reliably detect the presence of intermittency and estimate the intermittency coefficient from short-length coarse-resolution turbulent time series. Intermittency coefficients estimated from a large number of neutrally stratified atmospheric surface layer turbulent series from various field campaigns are shown to remarkably concur with well-known laboratory experimental results. In addition, surrogate-based hypothesis testing significantly reduces the likelihood of detecting a spurious nonzero intermittency coefficient from nonintermittent series. The discriminatory power of the proposed framework is promising for addressing the unresolved question of how atmospheric stability affects the intermittency properties of boundary layer turbulence.

Original languageEnglish (US)
Article number115102
JournalPhysics of Fluids
Volume19
Issue number11
DOIs
StatePublished - Nov 2007

Bibliographical note

Funding Information:
We would like to thank Gary Kunkel and Ivan Marusic for providing us with the hot-wire measurements taken at the SLTEST facility, Utah. We are also grateful to all the researchers who painstakingly collected data during the Davis field campaigns. This work was partially funded by the National Science Foundation (ANT-0538453) and the Texas Advanced Research Program (003644-0003-2006) grants awarded to S.B. E.F.-G. acknowledges support by NASA, under its Global Precipitation Mission (GPM) program, and by NSF via the National Center for Earth-surface Dynamics (NCED) under agreement EAR-0120914.

Fingerprint

Dive into the research topics of 'Estimating intermittency exponent in neutrally stratified atmospheric surface layer flows: A robust framework based on magnitude cumulant and surrogate analyses'. Together they form a unique fingerprint.

Cite this