On Reynolds Averaging of Turbulence Time Series
We show that validity of Reynolds averaging for estimating the (ensemble) mean of a turbulence time series requires that the series values be both stationary and uncorrelated. In strict statistical terminology, these two conditions are jointly designated as independent identically distributed (i.i.d...
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Veröffentlicht in: | Boundary-layer meteorology 2008-08, Vol.128 (2), p.303-311 |
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Format: | Artikel |
Sprache: | eng |
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Zusammenfassung: | We show that validity of Reynolds averaging for estimating the (ensemble) mean of a turbulence time series requires that the series values be both stationary and uncorrelated. In strict statistical terminology, these two conditions are jointly designated as independent identically distributed (i.i.d.). Moreover, we show that when the series values are correlated, knowledge of the correlation between the values is needed to obtain a reliable estimate of the mean. Last, we contend that a viable averaging algorithm must be Reynolds number (Re) dependent, requiring one version for low Re (Gaussian) turbulence and another for high Re (non-Gaussian) turbulence. Alternatively the median (as opposed to the mean) is recommended as a measure of the central tendency of the turbulence probability density function. |
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ISSN: | 0006-8314 1573-1472 |
DOI: | 10.1007/s10546-008-9288-8 |