Flux–gradient relationship, self‐correlation and intermittency in the stable boundary layer

The correlation between dimensionless shear ϕm and dimensionless height z/L, where L is the Obukhov length, for stable conditions is strongly influenced by self‐correlation for the present datasets. This effect is quite large for stronger stability but still significant for near‐neutral conditions....

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Published in:Quarterly journal of the Royal Meteorological Society 2004-07, Vol.130 (601), p.2087-2103
Main Authors: Klipp, Cheryl L., Mahrt, Larry
Format: Article
Language:English
Subjects:
CASES99
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Monin–Obukhov similarity
Nocturnal boundary layer
z‐less similarity
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description The correlation between dimensionless shear ϕm and dimensionless height z/L, where L is the Obukhov length, for stable conditions is strongly influenced by self‐correlation for the present datasets. This effect is quite large for stronger stability but still significant for near‐neutral conditions. A conditional analysis of nocturnal stable boundary‐layer data, where ‘non‐turbulent’ parts of the record are removed, reduces the impact of nonstationarity and therefore reduces the scatter. The conditional analysis also reduces the relative importance of self‐correlation. Difficulties with estimating self‐correlation are also discussed. Copyright © 2004 Royal Meteorological Society
doi_str_mv 10.1256/qj.03.161
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subjects CASES99
Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Monin–Obukhov similarity
Nocturnal boundary layer
z‐less similarity
title Flux–gradient relationship, self‐correlation and intermittency in the stable boundary layer
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