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@ARTICLE{Graf:8873,
author = {Graf, A. and Schüttemeyer, D. and Geiss, H. and Knaps, A.
and Möllmann-Coers, M. and Schween, J.H. and Kollet, S. and
Neininger, B. and Herbst, M. and Vereecken, H.},
title = {{B}oundedness of turbulent temperature probability
distributions, and their relation to the vertical profile in
the convective boundary layer},
journal = {Boundary layer meteorology},
volume = {134},
issn = {0006-8314},
address = {Dordrecht [u.a.]},
publisher = {Springer Science + Business Media B.V},
reportid = {PreJuSER-8873},
pages = {459 - 486},
year = {2010},
note = {We gratefully acknowledge field assistance by Rainer Harms
(Julich Research Centre) and Martin Lennefer (Bonn
University), financial support by the Helmholtz-funded
FLOWatch project and by the Transregional collaborative
research centre (SFB/TR) 32 "Patterns in
Soil-Vegetation-Atmosphere Systems: Monitoring, Modelling,
and Data Assimilation" funded by the Deutsche
Forschungsgemeinschaft (DFG), by the DFG project GR2687/3-1,
and valuable comments of two anonymous referees.},
abstract = {Higher-order moments, minima and maxima of turbulent
temperature and water vapour mixing ratio probability
density functions measured with an eddy-covariance system
near the ground were related to each other and to vertical
boundary-layer profiles of the same scalars obtained through
airborne soundings. The dependence of kurtosis on squared
skewness showed a kurtosis intercept below the Gaussian
expectation, suggesting a compression of the probability
density function by the presence of natural boundaries. This
hypothesis was corroborated by comparing actual minima and
maxima of turbulent fluctuations to estimates obtained from
the first four sample moments by fitting a four-parameter
beta distribution. The most sharply defined boundaries were
found for the minima of temperature datasets during the day,
indicating that negative temperature fluctuations at the
sensor are limited by the availability of lower temperatures
in the boundary layer. By comparison to vertical profiles,
it could be verified that the turbulent minimum of
temperature near the ground is close to the minimum of
potential temperature in the boundary layer. The turbulent
minimum of water vapour mixing ratio was found to be equal
to the mixing ratio at a height above the minimum of the
temperature profile. This height roughly agrees with the top
of the non-local unstable domain according to bulk
Richardson number profiles. We conclude that turbulence
statistics measured near the surface cannot be solely
explained by local effects, but contain information about
the whole boundary layer including the entrainment zone.},
keywords = {J (WoSType)},
cin = {ICG-2 / ICG-4 / S},
ddc = {550},
cid = {I:(DE-Juel1)VDB791 / I:(DE-Juel1)VDB793 /
I:(DE-Juel1)VDB224},
pnm = {Atmosphäre und Klima},
pid = {G:(DE-Juel1)FUEK406},
shelfmark = {Meteorology $\&$ Atmospheric Sciences},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000274013600005},
doi = {10.1007/s10546-009-9444-9},
url = {https://juser.fz-juelich.de/record/8873},
}