@Article{BolzanRamSaRodRos:2002:AnFiCa,
author = "Bolzan, Mauricio Jose Alves and Ramos, Fernando Manuel and Sa,
Leonardo Deane de Abreu and Rodrigues Neto, Camilo and Rosa,
Reinaldo Roberto",
affiliation = "{Instituto Nacional de Pesquisas Espaciais. Centro de
Previs{\~a}o do Tempo e Estudos Clim{\'a}ticos (INPE.CPTEC)} and
Instituto Nacional de Pesquisas Espaciais, Laborat{\'o}rio
Associado de Matem{\'a}tica e Computa{\c{c}}{\~a}o Aplicada
(INPE.LAC) and {Instituto Nacional de Pesquisas Espaciais. Centro
de Previs{\~a}o do Tempo e Estudos Clim{\'a}ticos (INPE.CPTEC)}
and Instituto Nacional de Pesquisas Espaciais, Laborat{\'o}rio
Associado de Matem{\'a}tica e Computa{\c{c}}{\~a}o Aplicada
(INPE.LAC) and Instituto Nacional de Pesquisas Espaciais,
Laborat{\'o}rio Associado de Matem{\'a}tica e
Computa{\c{c}}{\~a}o Aplicada (INPE.LAC)",
title = "Analysis of fine-scale canopy turbulence within and above an
Amazon Forest using Tsallis' Generalized thermostatistics",
journal = "Journal of Geophysical Research",
year = "2002",
volume = "107",
number = "D20",
pages = "art. no. 8063",
keywords = "METEOROLOGY, Turbulence, Amazonian forest, Intermittency, Tsallis'
entropy, Atmospheric surface-layer, Fully-developed turbulence,
Probability density, Deciduous forest, Taylors hypothesis,
Coherent eddies, Reynolds-stress, Boundary-layer, Rain-forest,
METEOROLOGIA, Turbul{\^e}ncia, Floresta Amaz{\^o}nica.",
abstract = "We analyzed the probability density function (PDF)of velocity and
temperature differences in the canopy sublayer of Amazonia based
on Tsallis' generalized thermostatistics theory. We show that such
a theory provides an accurate framework for modeling the
statistical behavior of the inertial subrange above and below the
canopy. For this, we compared the experimental PDFs with the
theoretically predicted ones. The data were measured during the
wet season of the Large-Scale Biosphere-Atmosphere Experiment in
Amazonia (LBA), which was carried out during the months of
January-March 1999 in the southwestern part of Amazonia region.
Measurements were made simultaneously at different heights in a 60
m micrometeorological tower located in the Biological Reserve of
Jaru (10degrees04'S, 61degrees56'W), Brazil. The fast response
wind speed measurements, sampled at 60 Hz rate, were made using
three-dimensional sonic anemometers at the heights of 66 m (above
the canopy)and 21 m (below the canopy). The results showed good
agreement between experimental data measured above the canopy
forest and Tsallis' generalized thermostatistics theory. For below
canopy data, the agreement between experimental and theoretical
PDFs was fairly good, but some distortion was observed. This is
probably due to some peculiar characteristics of turbulent
momentum transfer process inside the forest crown. Discussion is
presented to explain these results. Conclusions regarding the
absence of {"}universal scaling{"} in the inertial subrange are
also presented in the context of the entropic parameter of
Tsallis' theory.",
copyholder = "SID/SCD",
issn = "0148-0227 and 2156-2202",
language = "en",
targetfile = "Bolzan_Analysis_of_fine-scale.pdf",
urlaccessdate = "23 abr. 2024"
}