Scalar turbulent behavior in the roughness sublayer of an Amazonian forest.

An important current problem in micrometeorology is the characterization of turbulence in the roughness sublayer (RSL), where most of the measurements above tall forests are made. There, scalar turbulent fluctuations display significant departures from the predictions of Monin?Obukhov similarity theory (MOST). In this work, we analyze turbulence data of virtual temperature, carbon dioxide, and water vapor in the RSL above an Amazonian forest (with a canopy height of 40?m), measured at 39.4 and 81.6?m above the ground under unstable conditions. We found that dimensionless statistics related to the rate of dissipation of turbulence kinetic energy (TKE) and the scalar variance display significant departures from MOST as expected, whereas the vertical velocity variance follows MOST much more closely. Much better agreement between the dimensionless statistics with the Obukhov similarity variable, however, was found for the subset of measurements made at a low zenith angle Z, in the range 0°??<??|Z|??<??20°. We conjecture that this improvement is due to the relationship between sunlight incidence and the ?activation?deactivation? of scalar sinks and sources vertically distributed in the forest. Finally, we evaluated the relaxation coefficient of relaxed eddy accumulation: it is also affected by zenith angle, with considerable improvement in the range 0°??<??|Z|??<??20°, and its values fall within the range reported in the literature for the unstable surface layer. In general, our results indicate the possibility of better stability-derived flux estimates for low zenith angle ranges.

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Main Authors: ZAHN, E., DIAS, N. L., ARAUJO, A., SÁ, L., SÖRGEL, M., TREBS, I., WOLFF, S., MANZI, A.
Other Authors: EINARA ZAHN, UFPR
Format: Artigo de periódico biblioteca
Language:pt_BR
por
Published: 2016-11-04
Subjects:Climatologia, Floresta Tropical.,
Online Access:http://www.alice.cnptia.embrapa.br/alice/handle/doc/1055916
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spelling dig-alice-doc-10559162017-08-16T02:54:15Z Scalar turbulent behavior in the roughness sublayer of an Amazonian forest. ZAHN, E. DIAS, N. L. ARAUJO, A. SÁ, L. SÖRGEL, M. TREBS, I. WOLFF, S. MANZI, A. EINARA ZAHN, UFPR NELSON L. DIAS, UFPR ALESSANDRO CARIOCA DE ARAUJO, CPATU LEONARDO SÁ, INPE MATTHIAS SÖERGE, Max Planck Institute for Chemistry IVONNE TREBS, ERIN STEFAN WOLFF, Max Planck Institute for Chemistry ANTÔNIO MANZI, INPA. Climatologia Floresta Tropical. An important current problem in micrometeorology is the characterization of turbulence in the roughness sublayer (RSL), where most of the measurements above tall forests are made. There, scalar turbulent fluctuations display significant departures from the predictions of Monin?Obukhov similarity theory (MOST). In this work, we analyze turbulence data of virtual temperature, carbon dioxide, and water vapor in the RSL above an Amazonian forest (with a canopy height of 40?m), measured at 39.4 and 81.6?m above the ground under unstable conditions. We found that dimensionless statistics related to the rate of dissipation of turbulence kinetic energy (TKE) and the scalar variance display significant departures from MOST as expected, whereas the vertical velocity variance follows MOST much more closely. Much better agreement between the dimensionless statistics with the Obukhov similarity variable, however, was found for the subset of measurements made at a low zenith angle Z, in the range 0°??<??|Z|??<??20°. We conjecture that this improvement is due to the relationship between sunlight incidence and the ?activation?deactivation? of scalar sinks and sources vertically distributed in the forest. Finally, we evaluated the relaxation coefficient of relaxed eddy accumulation: it is also affected by zenith angle, with considerable improvement in the range 0°??<??|Z|??<??20°, and its values fall within the range reported in the literature for the unstable surface layer. In general, our results indicate the possibility of better stability-derived flux estimates for low zenith angle ranges. 2016-11-04T11:11:11Z 2016-11-04T11:11:11Z 2016-11-04 2016 2017-03-03T11:11:11Z Artigo de periódico Atmospheric Chemistry and Physics Discussions, 18 Jan. 2016. http://www.alice.cnptia.embrapa.br/alice/handle/doc/1055916 10.5194/acp-2015-1043 pt_BR por openAccess
institution EMBRAPA
collection DSpace
country Brasil
countrycode BR
component Bibliográfico
access En linea
databasecode dig-alice
tag biblioteca
region America del Sur
libraryname Sistema de bibliotecas de EMBRAPA
language pt_BR
por
topic Climatologia
Floresta Tropical.
Climatologia
Floresta Tropical.
spellingShingle Climatologia
Floresta Tropical.
Climatologia
Floresta Tropical.
ZAHN, E.
DIAS, N. L.
ARAUJO, A.
SÁ, L.
SÖRGEL, M.
TREBS, I.
WOLFF, S.
MANZI, A.
Scalar turbulent behavior in the roughness sublayer of an Amazonian forest.
description An important current problem in micrometeorology is the characterization of turbulence in the roughness sublayer (RSL), where most of the measurements above tall forests are made. There, scalar turbulent fluctuations display significant departures from the predictions of Monin?Obukhov similarity theory (MOST). In this work, we analyze turbulence data of virtual temperature, carbon dioxide, and water vapor in the RSL above an Amazonian forest (with a canopy height of 40?m), measured at 39.4 and 81.6?m above the ground under unstable conditions. We found that dimensionless statistics related to the rate of dissipation of turbulence kinetic energy (TKE) and the scalar variance display significant departures from MOST as expected, whereas the vertical velocity variance follows MOST much more closely. Much better agreement between the dimensionless statistics with the Obukhov similarity variable, however, was found for the subset of measurements made at a low zenith angle Z, in the range 0°??<??|Z|??<??20°. We conjecture that this improvement is due to the relationship between sunlight incidence and the ?activation?deactivation? of scalar sinks and sources vertically distributed in the forest. Finally, we evaluated the relaxation coefficient of relaxed eddy accumulation: it is also affected by zenith angle, with considerable improvement in the range 0°??<??|Z|??<??20°, and its values fall within the range reported in the literature for the unstable surface layer. In general, our results indicate the possibility of better stability-derived flux estimates for low zenith angle ranges.
author2 EINARA ZAHN, UFPR
author_facet EINARA ZAHN, UFPR
ZAHN, E.
DIAS, N. L.
ARAUJO, A.
SÁ, L.
SÖRGEL, M.
TREBS, I.
WOLFF, S.
MANZI, A.
format Artigo de periódico
topic_facet Climatologia
Floresta Tropical.
author ZAHN, E.
DIAS, N. L.
ARAUJO, A.
SÁ, L.
SÖRGEL, M.
TREBS, I.
WOLFF, S.
MANZI, A.
author_sort ZAHN, E.
title Scalar turbulent behavior in the roughness sublayer of an Amazonian forest.
title_short Scalar turbulent behavior in the roughness sublayer of an Amazonian forest.
title_full Scalar turbulent behavior in the roughness sublayer of an Amazonian forest.
title_fullStr Scalar turbulent behavior in the roughness sublayer of an Amazonian forest.
title_full_unstemmed Scalar turbulent behavior in the roughness sublayer of an Amazonian forest.
title_sort scalar turbulent behavior in the roughness sublayer of an amazonian forest.
publishDate 2016-11-04
url http://www.alice.cnptia.embrapa.br/alice/handle/doc/1055916
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