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

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dc.contributorEINARA ZAHN, UFPR
dc.contributorNELSON L. DIAS, UFPR
dc.contributorALESSANDRO CARIOCA DE ARAUJO, CPATU
dc.contributorLEONARDO SÁ, INPE
dc.contributorMATTHIAS SÖERGE, Max Planck Institute for Chemistry
dc.contributorIVONNE TREBS, ERIN
dc.contributorSTEFAN WOLFF, Max Planck Institute for Chemistry
dc.contributorANTÔNIO MANZI, INPA.
dc.creatorZAHN, E.
dc.creatorDIAS, N. L.
dc.creatorARAUJO, A.
dc.creatorSÁ, L.
dc.creatorSÖRGEL, M.
dc.creatorTREBS, I.
dc.creatorWOLFF, S.
dc.creatorMANZI, A.
dc.date2016-11-04T11:11:11Z
dc.date2016-11-04T11:11:11Z
dc.date2016-11-04
dc.date2016
dc.date2017-03-03T11:11:11Z
dc.date.accessioned2026-06-30T23:43:29Z
dc.descriptionAn 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.
dc.identifierAtmospheric Chemistry and Physics Discussions, 18 Jan. 2016.
dc.identifierhttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1055916
dc.identifier10.5194/acp-2015-1043
dc.identifier.urihttp://hdl.handle.net/123456789/388834
dc.languagepor
dc.rightsopenAccess
dc.subjectClimatologia
dc.subjectFloresta Tropical
dc.titleScalar turbulent behavior in the roughness sublayer of an Amazonian forest.
dc.typeArtigo de periódico

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Embrapa Amazonía Oriental (CPATU)