Use este identificador para citar ou linkar para este item: http://www.alice.cnptia.embrapa.br/alice/handle/doc/1055916
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dc.contributor.authorZAHN, E.pt_BR
dc.contributor.authorDIAS, N. L.pt_BR
dc.contributor.authorARAUJO, A.pt_BR
dc.contributor.authorSÁ, L.pt_BR
dc.contributor.authorSÖRGEL, M.pt_BR
dc.contributor.authorTREBS, I.pt_BR
dc.contributor.authorWOLFF, S.pt_BR
dc.contributor.authorMANZI, A.pt_BR
dc.date.accessioned2016-11-04T11:11:11Zpt_BR
dc.date.available2016-11-04T11:11:11Zpt_BR
dc.date.created2016-11-04pt_BR
dc.date.issued2016pt_BR
dc.identifier.citationAtmospheric Chemistry and Physics Discussions, 18 Jan. 2016.pt_BR
dc.identifier.urihttp://www.alice.cnptia.embrapa.br/alice/handle/doc/1055916pt_BR
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.pt_BR
dc.language.isoporpt_BR
dc.rightsopenAccesspt_BR
dc.titleScalar turbulent behavior in the roughness sublayer of an Amazonian forest.pt_BR
dc.typeArtigo de periódicopt_BR
dc.date.updated2017-03-03T11:11:11Zpt_BR
dc.subject.thesagroClimatologiapt_BR
dc.subject.thesagroFloresta Tropicalpt_BR
riaa.ainfo.id1055916pt_BR
riaa.ainfo.lastupdate2017-03-03pt_BR
dc.identifier.doi10.5194/acp-2015-1043pt_BR
dc.contributor.institutionEINARA ZAHN, UFPRpt_BR
dc.contributor.institutionNELSON L. DIAS, UFPRpt_BR
dc.contributor.institutionALESSANDRO CARIOCA DE ARAUJO, CPATUpt_BR
dc.contributor.institutionLEONARDO SÁ, INPEpt_BR
dc.contributor.institutionMATTHIAS SÖERGE, Max Planck Institute for Chemistrypt_BR
dc.contributor.institutionIVONNE TREBS, ERINpt_BR
dc.contributor.institutionSTEFAN WOLFF, Max Planck Institute for Chemistrypt_BR
dc.contributor.institutionANTÔNIO MANZI, INPA.pt_BR
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