Use este identificador para citar ou linkar para este item: https://repositorio.inpa.gov.br/handle/1/16674
Registro completo de metadados
Campo DCValorIdioma
dc.contributor.authorDias Júnior, Cléo Quaresma-
dc.contributor.authorDias, Nelson Luís da Costa-
dc.contributor.authordos Santos, Rosa Maria Nascimento-
dc.contributor.authorSörgel, Matthias-
dc.contributor.authorAraüjo, Alessandro Carioca de-
dc.contributor.authorTsokankunku, Anywhere-
dc.contributor.authorDitas, Florian-
dc.contributor.authorSantana, Raoni Aquino Silva de-
dc.contributor.authorRandow, Celso Von-
dc.contributor.authorMarta, S. Á.-
dc.contributor.authorPöhlker, Christopher-
dc.contributor.authorMachado, Luiz Augusto Toledo-
dc.contributor.authorSá, Leonardo Deane de-
dc.contributor.authorMorán-Zuloaga, Daniel-
dc.contributor.authorJanssen, Ruud H.H.-
dc.contributor.authorAcevedo, Otávio C.-
dc.contributor.authorOliveira, Pablo E.S.-
dc.contributor.authorFisch, Gilberto Fernando-
dc.contributor.authorChor, Tomás L.-
dc.contributor.authorManzi, Antônio Ocimar-
dc.date.accessioned2020-06-15T21:35:41Z-
dc.date.available2020-06-15T21:35:41Z-
dc.date.issued2019-
dc.identifier.urihttps://repositorio.inpa.gov.br/handle/1/16674-
dc.description.abstractOn the basis of measurements over different surfaces, an inertial sublayer (ISL), where Monin-Obukhov Similarity Theory applies, exists above z=3h, where h is canopy height. The roughness sublayer is within h<z<3h. Most studies of the surface layer above forests, however, are able to probe only a narrow region above h. Therefore, direct verification of an ISL above tall forests is difficult. In this study we conducted a systematic analysis of unstable turbulence characteristics at heights from 40 to 325 m, measured at an 80m, and the recently built 325-m Amazon Tall Tower Observatory towers over the Amazon forest. Our analyses have revealed no indication of the existence of an ISL; instead, the roughness sublayer directly merges with the convective mixed layer above. Implications for estimates of momentum and scalar fluxes in numerical models and observational studies can be significant. ©2019. American Geophysical Union. All Rights Reserved.en
dc.language.isoenpt_BR
dc.relation.ispartofVolume 46, Número 10, Pags. 5614-5622pt_BR
dc.rightsRestrito*
dc.subjectSurface Roughnessen
dc.subjectAmazon Forestsen
dc.subjectInertial Sublayeren
dc.subjectMonin-obukhov Similarity Theoryen
dc.subjectRoughness Sublayersen
dc.subjectSurface Layersen
dc.subjectForestryen
dc.subjectAtmospheric Convectionen
dc.subjectBoundary Layeren
dc.subjectFlux Measurementen
dc.subjectForest Canopyen
dc.subjectMixed Layeren
dc.subjectSurface Layeren
dc.subjectSurface Roughnessen
dc.subjectTurbulenceen
dc.subjectAmazoniaen
dc.titleIs There a Classical Inertial Sublayer Over the Amazon Forest?en
dc.typeArtigopt_BR
dc.identifier.doi10.1029/2019GL083237-
dc.publisher.journalGeophysical Research Letterspt_BR
Aparece nas coleções:Artigos

Arquivos associados a este item:
Não existem arquivos associados a este item.


Os itens no repositório estão protegidos por copyright, com todos os direitos reservados, salvo quando é indicado o contrário.