Is There a Classical Inertial Sublayer Over the Amazon Forest?

On 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

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Bibliographic Details
Published in:Geophysical research letters 2019-05, Vol.46 (10), p.5614-5622
Main Authors: Dias‐Júnior, Cléo Quaresma, Dias, Nelson Luís, Santos, Rosa Maria N., Sörgel, Matthias, Araújo, Alessandro, Tsokankunku, Anywhere, Ditas, Florian, Santana, Raoni Aquino, Randow, Celso, Sá, Marta, Pöhlker, Christopher, Toledo Machado, Luiz Augusto, Sá, Leonardo Deane, Moran‐Zuloaga, Daniel, Janssen, Ruud, Acevedo, Otávio, Oliveira, Pablo, Fisch, Gilberto, Chor, Tomas, Manzi, Antonio
Format: Article
Language:English
Subjects:
Absorption
Amazon forest
Atmospheric models
Carbon dioxide
Climate
Deforestation
Emission
Estimates
Fluxes
Forests
inertial sublayer
Mathematical models
Mixed layer
Momentum
Monin‐Obukhov Similarity Theory
Numerical models
Observational studies
Organic compounds
Ozone
Plant cover
Rainforests
Regional climates
Roughness
roughness sublayer
Similarity theory
Surface boundary layer
Surface chemistry
surface layer
Surface layers
Towers
Turbulence
Vegetation
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Description
Summary:On 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
ISSN:0094-8276
1944-8007
DOI:10.1029/2019GL083237