Articles | Volume 20, issue 1
https://doi.org/10.5194/acp-20-15-2020
https://doi.org/10.5194/acp-20-15-2020
Research article
 | 
02 Jan 2020
Research article |  | 02 Jan 2020

Planetary boundary layer evolution over the Amazon rainforest in episodes of deep moist convection at the Amazon Tall Tower Observatory

Maurício I. Oliveira, Otávio C. Acevedo, Matthias Sörgel, Ernani L. Nascimento, Antonio O. Manzi, Pablo E. S. Oliveira, Daiane V. Brondani, Anywhere Tsokankunku, and Meinrat O. Andreae

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Pablo E. S. Oliveira on behalf of the Authors (17 Oct 2019)  Author's response   Manuscript 
ED: Publish as is (03 Nov 2019) by Gilberto Fisch
AR by Pablo E. S. Oliveira on behalf of the Authors (11 Nov 2019)  Manuscript 
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Short summary
In this study, data collected during four deep convection events at the 80 m tower from the Amazon Tall Tower Observatory are analyzed. It provides a unique view on how such events affect the local boundary layer and how it recovers after their passage. Quantities analyzed include mean wind speed, virtual potential temperature, turbulent kinetic energy, sensible, and latent heat fluxes. A conceptual model for boundary layer structure along the passage of deep convection events is proposed.
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