Amazon boundary layer aerosol concentration sustained by vertical transport during rainfall

Pequeñas partículas en la
troposfera libre
descienden durante eventos de lluvia
Cloud condensation nuclei
Amazon rainforest
Autores/as

Jian Wang

Radovan Krejci

Scott Giangrande

Chongai Kuang

Henrique M. J. Barbosa

Joel Brito

Samara Carbone

Xuguang Chi

Jennifer Comstock

Florian Ditas

Jost Lavric

Hanna E. Manninen

Fan Mei

Daniel Moran-Zuloaga

Christopher Pöhlker

Mira L. Pöhlker

Jorge Saturno

Beat Schmid

Rodrigo A. F. Souza

Stephen R. Springston

Jason M. Tomlinson

Tami Toto

David Walter

Daniela Wimmer

James N. Smith

Markku Kulmala

Luiz A. T. Machado

Paulo Artaxo

Meinrat O. Andreae

Tuukka Petäjä

Scot T. Martin

Fecha de publicación

octubre 2016

Doi
Otros detalles

The Amazon rainforest is one of the few continental regions where atmospheric aerosol processes can be studied under near-natural conditions, but the origin of small aerosol particles that grow into cloud condensation nuclei in the Amazon boundary layer remains poorly understood. This paper reports rapid vertical transport of small aerosol particles from the free troposphere into the boundary layer during precipitation events by strong convective downdrafts and weaker downward motions in the trailing stratiform region. This effect can help to maintain the population of aerosol particles in the pristine Amazon boundary layer, so may influence cloud properties and climate under natural conditions.

Abstract

The nucleation of atmospheric vapours is an important source of new aerosol particles that can subsequently grow to form cloud condensation nuclei in the atmosphere. Most field studies of atmospheric aerosols over continents are influenced by atmospheric vapours of anthropogenic origin (for example, ref. 2) and, in consequence, aerosol processes in pristine, terrestrial environments remain poorly understood. The Amazon rainforest is one of the few continental regions where aerosol particles and their precursors can be studied under near-natural conditions but the origin of small aerosol particles that grow into cloud condensation nuclei in the Amazon boundary layer remains unclear. Here we present aircraft- and ground-based measurements under clean conditions during the wet season in the central Amazon basin. We find that high concentrations of small aerosol particles (with diameters of less than 50 nanometres) in the lower free troposphere are transported from the free troposphere into the boundary layer during precipitation events by strong convective downdrafts and weaker downward motions in the trailing stratiform region. This rapid vertical transport can help to maintain the population of particles in the pristine Amazon boundary layer, and may therefore influence cloud properties and climate under natural conditions.

Citation

@article{Wang2016,
 author = {Wang, Jian and Krejci, Radovan and Giangrande, Scott and Kuang, Chongai and Barbosa, Henrique M. J. and Brito, Joel and Carbone, Samara and Chi, Xuguang and Comstock, Jennifer and Ditas, Florian and Lavric, Jost and Manninen, Hanna E. and Mei, Fan and Moran-Zuloaga, Daniel and Pöhlker, Christopher and Pöhlker, Mira L. and Saturno, Jorge and Schmid, Beat and Souza, Rodrigo A. F. and Springston, Stephen R. and Tomlinson, Jason M. and Toto, Tami and Walter, David and Wimmer, Daniela and Smith, James N. and Kulmala, Markku and Machado, Luiz A. T. and Artaxo, Paulo and Andreae, Meinrat O. and Petäjä, Tuukka and Martin, Scot T.},
 doi = {10.1038/nature19819},
 issn = {0028-0836},
 journal = {Nature},
 keywords = {Amazon,CLouds},
 mendeley-tags = {Amazon,CLouds},
 month = {oct},
 pages = {1--17},
 publisher = {Nature Publishing Group},
 title = {Amazon boundary layer aerosol concentration sustained by vertical transport during rainfall},
 url = {http://dx.doi.org/10.1038/nature19819 http://www.nature.com/doifinder/10.1038/nature19819},
 year = {2016}
}