The ATTO-Campina site: A new observatory for tropical convection and gas-aerosol-cloud-precipitation interactions in the Amazon

Abstract We present results from ATTO-Campina, a new permanent observational site in central Amazon, about 4 km from the ATTO towers. Operational since 2020, ATTO-Campina characterizes atmospheric, cloud and rainfall properties through remote sensing. The goal is to provide continuous, complementary measurements to the ATTO towers, addressing the rainforest’s complex gas-aerosol-cloud-precipitation dynamics. Using a 3.5-year dataset, we classified convective clouds into three types: shallow cumulus ( ShCu ), congestus ( Con ) or ( Deep ) clouds. The shallow-to-deep transition takes about three hours, starting with ShCu formation at 11:00 local time. The accumulated rainfall peak follows at about 16:00. Only weak downdrafts are present in the upper troposphere where previous studies indicate new particle formation (NPF) occurrence. Strong downdrafts are mostly limited to heights below 5 km. Con and Deep convective days have higher concentrations of ultrafine aerosol and lower concentrations of accumulation-mode particles compared to ShCu . Convective clouds also significantly modify gas mixing ratios. Deep convective clouds are associated with high near-surface O 3 , consistent with downward transport from the midtroposphere. Our results showcase the added detail achieved by integrating data from the ATTO towers and ATTO-Campina sites. Together, these sites support better understanding of interconnected gas-aerosol-cloud-precipitation processes in the Amazon and their evolution under climate change.

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Journal
Bulletin of the American Meteorological Society
Published
2025-10-21
DOI
https://doi.org/10.1175/bams-d-24-0092.1
Primary Topic
Environmental and biological studies
Type
article
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article

The ATTO-Campina site: A new observatory for tropical convection and gas-aerosol-cloud-precipitation interactions in the Amazon

Arturo Balderas Torres, Philipp Faulhammer, M. Conde, Susan Trumbore et al.
Bulletin of the American Meteorological Society
Environmental and biological studies
article

The ATTO-Campina site: A new observatory for tropical convection and gas-aerosol-cloud-precipitation interactions in the Amazon

Arturo Balderas Torres, Philipp Faulhammer, M. Conde, Susan Trumbore, Rachel I. Albrecht, Patric Seifert, Micael A. Cecchini, Christopher R. Williams, Subha S. Raj, Alan J. P. Calheiros, Cybelli G. G. Barbosa, Hartwig Harder, Anywhere Tsokankunku, Flávio C. Magina, Mira L. Pöhlker, Bettina Weber, Cléo Quaresma Dias‐Júnior, Jordi Vilà-Guerau De Arellano, Jos Lelieveld, J. Kesselmeier, Ivan Saraiva, Gholamhossein Bagheri, Scott Edward Giangrande, A. Massafferri, Rafael Delmond Bueno, J. Christine Chiu, Luiz A. T. Machado, Thiago Biscaro, Eberhard Bodenschatz, Fernando G. Morais, Ulrich Pöschl, Marco A. Franco, Carolina Monteiro, André C. Pugliesi, Jonathan Williams, Maria Isabel D. Rossi, Luiz Fernando Sapucci, Rodrigo Augusto Ferreira De Souza, Meinrat O. Andreae, Dirceu Luís Herdies, Edio da Costa, Laura Brito, Santiago Botía, Hella van Asperen, Sam P. Jones, Gabriela R. Unfer, Stefan Herdy, Guido G. Haytzmann, Wanda I. D. Valenti, Dina Silva, Caio Henrique Santos Lopes, Carla Maria Alves Souza, Carlos A. Quesada, Friederike Lipken, Ferreira Silva, Luciana V. Rizzo, L.M. Camargo, Bruno Takeshi, Henrique M. J. Barbosa, Christopher Pöhlker, Tabata L. B. de Macêdo, Gabriel G. Balestra, Amábile S. Bighetto, Marina C. S. Neofiti, Puig B. Raidiel
article en

Abstract

Abstract We present results from ATTO-Campina, a new permanent observational site in central Amazon, about 4 km from the ATTO towers. Operational since 2020, ATTO-Campina characterizes atmospheric, cloud and rainfall properties through remote sensing. The goal is to provide continuous, complementary measurements to the ATTO towers, addressing the rainforest’s complex gas-aerosol-cloud-precipitation dynamics. Using a 3.5-year dataset, we classified convective clouds into three types: shallow cumulus ( ShCu ), congestus ( Con ) or ( Deep ) clouds. The shallow-to-deep transition takes about three hours, starting with ShCu formation at 11:00 local time. The accumulated rainfall peak follows at about 16:00. Only weak downdrafts are present in the upper troposphere where previous studies indicate new particle formation (NPF) occurrence. Strong downdrafts are mostly limited to heights below 5 km. Con and Deep convective days have higher concentrations of ultrafine aerosol and lower concentrations of accumulation-mode particles compared to ShCu . Convective clouds also significantly modify gas mixing ratios. Deep convective clouds are associated with high near-surface O 3 , consistent with downward transport from the midtroposphere. Our results showcase the added detail achieved by integrating data from the ATTO towers and ATTO-Campina sites. Together, these sites support better understanding of interconnected gas-aerosol-cloud-precipitation processes in the Amazon and their evolution under climate change.

Bulletin of the American Meteorological Society
Scripps Institution of Oceanography (US), University of Graz (AT), Universidade de São Paulo (BR), Instituto Nacional de Pesquisas da Amazônia (BR), University of Colorado Boulder (US), Brookhaven National Laboratory (US), King Saud University (SA), Instituto Federal de Educação, Ciência e Tecnologia do Pará (BR), Max Planck Institute for Chemistry (DE), Leibniz Institute for Tropospheric Research (DE), Centro Brasileiro de Pesquisas Físicas (BR), Proteca (Brazil) (BR), Escola Superior de Ciências da Saúde (BR), Universidade do Estado do Amazonas (BR), Max Planck Institute for Biogeochemistry (DE), University of Maryland, Baltimore County (US), Instituto Nacional de Pesquisas Espaciais (BR), Wageningen University & Research (NL), Colorado State University (US)
Openalex Percentile: Top 71%
Environmental and biological studies
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