Articles | Volume 24, issue 2
https://doi.org/10.5194/acp-24-1315-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/acp-24-1315-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
30 Jan 2024
Research article |
| 30 Jan 2024
| 30 Jan 2024
Analysis of atmospheric particle growth based on vapor concentrations measured at the high-altitude GAW station Chacaltaya in the Bolivian Andes
Department of Technical Physics, University of Eastern Finland, 70211 Kuopio, Finland
Cheng Wu
CORRESPONDING AUTHOR
Department of Environmental Science and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
now at: Department of Chemistry and Molecular Biology, University of Gothenburg, Gothenburg, Sweden
Diego Aliaga
Institute for Atmospheric and Earth System Research/Physics, University of Helsinki, 00014 Helsinki, Finland
Luis Blacutt
Laboratorio de Física de la Atmósfera, Instituto de Investigaciones Físicas, Universidad Mayor de San Andrés, La Paz, Bolivia
Xuemeng Chen
Institute for Atmospheric and Earth System Research/Physics, University of Helsinki, 00014 Helsinki, Finland
Yvette Gramlich
Department of Environmental Science and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Liine Heikkinen
Department of Environmental Science and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Wei Huang
Institute for Atmospheric and Earth System Research/Physics, University of Helsinki, 00014 Helsinki, Finland
Radovan Krejci
Department of Environmental Science and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Paolo Laj
Institute for Atmospheric and Earth System Research/Physics, University of Helsinki, 00014 Helsinki, Finland
Institute for Geosciences and Environmental Research (IGE), University of Grenoble Alpes, Grenoble 38000, France
Isabel Moreno
Laboratorio de Física de la Atmósfera, Instituto de Investigaciones Físicas, Universidad Mayor de San Andrés, La Paz, Bolivia
Karine Sellegri
CNRS, Laboratoire de Météorologie Physique (LaMP), Université Clermont Auvergne, 63000 Clermont-Ferrand, France
Fernando Velarde
Laboratorio de Física de la Atmósfera, Instituto de Investigaciones Físicas, Universidad Mayor de San Andrés, La Paz, Bolivia
Kay Weinhold
Leibniz Institute for Tropospheric Research, 04318 Leipzig, Germany
Alfred Wiedensohler
Leibniz Institute for Tropospheric Research, 04318 Leipzig, Germany
Qiaozhi Zha
Institute for Atmospheric and Earth System Research/Physics, University of Helsinki, 00014 Helsinki, Finland
Federico Bianchi
Institute for Atmospheric and Earth System Research/Physics, University of Helsinki, 00014 Helsinki, Finland
Marcos Andrade
Laboratorio de Física de la Atmósfera, Instituto de Investigaciones Físicas, Universidad Mayor de San Andrés, La Paz, Bolivia
Kari E. J. Lehtinen
Department of Technical Physics, University of Eastern Finland, 70211 Kuopio, Finland
Claudia Mohr
Department of Environmental Science and Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
now at: Laboratory of Atmospheric Chemistry, Paul Scherrer Institute, Villigen, Switzerland
Taina Yli-Juuti
Department of Technical Physics, University of Eastern Finland, 70211 Kuopio, Finland
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Latest update: 06 Mar 2025
Short summary
Particle growth at the Chacaltaya station in Bolivia was simulated based on measured vapor concentrations and ambient conditions. Major contributors to the simulated growth were low-volatility organic compounds (LVOCs). Also, sulfuric acid had major role when volcanic activity was occurring in the area. This study provides insight on nanoparticle growth at this high-altitude Southern Hemispheric site and hence contributes to building knowledge of early growth of atmospheric particles.
Particle growth at the Chacaltaya station in Bolivia was simulated based on measured vapor...
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