Articles | Volume 18, issue 14
https://doi.org/10.5194/acp-18-10255-2018
© Author(s) 2018. 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-18-10255-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
19 Jul 2018
Research article |
| 19 Jul 2018
| 19 Jul 2018
Multi-year statistical and modeling analysis of submicrometer aerosol number size distributions at a rain forest site in Amazonia
Departamento de Ciências Ambientais, Universidade Federal de São Paulo, Diadema, Brazil
Pontus Roldin
Department of Physics, Lund University, Lund, Sweden
Joel Brito
Instituto de Física, Universidade de São Paulo, São Paulo, Brazil
now at: Laboratory for Meteorological Physics, Université Clermont Auvergne, Clermont-Ferrand, France
John Backman
Department of Physics, University of Helsinki, Helsinki, Finland
now at: Finnish Meteorological Institute, Atmospheric Composition Research, Helsinki, Finland
Erik Swietlicki
Department of Physics, Lund University, Lund, Sweden
Radovan Krejci
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, Stockholm, Sweden
Peter Tunved
Department of Environmental Science and Analytical Chemistry (ACES), Stockholm University, Stockholm, Sweden
Tukka Petäjä
Department of Physics, University of Helsinki, Helsinki, Finland
Markku Kulmala
Department of Physics, University of Helsinki, Helsinki, Finland
Paulo Artaxo
Instituto de Física, Universidade de São Paulo, São Paulo, Brazil
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Cited
19 citations as recorded by crossref.
- CRI-HOM: A novel chemical mechanism for simulating highly oxygenated organic molecules (HOMs) in global chemistry–aerosol–climate models J. Weber et al. 10.5194/acp-20-10889-2020
- Formation Process of Particles and Cloud Condensation Nuclei Over the Amazon Rainforest: The Role of Local and Remote New‐Particle Formation B. Zhao et al. 10.1029/2022GL100940
- On the Sensitivity of a Ground-Based Tropospheric Lidar to Aitken Mode Particles in the Upper Troposphere M. Silva et al. 10.3390/rs14194913
- Frequent new particle formation at remote sites in the subboreal forest of North America M. Andreae et al. 10.5194/acp-22-2487-2022
- Importance of Hydroxyl Radical Chemistry in Isoprene Suppression of Particle Formation from α-Pinene Ozonolysis Y. Wang et al. 10.1021/acsearthspacechem.0c00294
- Decrease in radiative forcing by organic aerosol nucleation, climate, and land use change J. Zhu et al. 10.1038/s41467-019-08407-7
- Contribution of regional aerosol nucleation to low-level CCN in an Amazonian deep convective environment: results from a regionally nested global model X. Wang et al. 10.5194/acp-23-4431-2023
- On the seasonal variation in observed size distributions in northern Europe and their changes with decreasing anthropogenic emissions in Europe: climatology and trend analysis based on 17 years of data from Aspvreten, Sweden P. Tunved & J. Ström 10.5194/acp-19-14849-2019
- How weather events modify aerosol particle size distributions in the Amazon boundary layer L. Machado et al. 10.5194/acp-21-18065-2021
- The Atmospheric Aerosol over Western Greece-Six Years of Aerosol Observations at the Navarino Environmental Observatory H. Hansson et al. 10.3390/atmos12040445
- Tropical and Boreal Forest – Atmosphere Interactions: A Review P. Artaxo et al. 10.16993/tellusb.34
- New Particle Formation in the Atmosphere: From Molecular Clusters to Global Climate S. Lee et al. 10.1029/2018JD029356
- Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
- Temperature effects on sulfuric acid aerosol nucleation and growth: initial results from the TANGENT study L. Tiszenkel et al. 10.5194/acp-19-8915-2019
- Molecular understanding of the suppression of new-particle formation by isoprene M. Heinritzi et al. 10.5194/acp-20-11809-2020
- High contribution of new particle formation to ultrafine particles in four seasons in an urban atmosphere in south China L. Tao et al. 10.1016/j.scitotenv.2023.164202
- Occurrence and growth of sub-50 nm aerosol particles in the Amazonian boundary layer M. Franco et al. 10.5194/acp-22-3469-2022
- Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season H. Glicker et al. 10.5194/acp-19-13053-2019
- Amazonian aerosol size distributions in a lognormal phase space: characteristics and trajectories G. Unfer et al. 10.5194/acp-24-3869-2024
19 citations as recorded by crossref.
- CRI-HOM: A novel chemical mechanism for simulating highly oxygenated organic molecules (HOMs) in global chemistry–aerosol–climate models J. Weber et al. 10.5194/acp-20-10889-2020
- Formation Process of Particles and Cloud Condensation Nuclei Over the Amazon Rainforest: The Role of Local and Remote New‐Particle Formation B. Zhao et al. 10.1029/2022GL100940
- On the Sensitivity of a Ground-Based Tropospheric Lidar to Aitken Mode Particles in the Upper Troposphere M. Silva et al. 10.3390/rs14194913
- Frequent new particle formation at remote sites in the subboreal forest of North America M. Andreae et al. 10.5194/acp-22-2487-2022
- Importance of Hydroxyl Radical Chemistry in Isoprene Suppression of Particle Formation from α-Pinene Ozonolysis Y. Wang et al. 10.1021/acsearthspacechem.0c00294
- Decrease in radiative forcing by organic aerosol nucleation, climate, and land use change J. Zhu et al. 10.1038/s41467-019-08407-7
- Contribution of regional aerosol nucleation to low-level CCN in an Amazonian deep convective environment: results from a regionally nested global model X. Wang et al. 10.5194/acp-23-4431-2023
- On the seasonal variation in observed size distributions in northern Europe and their changes with decreasing anthropogenic emissions in Europe: climatology and trend analysis based on 17 years of data from Aspvreten, Sweden P. Tunved & J. Ström 10.5194/acp-19-14849-2019
- How weather events modify aerosol particle size distributions in the Amazon boundary layer L. Machado et al. 10.5194/acp-21-18065-2021
- The Atmospheric Aerosol over Western Greece-Six Years of Aerosol Observations at the Navarino Environmental Observatory H. Hansson et al. 10.3390/atmos12040445
- Tropical and Boreal Forest – Atmosphere Interactions: A Review P. Artaxo et al. 10.16993/tellusb.34
- New Particle Formation in the Atmosphere: From Molecular Clusters to Global Climate S. Lee et al. 10.1029/2018JD029356
- Atmospheric new particle formation and growth: review of field observations V. Kerminen et al. 10.1088/1748-9326/aadf3c
- Temperature effects on sulfuric acid aerosol nucleation and growth: initial results from the TANGENT study L. Tiszenkel et al. 10.5194/acp-19-8915-2019
- Molecular understanding of the suppression of new-particle formation by isoprene M. Heinritzi et al. 10.5194/acp-20-11809-2020
- High contribution of new particle formation to ultrafine particles in four seasons in an urban atmosphere in south China L. Tao et al. 10.1016/j.scitotenv.2023.164202
- Occurrence and growth of sub-50 nm aerosol particles in the Amazonian boundary layer M. Franco et al. 10.5194/acp-22-3469-2022
- Chemical composition of ultrafine aerosol particles in central Amazonia during the wet season H. Glicker et al. 10.5194/acp-19-13053-2019
- Amazonian aerosol size distributions in a lognormal phase space: characteristics and trajectories G. Unfer et al. 10.5194/acp-24-3869-2024
Latest update: 18 Apr 2024
Short summary
Aerosols are tiny particles suspended in the air that can interact with sunlight and form clouds, which in turn affect the climate. They can also recycle nutrients in forest environments. Aerosols are naturally emitted at the surface in the Amazon forest, in addition to being brought down from above the boundary layer by intense air movements. In this work, we describe how the particle size number concentrations of aerosols change over hours, days and seasons in a multi-year study in Amazonia.
Aerosols are tiny particles suspended in the air that can interact with sunlight and form...
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