Articles | Volume 21, issue 22
https://doi.org/10.5194/acp-21-17017-2021
© Author(s) 2021. 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-21-17017-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Origin of water-soluble organic aerosols at the Maïdo high-altitude observatory, Réunion Island, in the tropical Indian Ocean
Sharmine Akter Simu
Graduate School of Environmental Science, Hokkaido University,
Sapporo, 0600810, Japan
Institute of Low Temperature Science, Hokkaido University, Sapporo,
0600819, Japan
Institute of Low Temperature Science, Hokkaido University, Sapporo,
0600819, Japan
Eri Tachibana
Institute of Low Temperature Science, Hokkaido University, Sapporo,
0600819, Japan
Henning Finkenzeller
Department of Chemistry, University of Colorado Boulder, Boulder, CO
80309-0215, USA
Cooperative Institute for Research in Environmental Sciences (CIRES),
University of Colorado Boulder, Boulder, CO, USA
Jérôme Brioude
Laboratoire de l'Atmosphère et des Cyclones, UMR8105, CNRS,
Université de La Réunion, 97744 Saint-Denis, France
Aurélie Colomb
Laboratoire de Météorologie Physique, UMR6016, CNRS,
Université Clermont Auvergne, 63178 Aubière, France
Olivier Magand
Univ. Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, 38000 Grenoble,
France
Bert Verreyken
Laboratoire de l'Atmosphère et des Cyclones, UMR8105, CNRS,
Université de La Réunion, 97744 Saint-Denis, France
Royal Belgian Institute for Space Aeronomy, 1180 Brussels, Belgium
Department of Chemistry, Ghent University, 9000 Ghent, Belgium
Stephanie Evan
Laboratoire de l'Atmosphère et des Cyclones, UMR8105, CNRS,
Université de La Réunion, 97744 Saint-Denis, France
Rainer Volkamer
Department of Chemistry, University of Colorado Boulder, Boulder, CO
80309-0215, USA
Cooperative Institute for Research in Environmental Sciences (CIRES),
University of Colorado Boulder, Boulder, CO, USA
Trissevgeni Stavrakou
Royal Belgian Institute for Space Aeronomy, 1180 Brussels, Belgium
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Cited
6 citations as recorded by crossref.
- A competition–species model for water vapour-aerosol-cloud-rain interactions F. Mascaut et al. 10.1016/j.atmosres.2022.106588
- A review on air–sea exchange of reactive trace gases over the northern Indian Ocean M. Gupta et al. 10.1007/s12040-024-02268-5
- A Competition–Species Model for Water Vapour-Aerosol-Cloud-Rain Interactions F. Mascaut et al. 10.2139/ssrn.4197632
- Evaluation of the Sources, Precursors, and Processing of Aerosols at a High-Altitude Tropical Site P. Dominutti et al. 10.1021/acsearthspacechem.2c00149
- Measurement report: Bio-physicochemistry of tropical clouds at Maïdo (Réunion, Indian Ocean): overview of results from the BIO-MAÏDO campaign M. Leriche et al. 10.5194/acp-24-4129-2024
- Observed in-plume gaseous elemental mercury depletion suggests significant mercury scavenging by volcanic aerosols A. Koenig et al. 10.1039/D3EA00063J
6 citations as recorded by crossref.
- A competition–species model for water vapour-aerosol-cloud-rain interactions F. Mascaut et al. 10.1016/j.atmosres.2022.106588
- A review on air–sea exchange of reactive trace gases over the northern Indian Ocean M. Gupta et al. 10.1007/s12040-024-02268-5
- A Competition–Species Model for Water Vapour-Aerosol-Cloud-Rain Interactions F. Mascaut et al. 10.2139/ssrn.4197632
- Evaluation of the Sources, Precursors, and Processing of Aerosols at a High-Altitude Tropical Site P. Dominutti et al. 10.1021/acsearthspacechem.2c00149
- Measurement report: Bio-physicochemistry of tropical clouds at Maïdo (Réunion, Indian Ocean): overview of results from the BIO-MAÏDO campaign M. Leriche et al. 10.5194/acp-24-4129-2024
- Observed in-plume gaseous elemental mercury depletion suggests significant mercury scavenging by volcanic aerosols A. Koenig et al. 10.1039/D3EA00063J
Latest update: 20 Nov 2024
Short summary
The tropical Indian Ocean (IO) is expected to be a significant source of water-soluble organic carbon (WSOC), which is relevant to cloud formation. Our study showed that marine secondary organic formation dominantly contributed to the aerosol WSOC mass at the high-altitude observatory in the southwest IO in the wet season in both marine boundary layer and free troposphere (FT). This suggests that the effect of marine secondary sources is important up to FT, a process missing in climate models.
The tropical Indian Ocean (IO) is expected to be a significant source of water-soluble organic...
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