Articles | Volume 19, issue 23
https://doi.org/10.5194/acp-19-14455-2019
© Author(s) 2019. 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-19-14455-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Dimethyl sulfide and its role in aerosol formation and growth in the Arctic summer – a modelling study
Environment and Climate Change Canada, Toronto, Ontario, Canada
Wanmin Gong
Environment and Climate Change Canada, Toronto, Ontario, Canada
Martí Galí
Québec-Océan, Department of Biology, Université Laval,
Québec, Canada
Ann-Lise Norman
Department of Physics and Astronomy, University of Calgary, Calgary, Canada
Stephen R. Beagley
Environment and Climate Change Canada, Toronto, Ontario, Canada
Ayodeji Akingunola
Environment and Climate Change Canada, Toronto, Ontario, Canada
Qiong Zheng
Environment and Climate Change Canada, Toronto, Ontario, Canada
Alexandru Lupu
Environment and Climate Change Canada, Toronto, Ontario, Canada
Martine Lizotte
Québec-Océan, Department of Biology, Université Laval,
Québec, Canada
Maurice Levasseur
Québec-Océan, Department of Biology, Université Laval,
Québec, Canada
W. Richard Leaitch
Environment and Climate Change Canada, Toronto, Ontario, Canada
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Cited
20 citations as recorded by crossref.
- Sea Salt Aerosol Identification Based on Multispectral Optical Properties and Its Impact on Radiative Forcing over the Ocean D. Atmoko & T. Lin 10.3390/rs14133188
- Importance of Atmospheric Transport on Methanesulfonic Acid (MSA) Concentrations in the Arctic Ocean During Summer Under Global Warming B. Jiang et al. 10.1029/2022JD037271
- Rapid growth of Aitken-mode particles during Arctic summer by fog chemical processing and its implication S. Kecorius et al. 10.1093/pnasnexus/pgad124
- Microorganisms associated with Sporobolus anglicus, an invasive dimethylsulfoniopropionate producing salt marsh plant, are an unrecognized sink for dimethylsulfide E. Kröber et al. 10.3389/fmicb.2022.950460
- Tethered balloon measurements reveal enhanced aerosol occurrence aloft interacting with Arctic low-level clouds C. Pilz et al. 10.1525/elementa.2023.00120
- Secondary aerosol formation from dimethyl sulfide – improved mechanistic understanding based on smog chamber experiments and modelling R. Wollesen de Jonge et al. 10.5194/acp-21-9955-2021
- The occurrence of lower-than-expected bulk NCCN values over the marginal seas of China - Implications for competitive activation of marine aerosols J. Gong et al. 10.1016/j.scitotenv.2022.159938
- The annual cycle and sources of relevant aerosol precursor vapors in the central Arctic during the MOSAiC expedition M. Boyer et al. 10.5194/acp-24-12595-2024
- Ultrahigh resolution spectroscopy for dimethyl sulfide at the ν1- and ν8-bands by a distributed feedback interband cascade laser Z. Wang et al. 10.1016/j.jqsrt.2020.106930
- Seasonal dynamics of airborne biomolecules influence the size distribution of Arctic aerosols E. Jang et al. 10.1016/j.ese.2024.100458
- Large seasonal and interannual variations of biogenic sulfur compounds in the Arctic atmosphere (Svalbard; 78.9° N, 11.9° E) S. Jang et al. 10.5194/acp-21-9761-2021
- Long‐Term Trends for Marine Sulfur Aerosol in the Alaskan Arctic and Relationships With Temperature C. Moffett et al. 10.1029/2020JD033225
- Simulated perturbation in the sea-to-air flux of dimethylsulfide and the impact on polar climate B. Qu et al. 10.1007/s00343-020-0007-8
- Solid organic-coated ammonium sulfate particles at high relative humidity in the summertime Arctic atmosphere R. Kirpes et al. 10.1073/pnas.2104496119
- Vertical Chlorophyll and Dimethylsulfide Profile Simulations in Southern Greenland Sea B. Qu & W. Sun 10.1007/s11802-022-5298-2
- Modeling Aerosol Effects on Liquid Clouds in the Summertime Arctic R. Ghahreman et al. 10.1029/2021JD034962
- Pan-Arctic methanesulfonic acid aerosol: source regions, atmospheric drivers, and future projections J. Pernov et al. 10.1038/s41612-024-00712-3
- Factors controlling marine aerosol size distributions and their climate effects over the northwest Atlantic Ocean region B. Croft et al. 10.5194/acp-21-1889-2021
- Pollution drives multidecadal decline in subarctic methanesulfonic acid J. Chalif et al. 10.1038/s41561-024-01543-w
- DMS emissions from the Arctic marginal ice zone M. Galí et al. 10.1525/elementa.2020.00113
20 citations as recorded by crossref.
- Sea Salt Aerosol Identification Based on Multispectral Optical Properties and Its Impact on Radiative Forcing over the Ocean D. Atmoko & T. Lin 10.3390/rs14133188
- Importance of Atmospheric Transport on Methanesulfonic Acid (MSA) Concentrations in the Arctic Ocean During Summer Under Global Warming B. Jiang et al. 10.1029/2022JD037271
- Rapid growth of Aitken-mode particles during Arctic summer by fog chemical processing and its implication S. Kecorius et al. 10.1093/pnasnexus/pgad124
- Microorganisms associated with Sporobolus anglicus, an invasive dimethylsulfoniopropionate producing salt marsh plant, are an unrecognized sink for dimethylsulfide E. Kröber et al. 10.3389/fmicb.2022.950460
- Tethered balloon measurements reveal enhanced aerosol occurrence aloft interacting with Arctic low-level clouds C. Pilz et al. 10.1525/elementa.2023.00120
- Secondary aerosol formation from dimethyl sulfide – improved mechanistic understanding based on smog chamber experiments and modelling R. Wollesen de Jonge et al. 10.5194/acp-21-9955-2021
- The occurrence of lower-than-expected bulk NCCN values over the marginal seas of China - Implications for competitive activation of marine aerosols J. Gong et al. 10.1016/j.scitotenv.2022.159938
- The annual cycle and sources of relevant aerosol precursor vapors in the central Arctic during the MOSAiC expedition M. Boyer et al. 10.5194/acp-24-12595-2024
- Ultrahigh resolution spectroscopy for dimethyl sulfide at the ν1- and ν8-bands by a distributed feedback interband cascade laser Z. Wang et al. 10.1016/j.jqsrt.2020.106930
- Seasonal dynamics of airborne biomolecules influence the size distribution of Arctic aerosols E. Jang et al. 10.1016/j.ese.2024.100458
- Large seasonal and interannual variations of biogenic sulfur compounds in the Arctic atmosphere (Svalbard; 78.9° N, 11.9° E) S. Jang et al. 10.5194/acp-21-9761-2021
- Long‐Term Trends for Marine Sulfur Aerosol in the Alaskan Arctic and Relationships With Temperature C. Moffett et al. 10.1029/2020JD033225
- Simulated perturbation in the sea-to-air flux of dimethylsulfide and the impact on polar climate B. Qu et al. 10.1007/s00343-020-0007-8
- Solid organic-coated ammonium sulfate particles at high relative humidity in the summertime Arctic atmosphere R. Kirpes et al. 10.1073/pnas.2104496119
- Vertical Chlorophyll and Dimethylsulfide Profile Simulations in Southern Greenland Sea B. Qu & W. Sun 10.1007/s11802-022-5298-2
- Modeling Aerosol Effects on Liquid Clouds in the Summertime Arctic R. Ghahreman et al. 10.1029/2021JD034962
- Pan-Arctic methanesulfonic acid aerosol: source regions, atmospheric drivers, and future projections J. Pernov et al. 10.1038/s41612-024-00712-3
- Factors controlling marine aerosol size distributions and their climate effects over the northwest Atlantic Ocean region B. Croft et al. 10.5194/acp-21-1889-2021
- Pollution drives multidecadal decline in subarctic methanesulfonic acid J. Chalif et al. 10.1038/s41561-024-01543-w
- DMS emissions from the Arctic marginal ice zone M. Galí et al. 10.1525/elementa.2020.00113
Latest update: 06 Dec 2024
Short summary
Atmospheric DMS(g) is a climatically important compound and the main source of biogenic sulfate in the Arctic. Its abundance in the Arctic increases during summer due to greater ice-free sea surface and higher biological activity. In this study, we implemented DMS(g) in a regional air quality forecast model configured for the Arctic. The study showed a significant impact from DMS(g) on sulfate aerosols, particularly in the 50–100 nm size range, in the Arctic marine boundary layer during summer.
Atmospheric DMS(g) is a climatically important compound and the main source of biogenic sulfate...
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