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Cited by 328

The DOI matches its Crossref record; 29 of the 29 references it cites were found in a registry or an index.

Global airborne sampling reveals a previously unobserved dimethyl sulfide oxidation mechanism in the marine atmosphere

Open access
Veres, Patrick R., Neuman, J. Andrew, Bertram, Timothy H., Assaf, Emmanuel, Wolfe, Glenn M., Williamson, Christina J., Weinzierl, Bernadett, Tilmes, Simone, Thompson, Chelsea R., Thames, Alexander B., Schroder, Jason C., Saiz-Lopez, Alfonso, Rollins, Andrew W., Roberts, James M., Price, Derek, Peischl, Jeff, Nault, Benjamin A., Møller, Kristian H., Miller, David O., Meinardi, Simone, Li, Qinyi, Lamarque, Jean-François, Kupc, Agnieszka, Kjaergaard, Henrik G., Kinnison, Douglas, Jimenez, Jose L., Jernigan, Christopher M., Hornbrook, Rebecca S., Hills, Alan, Dollner, Maximilian, Day, Douglas A., Cuevas, Carlos A., Campuzano-Jost, Pedro, Burkholder, James, Bui, T. Paul, Brune, William H., Brown, Steven S., Brock, Charles A., Bourgeois, Ilann, Blake, Donald R., Apel, Eric C., Ryerson, Thomas B.·2020·Proceedings of the National Academy of Sciences

Abstract

Dimethyl sulfide (DMS), emitted from the oceans, is the most abundant biological source of sulfur to the marine atmosphere. Atmospheric DMS is oxidized to condensable products that form secondary aerosols that affect Earth’s radiative balance by scattering solar radiation and serving as cloud condensation nuclei. We report the atmospheric discovery of a previously unquantified DMS oxidation product, hydroperoxymethyl thioformate (HPMTF, HOOCH 2 SCHO), identified through global-scale airborne observations that demonstrate it to be a major reservoir of marine sulfur. Observationally constrained model results show that more than 30% of oceanic DMS emitted to the atmosphere forms HPMTF. Coincident particle measurements suggest a strong link between HPMTF concentration and new particle formation and growth. Analyses of these observations show that HPMTF chemistry must be included in atmospheric models to improve representation of key linkages between the biogeochemistry of the ocean, marine aerosol formation and growth, and their combined effects on climate.

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Authors
Veres, P. R., Neuman, J. A., Bertram, T. H., Assaf, E., Wolfe, G. M., Williamson, C. J., Weinzierl, B., Tilmes, S., Thompson, C. R., Thames, A. B., Schroder, J. C., Saiz-Lopez, A., Rollins, A. W., Roberts, J. M., Price, D., Peischl, J., Nault, B. A., Møller, K. H., Miller, D. O., Meinardi, S., Li, Q., Lamarque, J.-F., Kupc, A., Kjaergaard, H. G., Kinnison, D., Jimenez, J. L., Jernigan, C. M., Hornbrook, R. S., Hills, A., Dollner, M., Day, D. A., Cuevas, C. A., Campuzano-Jost, P., Burkholder, J., Bui, T. P., Brune, W. H., Brown, S. S., Brock, C. A., Bourgeois, I., Blake, D. R., Apel, E. C., & Ryerson, T. B.
Venue
Proceedings of the National Academy of Sciences
Published
2020-02-18
Volume
117
Issue
9
Pages
4505-4510
ISSN
  • 0027-8424 (ISSN-L)
  • 1091-6490
OpenAlex
W3007487957
Cited by
328
References
29
FWCI
17.30
Type
journal article
Language
en
Open access
bronze

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CoChat. (2026). Citation check: Global airborne sampling reveals a previously unobserved dimethyl sulfide oxidation mechanism in the marine atmosphere. https://app.cochat.ai/papers/10.1073/pnas.1919344117
The paper
Veres, P. R., Neuman, J. A., Bertram, T. H., Assaf, E., Wolfe, G. M., Williamson, C. J., Weinzierl, B., Tilmes, S., Thompson, C. R., Thames, A. B., Schroder, J. C., Saiz-Lopez, A., Rollins, A. W., Roberts, J. M., Price, D., Peischl, J., Nault, B. A., Møller, K. H., Miller, D. O., . . . Ryerson, T. B. (2020). Global airborne sampling reveals a previously unobserved dimethyl sulfide oxidation mechanism in the marine atmosphere. Proceedings of the National Academy of Sciences. https://doi.org/10.1073/pnas.1919344117

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

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