The DOI matches its Crossref record; 58 of the 58 references it cites were found in a registry or an index.
Global distribution of particle phase state in atmospheric secondary organic aerosols
Open accessAbstract
Secondary organic aerosols (SOA) are a large source of uncertainty in our current understanding of climate change and air pollution. The phase state of SOA is important for quantifying their effects on climate and air quality, but its global distribution is poorly characterized. We developed a method to estimate glass transition temperatures based on the molar mass and molecular O:C ratio of SOA components, and we used the global chemistry climate model EMAC with the organic aerosol module ORACLE to predict the phase state of atmospheric SOA. For the planetary boundary layer, global simulations indicate that SOA are mostly liquid in tropical and polar air with high relative humidity, semi-solid in the mid-latitudes and solid over dry lands. We find that in the middle and upper troposphere SOA should be mostly in a glassy solid phase state. Thus, slow diffusion of water, oxidants and organic molecules could kinetically limit gas–particle interactions of SOA in the free and upper troposphere, promote ice nucleation and facilitate long-range transport of reactive and toxic organic pollutants embedded in SOA.
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Cites
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Evolution of Organic Aerosols in the Atmosphere
Jimenez, J. L., Canagaratna, M. R., Donahue, N. M., Prevot, A. S. H., Zhang, Q., Kroll, J. H., DeCarlo, P. F., Allan, J. D., Coe, H., Ng, N. L., et al. (2009) · Science · doi:10.1126/science.1180353 · Cited by 4,167
A single parameter representation of hygroscopic growth and cloud condensation nucleus activity
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A large source of low-volatility secondary organic aerosol
Ehn, M., Thornton, J. A., Kleist, E., Sipilä, M., Junninen, H., Pullinen, I., Springer, M., Rubach, F., Tillmann, R., Lee, B., et al. (2014) · Nature · doi:10.1038/nature13032 · Cited by 2,009
Coupled Partitioning, Dilution, and Chemical Aging of Semivolatile Organics
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Self-citationThe role of low-volatility organic compounds in initial particle growth in the atmosphere
Tröstl, J., Chuang, W. K., Gordon, H., Heinritzi, M., Yan, C., Molteni, U., Ahlm, L., Frege, C., Bianchi, F., Wagner, R., et al. (2016) · Nature · doi:10.1038/nature18271 · Cited by 850
An amorphous solid state of biogenic secondary organic aerosol particles
Virtanen, A., Joutsensaari, J., Koop, T., Kannosto, J., Yli-Pirilä, P., Leskinen, J., Mäkelä, J. M., Holopainen, J. K., Pöschl, U., Kulmala, M., et al. (2010) · Nature · doi:10.1038/nature09455 · Cited by 828
Self-citationKoop, T., Bookhold, J., Shiraiwa, M., & Pöschl, U. (2011) · Physical Chemistry Chemical Physics · doi:10.1039/c1cp22617g · Cited by 785
Self-citationKinetics, products, and mechanisms of secondary organic aerosol formation
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Cited by
Huang, W., Saathoff, H., Pajunoja, A., Shen, X., Naumann, K.-H., Wagner, R., Virtanen, A., Leisner, T., & Mohr, C. (2018) · Atmospheric Chemistry and Physics · doi:10.5194/acp-18-2883-2018 · Cited by 129
Metadata
- Authors
- Shiraiwa, M., Li, Y., Tsimpidi, A. P., Karydis, V. A., Berkemeier, T., Pandis, S. N., Lelieveld, J., Koop, T., & Pöschl, U.
- Venue
- Nature Communications
- Published
- 2017-04-21
- Volume
- 8
- Issue
- 1
- Pages
- 15002-15002
- ISSN
- 2041-1723 (ISSN-L)
- OpenAlex
- W2606664845
- Cited by
- 484
- References
- 58
- FWCI
- 22.85
- Type
- journal article
- Language
- en
- Open access
- gold
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- Shiraiwa, M., Li, Y., Tsimpidi, A. P., Karydis, V. A., Berkemeier, T., Pandis, S. N., Lelieveld, J., Koop, T., & Pöschl, U. (2017). Global distribution of particle phase state in atmospheric secondary organic aerosols. Nature Communications. https://doi.org/10.1038/ncomms15002
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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.
Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.