The DOI matches its Crossref record; 98 of the 98 references it cites were found in a registry or an index.
A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model
Abstract
An ice nucleation parameterization based on classical nucleation theory, with aerosol-specific parameters derived from experiments, has been implemented into a global climate model—the Community Atmosphere Model (CAM)-Oslo. The parameterization treats immersion, contact, and deposition nucleation by mineral dust, soot, bacteria, fungal spores, and pollen in mixed-phase clouds at temperatures between 0° and −38°C. Immersion freezing is considered for insoluble particles that are activated to cloud droplets, and deposition and contact nucleation are only allowed for uncoated, unactivated aerosols. Immersion freezing by mineral dust is found to be the dominant ice formation process, followed by immersion and contact freezing by soot. The simulated biological aerosol contribution to global atmospheric ice formation is marginal, even with high estimates of their ice nucleation activity, because the number concentration of ice nucleation active biological particles in the atmosphere is low compared to other ice nucleating aerosols. Because of the dominance of mineral dust, the simulated ice nuclei concentrations at temperatures below −20°C are found to correlate with coarse-mode aerosol particle concentrations. The ice nuclei (IN) concentrations in the model agree well overall with in situ continuous flow diffusion chamber measurements. At individual locations, the model exhibits a stronger temperature dependence on IN concentrations than what is observed. The simulated IN composition (77% mineral dust, 23% soot, and 10−5% biological particles) lies in the range of observed ice nuclei and ice crystal residue compositions.
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Cites
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Cited by
Primary biological aerosol particles in the atmosphere: a review
Després, V. R., Huffman, J. A., Burrows, S. M., Hoose, C., Safatov, A. S., Buryak, G., Fröhlich-Nowoisky, J., Elbert, W., Andreae, M. O., Pöschl, U., et al. (2012) · Tellus B: Chemical and Physical Meteorology · doi:10.3402/tellusb.v64i0.15598 · Cited by 1,500
Self-citationHoose, C., & Möhler, O. (2012) · Atmospheric Chemistry and Physics · doi:10.5194/acp-12-9817-2012 · Cited by 1,227
Self-citationBentsen, M., Bethke, I., Debernard, J. B., Iversen, T., Kirkevåg, A., Seland, Ø., Drange, H., Roelandt, C., Seierstad, I. A., Hoose, C., et al. (2013) · Geoscientific Model Development · doi:10.5194/gmd-6-687-2013 · Cited by 1,084
Self-citationAerosol Mixing State: Measurements, Modeling, and Impacts
Riemer, N., Ault, A. P., West, M., Craig, R. L., & Curtis, J. H. (2019) · Reviews of Geophysics · doi:10.1029/2018rg000615 · Cited by 459
A Particle-Surface-Area-Based Parameterization of Immersion Freezing on Desert Dust Particles
Niemand, M., Möhler, O., Vogel, B., Vogel, H., Hoose, C., Connolly, P., Klein, H., Bingemer, H., DeMott, P., Skrotzki, J., et al. (2012) · Journal of the Atmospheric Sciences · doi:10.1175/jas-d-11-0249.1 · Cited by 451
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Metadata
- Authors
- Hoose, C., Kristjánsson, J. E., Chen, J.-P., & Hazra, A.
- Venue
- Journal of the Atmospheric Sciences
- Publisher
- American Meteorological Society
- Published
- 2010-08-01
- Volume
- 67
- Issue
- 8
- Pages
- 2483-2503
- ISSN
- 0022-4928 (ISSN-L)
- 1520-0469
- OpenAlex
- W2139774107
- Cited by
- 432
- References
- 98
- FWCI
- 17.15
- Type
- journal article
- Language
- en
- Open access
- closed
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- Hoose, C., Kristjánsson, J. E., Chen, J.-P., & Hazra, A. (2010). A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model. Journal of the Atmospheric Sciences. https://doi.org/10.1175/2010jas3425.1
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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.
