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A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and...

A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_759316586

A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model

About this item

Full title

A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model

Publisher

Boston, MA: American Meteorological Society

Journal title

Journal of the atmospheric sciences, 2010-08, Vol.67 (8), p.2483-2503

Language

English

Formats

Publication information

Publisher

Boston, MA: American Meteorological Society

More information

Scope and Contents

Contents

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...

Alternative Titles

Full title

A Classical-Theory-Based Parameterization of Heterogeneous Ice Nucleation by Mineral Dust, Soot, and Biological Particles in a Global Climate Model

Authors, Artists and Contributors

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_759316586

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_759316586

Other Identifiers

ISSN

0022-4928

E-ISSN

1520-0469

DOI

10.1175/2010JAS3425.1

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