The chemical fractionation of atmospheric aerosol as a result of snow crystal formation and growth

Author:

Borys Randolph D.,Hindman Edward E.,DeMott Paul J.

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science,Environmental Chemistry

Reference45 articles.

1. BaumgardnerD., 1983, An analysis and comparison of five water droplet measuring instruments, J. Clim. Appl. Meteor. 22, 891?910.

2. BorysR. D., 1983a, The interaction of aerosol particles, cloud water and ice crystals and their relationship to precipitation scavenging in the Arctic, in H. R.Pruppacher, R. G.Semonin and W. G. N.Slinn (eds.) Precipitation Scavenging, Dry Deposition and Resuspension, Vol. 2, Elsevier, Amsterdam, pp. 1281?1288.

3. Atmos. Sci. Pap.;R. D. Borys,1983

4. Borys, R. D., Lowenthal, D. H., and Rahn, K. A., 1987, Contributions of smelters and other sources to pollution sulfate at a mountaintop site in northwestern Colorado, in Roger Pielke (ed.), Acid Deposition in Colorado ? A Potential or Current Problem; Local Versus Long-distance Transport Into the State, CIRA Workshop Compendium, 13?15 August 1986, pp. 167?174.

5. BorysR. D., HindmanE. E., and DeMottP. J., 1983, The significance of snow crystal and mountain surface riming to the removal of atmospheric trace-constituents from cold clouds, in H. R.Pruppacher, R. G.Semonin and W. G. N.Slinn, (eds.) Precipitation Scavenging, Dry Deposition and Resuspension, Vol. 1, Elsevier, Amsterdam, pp. 181?190.

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