When Dry Air Is Too Humid-Reference-Cited by-同舟云学术

When Dry Air Is Too Humid

Published:2006-12 Issue:5804 Volume:314 Page:1399-1402
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Peter Thomas,Marcolli Claudia,Spichtinger Peter,Corti Thierry¹,Baker Marcia B.²,Koop Thomas³

Affiliation:

1. Th. Peter, C. Marcolli, P. Spichtinger, and T. Corti are at the Institute for Atmospheric and Climate Science, Eidgenössische Technische Hochschule (ETH) Zürich, 8092 Zürich, Switzerland.

2. M. B. Baker is in the Department of Atmospheric Sciences, University of Washington, Seattle, WA 98195, USA.

3. T. Koop is in the Department of Chemistry, Bielefeld University, D-33615 Bielefeld, Germany.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference19 articles.

1. Jensen E. J., et al., Atmos. Chem. Phys.5, 851 (2005).

2. Gao R. S., et al., Science303, (2004)[516].

3. Lee S. H., et al., J. Geophys. Res.109, D20209 (2004)10.1029/2004JD005033.

4. Koop T., et al., Nature406, 611 (2000).

5. In a cooling event when aerosol particles are exposed to a supersaturation of 60% the characteristic time for ice nucleation is ∼1 min. This drops to <1 s for the atmospheric measurements described in (1).

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