Can chemical effects on cloud droplet number rival the first indirect effect?

Author:

Nenes Athanasios1,Charlson Robert J.2,Facchini M. Cristina3,Kulmala Markku4,Laaksonen Ari5,Seinfeld John H.1

Affiliation:

1. Department of Chemical Engineering; California Institute of Technology; USA

2. Department of Atmospheric Sciences and Chemistry; University of Washington; USA

3. Istituto di Scienze dell'Atmosfera e del Clima - CNR; Italy

4. Department of Physical Sciences; University of Helsinki; Finland

5. Department of Applied Physics; University of Kuopio; Finland

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference16 articles.

1. Predicting particle critical supersaturation from hygroscopic growth measurements in the humidified TDMA, Part I: Theory and sensitivity studies;Brechtel;J. Aerosol Sci.,2000

2. Predicting particle critical supersaturation from hygroscopic growth measurements in the humidified TDMA, Part II: Laboratory and ambient studies;Brechtel;J. Aerosol Sci.,2000

3. Atmospheric science - reshaping the theory of cloud formation;Charlson;Science,2001

4. CCN measurements during ACE-2 and their relationship to cloud microphysical properties;Chuang;Tellus B,2000

5. Cloud albedo enhancement by surface-active organic solutes in growing droplets;Facchini;Nature,1999

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