Articles | Volume 18, issue 20
Atmos. Chem. Phys., 18, 14939–14948, 2018
Atmos. Chem. Phys., 18, 14939–14948, 2018

Research article 17 Oct 2018

Research article | 17 Oct 2018

A thermodynamic description for the hygroscopic growth of atmospheric aerosol particles

Dimitri Castarède and Erik S. Thomson


Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Erik Thomson on behalf of the Authors (26 Sep 2018)  Author's response    Manuscript
ED: Publish as is (08 Oct 2018) by Ashu Dastoor
Short summary
We present a new description for the continuous transition of soluble atmospheric particulate from dry to completely dissolved particles. The theoretical development is motivated by observations that suggest particle surfaces begin to dissolve even at very low relative humidities. The results extend the understanding of the potential phase behavior of atmospheric particles with a wide range of implications.
Final-revised paper