Articles | Volume 14, issue 22
https://doi.org/10.5194/acp-14-12513-2014
https://doi.org/10.5194/acp-14-12513-2014
Research article
 | 
27 Nov 2014
Research article |  | 27 Nov 2014

Competition between water uptake and ice nucleation by glassy organic aerosol particles

T. Berkemeier, M. Shiraiwa, U. Pöschl, and T. Koop

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
AR by Thomas Berkemeier on behalf of the Authors (09 Oct 2014)  Author's response    Manuscript
ED: Publish subject to technical corrections (24 Oct 2014) by David Topping
AR by Thomas Berkemeier on behalf of the Authors (28 Oct 2014)  Author's response    Manuscript
Download
Short summary
Glassy organic particles can serve as ice nuclei at low temperatures. We provide a rationale for these findings using a numerical aerosol diffusion model that describes particle phase state and its kinetics during simulated atmospheric updrafts dependent upon composition, size, updraft velocity, temperature and humidity. Our simulations suggest that aerosols from anthropogenic aromatic organics can be particularly relevant for ice cloud formation.
Altmetrics
Final-revised paper
Preprint