Articles | Volume 18, issue 21
https://doi.org/10.5194/acp-18-15903-2018
https://doi.org/10.5194/acp-18-15903-2018
Research article
 | 
07 Nov 2018
Research article |  | 07 Nov 2018

The influence of HCl on the evaporation rates of H2O over water ice in the range 188 to 210 K at small average concentrations

Christophe Delval and Michel J. Rossi

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 Michel J. Rossi on behalf of the Authors (10 Sep 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (12 Sep 2018) by Daniel Knopf
RR by Anonymous Referee #1 (02 Oct 2018)
ED: Publish subject to minor revisions (review by editor) (04 Oct 2018) by Daniel Knopf
AR by Michel J. Rossi on behalf of the Authors (09 Oct 2018)  Author's response
ED: Publish as is (16 Oct 2018) by Daniel Knopf
Download
Short summary
Evaporation rates of H2O and HCl were observed from a thin film condensate at low temperature at an average HCl mole fraction of 10(−5)–10(−3) in order to probe the evaporative lifetime of ice particles of the upper troposphere and lower stratosphere. The results show a decrease in the H2O evaporation rate with increasing mass loss of the condensate under conditions where the saturation vapor pressure corresponded to pure ice. This supports gas–surface reactions of HCl-doped ice particles.
Altmetrics
Final-revised paper
Preprint