Articles | Volume 21, issue 10
https://doi.org/10.5194/acp-21-8111-2021
https://doi.org/10.5194/acp-21-8111-2021
Research article
 | 
27 May 2021
Research article |  | 27 May 2021

The role of coarse aerosol particles as a sink of HNO3 in wintertime pollution events in the Salt Lake Valley

Amy Hrdina, Jennifer G. Murphy, Anna Gannet Hallar, John C. Lin, Alexander Moravek, Ryan Bares, Ross C. Petersen, Alessandro Franchin, Ann M. Middlebrook, Lexie Goldberger, Ben H. Lee, Munkh Baasandorj, and Steven S. Brown

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 Amy Hdrina on behalf of the Authors (15 Feb 2021)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (26 Feb 2021) by Ryan Sullivan
RR by Anonymous Referee #1 (10 Mar 2021)
RR by Anonymous Referee #2 (13 Mar 2021)
ED: Publish subject to minor revisions (review by editor) (13 Mar 2021) by Ryan Sullivan
AR by Amy Hdrina on behalf of the Authors (16 Mar 2021)  Manuscript 
ED: Publish as is (23 Mar 2021) by Ryan Sullivan
AR by Amy Hdrina on behalf of the Authors (23 Apr 2021)  Manuscript 
Download
Short summary
Wintertime air pollution in the Salt Lake Valley is primarily composed of ammonium nitrate, which is formed when gas-phase ammonia and nitric acid react. The major point in this work is that the chemical composition of snow tells a very different story to what we measured in the atmosphere. With the dust–sea salt cations observed in PM2.5 and particle sizing data, we can estimate how much nitric acid may be lost to dust–sea salt that is not accounted for and how much more PM2.5 this could form.
Altmetrics
Final-revised paper
Preprint