Articles | Volume 16, issue 21
Atmos. Chem. Phys., 16, 13837–13851, 2016

Special issue: Uintah Basin Winter Ozone Studies (ACP/AMT inter-journal SI)

Atmos. Chem. Phys., 16, 13837–13851, 2016

Research article 09 Nov 2016

Research article | 09 Nov 2016

The magnitude of the snow-sourced reactive nitrogen flux to the boundary layer in the Uintah Basin, Utah, USA

Maria Zatko et al.


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 Judy McMillan on behalf of the Authors (12 Aug 2016)  Author's response    Manuscript
ED: Reconsider after major revisions (11 Sep 2016) by Paul B. Shepson
ED: Referee Nomination & Report Request started (15 Sep 2016) by Paul B. Shepson
RR by Anonymous Referee #2 (30 Sep 2016)
ED: Publish as is (01 Oct 2016) by Paul B. Shepson
Short summary
This manuscript presents chemical and optical observations collected in the air and snow during UBWOS2014 in eastern Utah. These observations are used to calculate fluxes of reactive nitrogen associated with snow nitrate photolysis. Snow-sourced reactive nitrogen fluxes are compared to reactive nitrogen emission inventories to find that snow-sourced reactive nitrogen is a minor contributor to the reactive nitrogen budget, and thus wintertime ground-level ozone formation, in the Uintah Basin.
Final-revised paper