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On the effectiveness of nitrogen oxide reductions as a control over ammonium nitrate aerosol.

Authors :
Pusede, S. E.
Duffey, K. C.
Shusterman, A. A.
Saleh, A.
Laughner, J. L.
Wooldridge, P. J.
Zhang, Q.
Parworth, C. L.
Kim, H.
Capps, S. L.
Valin, L. C.
Cappa, C. D.
Fried, A.
Walega, J.
Nowak, J. B.
Hoff, R. M.
Berkoff, T. A.
Beyersdorf, A. J.
Olson, J.
Crawford, J. H.
Source :
Atmospheric Chemistry & Physics Discussions; 2015, Vol. 15 Issue 19, p27087-27136, 50p
Publication Year :
2015

Abstract

Nitrogen oxides (NO<subscript>x</subscript>) have fallen steadily across the US over the last fifteen years. At the same time, due to patterns diesel truck activities, NO<subscript>x</subscript> concentrations decrease on weekends relative to weekdays, largely without co-occurring changes in other gas-phase emissions. These trends taken together provide two independent constraints on the role of NO<subscript>x</subscript> in the nonlinear chemistry of atmospheric oxidation. In this context, we interpret interannual trends in wintertime ammonium nitrate (NH<subscript>4</subscript>NO<subscript>3</subscript>) in the San Joaquin Valley of California, a location with the worst aerosol pollution in the US and where a large portion of aerosol mass is NH<subscript>4</subscript>NO<subscript>3</subscript>. Here, we show that NO<subscript>x</subscript> reductions have simultaneously decreased nighttime and increased daytime NH<subscript>4</subscript>NO<subscript>3</subscript> production over the last decade. We find a substantial decrease in NH<subscript>4</subscript>NO<subscript>3</subscript> since 2000 and conclude that this decrease is due to reduced nitrate radical-initiated production at night in residual layers that are decoupled from fresh emissions at the surface. Further reductions in NO<subscript>x</subscript> are imminent in California, and nationwide, and we make a quantitative prediction of the response of NH<subscript>4</subscript>NO<subscript>3</subscript>. We show that the combination of rapid chemical production and efficient NH<subscript>4</subscript>NO<subscript>3</subscript> loss via deposition of gas-phase nitric acid implies high aerosol days in cities in the San Joaquin Valley air basin are responsive to local changes in NO<subscript>x</subscript> within those individual cities. Our calculations indicate that large decreases in NO<subscript>x</subscript> in the future will not only lower wintertime NH<subscript>4</subscript>NO<subscript>3</subscript> concentrations, they will also cause a transition in the dominant NH<subscript>4</subscript>NO<subscript>3</subscript> source from nighttime to daytime chemistry. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
16807367
Volume :
15
Issue :
19
Database :
Complementary Index
Journal :
Atmospheric Chemistry & Physics Discussions
Publication Type :
Academic Journal
Accession number :
110501749
Full Text :
https://doi.org/10.5194/acpd-15-27087-2015