Please use this identifier to cite or link to this item: https://hdl.handle.net/10356/100724
Title: Atmospheric ammonia and particulate inorganic nitrogen over the United States
Authors: Heald, C. L.
J. L. Collett Jr.
Lee, T.
Benedict, K. B.
Schwandner, F. M.
Li, Y.
Clarisse, L.
Hurtmans, D. R.
Van Damme, M.
Clerbaux, C.
Coheur, P.-F.
Philip, S.
Martin, R. V.
Pye, H. O. T.
Keywords: DRNTU::Engineering::Environmental engineering
Issue Date: 2012
Source: Heald, C. L., J. L. Collett Jr., Lee, T., Benedict, K. B., Schwandner, F. M., Li, Y., et al. (2012). Atmospheric ammonia and particulate inorganic nitrogen over the United States. Atmospheric chemistry and physics, 12(21), 10295-10312.
Series/Report no.: Atmospheric chemistry and physics
Abstract: We use in situ observations from the Interagency Monitoring of PROtected Visual Environments (IMPROVE) network, the Midwest Ammonia Monitoring Project, 11 surface site campaigns as well as Infrared Atmospheric Sounding Interferometer (IASI) satellite measurements with the GEOS-Chem model to investigate inorganic aerosol loading and atmospheric ammonia concentrations over the United States. IASI observations suggest that current ammonia emissions are underestimated in California and in the springtime in the Midwest. In California this underestimate likely drives the underestimate in nitrate formation in the GEOS-Chem model. However in the remaining continental United States we find that the nitrate simulation is biased high (normalized mean bias > = 1.0) year-round, except in Spring (due to the underestimate in ammonia in this season). None of the uncertainties in precursor emissions, the uptake efficiency of N2O5 on aerosols, OH concentrations, the reaction rate for the formation of nitric acid, or the dry deposition velocity of nitric acid are able to explain this bias. We find that reducing nitric acid concentrations to 75% of their simulated values corrects the bias in nitrate (as well as ammonium) in the US. However the mechanism for this potential reduction is unclear and may be a combination of errors in chemistry, deposition and sub-grid near-surface gradients. This "updated" simulation reproduces PM and ammonia loading and captures the strong seasonal and spatial gradients in gas-particle partitioning across the United States. We estimate that nitrogen makes up 15−35% of inorganic fine PM mass over the US, and that this fraction is likely to increase in the coming decade, both with decreases in sulfur emissions and increases in ammonia emissions.
URI: https://hdl.handle.net/10356/100724
http://hdl.handle.net/10220/18634
ISSN: 1680-7324
DOI: 10.5194/acp-12-10295-2012
Rights: © 2012 Author(s). This paper was published in Atmospheric Chemistry and Physics and is made available as an electronic reprint (preprint) with permission of Author(s). The paper can be found at the following official DOI: http://dx.doi.org/10.5194/acp-12-10295-2012.  One print or electronic copy may be made for personal use only. Systematic or multiple reproduction, distribution to multiple locations via electronic or other means, duplication of any material in this paper for a fee or for commercial purposes, or modification of the content of the paper is prohibited and is subject to penalties under law.
Fulltext Permission: open
Fulltext Availability: With Fulltext
Appears in Collections:EOS Journal Articles

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