Nitrogen Oxides Emissions, Chemistry, Deposition, and Export Over the Northeast United States During the WINTER Aircraft Campaign
Autor: | T. Sparks, Douglas A. Day, Thomas F. Hanisco, Viral Shah, Joel A. Thornton, H. S. Kenagy, Jason C. Schroder, Jose L. Jimenez, Andrew J. Weinheimer, Teresa Campos, Ben H. Lee, Denise D. Montzka, P. J. Wooldridge, Amy P. Sullivan, Erin E. McDuffie, C. J. Ebben, Dorothy L. Fibiger, Felipe D. Lopez-Hilfiker, Patrick R. Veres, Lyatt Jaeglé, Rodney J. Weber, Steven S. Brown, Glenn M. Wolfe, Hongyu Guo, Joshua P. DiGangi, Ronald C. Cohen, Pedro Campuzano-Jost |
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Rok vydání: | 2018 |
Předmět: |
Atmospheric Science
Dinitrogen pentoxide 010504 meteorology & atmospheric sciences Chemical transport model Reactive nitrogen 010501 environmental sciences Particulates 01 natural sciences Troposphere chemistry.chemical_compound Geophysics Deposition (aerosol physics) Nitrate chemistry Space and Planetary Science Environmental chemistry Earth and Planetary Sciences (miscellaneous) NOx 0105 earth and related environmental sciences |
Zdroj: | Journal of Geophysical Research: Atmospheres. 123 |
ISSN: | 2169-8996 2169-897X |
DOI: | 10.1029/2018jd029133 |
Popis: | We examine the distribution and fate of nitrogen oxides (NOx) in the lower 36 troposphere over the Northeast United States (NE US) using aircraft observations from the 37 Wintertime INvestigation of Transport, Emissions, and Reactivity (WINTER) campaign in February-March 2015, as well as the GEOS-Chem chemical transport model and concurrent ground-based observations. We find that the National Emission Inventory (NEI) from the US Environmental Protection Agency (EPA) is consistent with WINTER observations of total reactive nitrogen (TNOy) to within 10% on average, in contrast to the significant overestimate reported in past studies under warmer conditions. Updates to the dry deposition scheme and dinitrogen pentoxide (N2O5) reactive uptake probability, ɣ(N2O5), result in an improved simulation of gas-phase nitric acid (HNO3) and submicron particulate nitrate (pNO3⁻), reducing he longstanding factor of 2-3 overestimate in wintertime HNO3+pNO3⁻ to a 50% positive bias. We find a NOx lifetime against chemical loss and deposition of 22 hours in the lower troposphere over the NE US. Chemical loss of NOx is dominated by N2O5 hydrolysis (58% of loss) and reaction with OH (33%), while 7% of NOx leads to the production of organic nitrates. Wet and dry deposition account for 55% and 45% of TNOy deposition over land, respectively. We estimate that 42% of the NOx emitted is exported from the NE US boundary layer during winter, mostly in the form of HNO3+pNO3⁻ (40%) and NOx (38%). |
Databáze: | OpenAIRE |
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