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The Uintah Basin in northeastern Utah, a region of intense oil and gas extraction, experienced ozone (O₃) concentrations above levels harmful to human health for multiple days during the winters of 2009–2010 and 2010–2011. These wintertime O₃ pollution episodes occur during cold, stable periods when the ground is snow-covered, and have been linked to emissions from the oil and gas extraction process. The Uintah Basin Winter Ozone Study (UBWOS) was a field intensive in early 2012, whose goal was to address current uncertainties in the chemical and physical processes that drive wintertime O₃ production in regions of oil and gas development. Although elevated O₃ concentrations were not observed during the winter of 2011–2012, the comprehensive set of observations tests our understanding of O₃ photochemistry in this unusual emissions environment. A box model, constrained to the observations and using the near-explicit Master Chemical Mechanism (MCM) v3.2 chemistry scheme, has been used to investigate the sensitivities of O₃ production during UBWOS 2012. Simulations identify the O₃ production photochemistry to be highly radical limited (with a radical production rate significantly smaller than the NO_x emission rate). Production of OH from O₃ photolysis (through reaction of O(¹D) with water vapor) contributed only 170 pptv day⁻¹, 8% of the total primary radical source on average (primary radicals being those produced from non-radical precursors). Other radical sources, including the photolysis of formaldehyde (HCHO, 52%), nitrous acid (HONO, 26%), and nitryl chloride (ClNO₂, 13%) were larger. O₃ production was also found to be highly sensitive to aromatic volatile organic compound (VOC) concentrations, due to radical amplification reactions in the oxidation scheme of these species. Radical production was shown to be small in comparison to the emissions of nitrogen oxides (NO_x), such that NO_x acted as the primary radical sink. Consequently, the system was highly VOC sensitive, despite the much larger mixing ratio of total non-methane hydrocarbons (230 ppbv (2080 ppbC), 6 week average) relative to NO_x (5.6 ppbv average). However, the importance of radical sources which are themselves derived from NO_x emissions and chemistry, such as ClNO₂ and HONO, make the response of the system to changes in NO_x emissions uncertain. Model simulations attempting to reproduce conditions expected during snow-covered cold-pool conditions show a significant increase in O₃ production, although calculated concentrations do not achieve the highest seen during the 2010–2011 O₃ pollution events in the Uintah Basin. These box model simulations provide useful insight into the chemistry controlling winter O₃ production in regions of oil and gas extraction

The Salt Lake Valley experiences severe fine particulate matter pollution episodes in winter during persistent cold-air pools (PCAPs). We employ measurements throughout an entire winter from different elevations to examine the chemical and dynamical processes driving these episodes. Whereas primary pollutants such as NO and CO were enhanced twofold during PCAPs, O concentrations were approximately threefold lower. Atmospheric composition varies strongly with altitude within a PCAP at night with lower NO and higher oxidants (O) and oxidized reactive nitrogen (NO) aloft. We present observations of NO during PCAPs that provide evidence for its role in cold-pool nitrate formation. Our observations suggest that nighttime and early morning chemistry in the upper levels of a PCAP plays an important role in aerosol nitrate formation. Subsequent daytime mixing enhances surface PM by dispersing the aerosol throughout the PCAP. As pollutants accumulate and deplete oxidants, nitrate chemistry becomes less active during the later stages of the pollution episodes. This leads to distinct stages of PM pollution episodes, starting with a period of PM buildup and followed by a period with plateauing concentrations. We discuss the implications of these findings for mitigation strategies.

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