<p><strong>Abstract.</strong> Ammonium-containing aerosols are a major component of winter time air pollution in many densely populated regions around the world. Especially in mountain basins, the formation of persistent cold air pool (PCAP) periods can enhance particulate matter with diameters less than 2.5&#8201;&#956;m (PM<sub>2.5</sub>) to levels above air quality standards. Under these conditions, PM<sub>2.5</sub> in the Great Salt Lake Region of northern Utah has been shown to be primarily composed of ammonium nitrate, however, its formation processes and sources of its precursors are not fully understood. Hence, it is key to understand the emission sources of its gas-phase precursor, ammonia (NH<sub>3</sub>). To investigate the formation of ammonium nitrate, a suite of trace gases and aerosol composition were sampled from the NOAA Twin Otter aircraft during the Utah Winter Fine Particulate Study (UWFPS) in January and February 2017. NH<sub>3</sub> was measured using a Quantum Cascade Tunable Infrared Laser Differential Absorption Spectrometer (QC-TILDAS), while aerosol composition, including particulate ammonium (pNH<sub>4</sub>), was measured with an aerosol mass spectrometer (AMS). The origin of the sampled air masses was investigated using the Stochastic Time-Inverted Lagrangian Transport (STILT) model and combined with an NH<sub>3</sub> emission inventory to obtain model-predicted NH<sub>x</sub> (=&#8201;NH<sub>3</sub>&#8201;+&#8201;pNH<sub>4</sub>) enhancements. Comparison of these NH<sub>x</sub> enhancements with measured NH<sub>x</sub> from the Twin Otter shows that modelled values are a factor of 1.6 to 4.4 lower for the three major valleys in the region. Among these, the underestimation is largest for Cache Valley, an area with intensive agricultural activities. We find that one explanation for the underestimation of wintertime emissions may be the seasonality factors applied to NH<sub>3</sub> emissions from livestock. An investigation of inter-valley exchange revealed that transport of NH<sub>3</sub> between major valleys was limited and PM<sub>2.5</sub> in Salt Lake Valley (the most densely populated area in Utah) was not significantly impacted by NH<sub>3</sub> from the agricultural areas in Cache Valley. We found that in Salt Lake Valley around two thirds of NH<sub>x</sub> originated within the valley, while about 30&#8201;% originated from mobile source and 60&#8201;% from area source emissions in the region. For Cache Valley, a large fraction of NO<sub>x</sub> potentially leading to PM<sub>2.5</sub> formation may not be locally emitted but mixed in from other counties.</p>