<p><strong>Abstract.</strong> We present airborne measurements made in the Colorado Front Range aboard the NSF C-130 aircraft during the 2014 Front Range Air Pollution and Photochemistry &#201;xperiment (FRAPP&#201;) project. Data on trace gases, non-refractory sub-micron aerosol chemical constituents, and aerosol optical extinction (&#946;<sub>ext</sub>) at &#955;&#8201;=&#8201;632&#8201;nm in the presence and absence of a surface mesoscale circulation pattern, called the Denver Cyclone, were analyzed in three study regions of the Front Range: In-Flow, Northern Front Range (NFR), and Denver Metropolitan (DM). Pronounced increases in mass concentrations of organics, nitrate, and sulfate in NFR and DM were observed during the cyclone episodes (27&#8211;28 July) compared to the non-cyclonic days (26 July, 02&#8211;03 August). Organics (OA) dominated the mass concentrations on all evaluated days, with a 45&#8201;% increase in OA on cyclone days across all three regions while the increase during the cyclone episode was up to ~&#8201;80&#8201;% for DM, from 3.78&#8201;&#177;&#8201;1.55&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup> to 6.78&#8201;&#177;&#8201;1.78&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup>, where sm<sup>&#8722;3</sup> is the STP unit of volume of air. Average nitrate mass concentrations were 0.26&#8201;&#177;&#8201;0.27&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup> vs. 1.03&#8201;&#177;&#8201;0.74&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup> followed by sulfate with an average of 0.58&#8201;&#177;&#8201;0.23&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup> vs. 1.08&#8201;&#177;&#8201;0.73&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup> on non-cyclone vs. cyclonic days, respectively. In the most aged air masses (NO<sub>x</sub>/NO<sub>y</sub>&#8201;<&#8201;0.5), background OA over DM increased by a factor of ~&#8201;4, from 0.93&#8201;&#177;&#8201;0.33&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup> to 3.70&#8201;&#177;&#8201;0.28&#8201;&#181;g&#8201;sm<sup>&#8722;3</sup> due to transport from NFR. Furthermore, enhanced partitioning of nitric acid to the aerosol phase was observed during the cyclone episodes, mainly due to increased abundance of gas phase NH<sub>3</sub>. During the non-cyclone events, &#946;<sub>ext</sub> displayed strong correlations (<i>r</i>&#8201;=&#8201;0.71) with OA and NO<sub>3</sub><sup>&#8722;</sup> in NFR and only with OA (<i>r</i>&#8201;=&#8201;0.70) in DM while correlation of &#946;<sub>ext</sub> during the cyclone was strongest (<i>r</i>&#8201;=&#8201;0.86) with NO<sub>3</sub><sup>&#8722;</sup> in DM. Mass extinction efficiency values (MEE) values in DM were similar under cyclone (2.85&#8201;&#177;&#8201;0.63&#8201;m<sup>2</sup>&#8201;g<sup>&#8722;1</sup>) and non-cyclone (2.72&#8201;&#177;&#8201;0.61&#8201;m<sup>2</sup>&#8201;g<sup>&#8722;1</sup>) days despite the dominant influence of different aerosol species on &#946;<sub>ext</sub> (non-cyclone: OA, cyclone; NO<sub>3</sub><sup>&#8722;</sup>).</p>