Using the UC Irvine Whole Air Sampler, I measured volatile organic compounds (VOCs) onboard the NASA DC-8 during the Student Airborne Research Program. High levels of the harmful chemical ozone were observed near the surface over the Sierra Nevada mountains, which led to the focus of my independent research project on the study of VOC data in order to investigate factors that contributed to ozone production. This was done by calculating the hydroxyl radical reactivity, which can, in proper conditions, be used to predict ozone formation potential. I divided the region into three boxes from east to west, based on wind direction, and the reactivity was analyzed over each region with respect to methane, non-methane alkanes, alkenes, aromatics, and biogenic compounds. In the westernmost box the reactivity was 1.7 ± 0.5 s-1 (1σ), in the middle section it was 1.4 ± 1 s-1, and in the easternmost region it was 0.8 ± 0.3 s-1. I compared the data in the Sierra Nevada region with a region known to be heavily polluted, the Los Angeles (LA) basin, and it was observed that the reactivity was 1.1 ± 0.6 s-1, lower than in two of the mountainous regions. In the Sierra Nevada mountains a major percentage of the hydroxyl radical reactivity was the result of biogenic influence, at 24% for the western box, 39% for the middle box, and 31% for the easternmost box, in contrast to only 2% biogenic contribution in LA. My work indicates that biogenic factors greatly contributed to overall ozone formation in the Sierra Nevada mountains. These mountains are strategically protected, and high pollution levels of ozone and other VOCs could lead to health impacts for visitors, vegetation, and wildlife.