Summary
A significant rise in summertime ozone (O₃) levels at Carlsbad Caverns National Park, exceeding 70 ppbv, is linked to the rapid expansion of oil and natural gas (O&G) development in southeastern New Mexico. The study reveals that O₃ production is highly responsive to reductions in both nitrogen oxides (NOₓ) and O&G-related volatile organic compounds (VOCs), with NOₓ reductions proving most effective. Using a constrained F0AM box model, researchers analyzed VOC reactivity and radical budgets, demonstrating that morning O₃ levels are primarily controlled by local photochemistry, while afternoon levels become sensitive to NOₓ loss. A high-O₃ episode was found to be influenced by aged O&G emissions, as indicated by back-trajectory analysis and low i-/n-pentane ratios, suggesting significant nonlocal O₃ formation.
Citation
Marsavin, A., Pan, D., Pollack, I. B., Zhou, Y., Sullivan, A. P., Naimie, L. E., Benedict, K. B., Juncosa Calahoranno, J. F., Fischer, E. V., Prenni, A. J., Schichtel, B. A., Sive, B. C., & Collett, J. L. (2024). Summertime Ozone Production at Carlsbad Caverns National Park, New Mexico: Influence of Oil and Natural Gas Development. Journal of Geophysical Research: Atmospheres, 129(14). Portico. https://doi.org/10.1029/2024jd040877