Contrary to most regions in the U.S., ozone in the Northern Front Range Metropolitan Area (NFRMA) of Colorado was either stagnant or increasing between 2000 and 2015, despite substantial reductions in NO_x emissions. We used available long-term ozone and NO_x data in the NFRMA to investigate these trends. Ozone increased from weekdays to weekends for a number of sites in the NFRMA with weekend reductions in NO₂ at two sites in downtown Denver, indicating that the

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... egion was in a NO_x-saturated ozone production regime. The stagnation and increases in ozone in the NFRMA are likely the result of (1) decreasing NO_x emissions in a NO_x-saturated environment, and (2) increased anthropogenic VOC emissions in the NFRMA. Further investigation of the weekday-weekend effect showed that the region outside of the most heavily trafficked Denver area was transitioning to peak ozone production towards NO_x-limited chemistry. This transition implies that continued NO_x decreases will result in ozone being less sensitive to changes in either anthropogenic or biogenic VOC reactivity in the NFRMA. Biogenic VOCs are unlikely to have increased in the NFRMA between 2000 and 2015, but are temperature dependent and likely vary by drought year. Ozone in the NFRMA has a temperature dependence, consistent with biogenic VOC contributions to ozone production in the region. We show that while ozone increased with temperature in the NFRMA, which is consistent with a NOx-saturated regime, this relationship is suppressed in drought years. We attribute this drought year suppression to decreased biogenic isoprene emissions due to long-term drought stress.