Drought, as a recurring hydroclimate extreme, can strike the contiguous United States (CONUS) with various severity, duration, and frequency (Chen et al., 2019). Drought brings prolonged dry conditions of the atmosphere and the land, often accompanied by high temperatures. These conditions not only change atmospheric processing mechanisms of chemical constituents, such as chemistry and transport, but also perturb the land-atmosphere exchange of chemical species. Therefore, droughts potentially impose large changes on the abundance of reactive species in the atmosphere, such as ozone (O 3 ), a criteria air pollutant detrimental to human and ecosystem health.Most of the prior investigations of O 3 changes under drought are case studies of a given drought period over a specific region (