文摘
In this study, we quantify the frequency of stratosphere-troposphere exchange (STE) events that result in ozone (O<sub>3sub>) concentration enhancements (i.e., hourly average concentrations?¡Ý50?ppb) observed at 39 high- and low-elevation monitoring sites in the US during the years 2007-2009. We employ a refined forward trajectory-based approach to address the relationship between stratospheric intrusions and enhancements in hourly average O<sub>3sub> concentrations. The model is applied to high-resolution European Center for Medium-Range Weather Forecasting (ECMWF) analyses to identify specific days when the potential for stratosphere-to-troposphere transport (STT) exists to affect surface O<sub>3sub> levels. Our results indicate that STT down to the surface (STT-S) frequently contributes to enhanced surface O<sub>3sub> hourly averaged concentrations at sites across the US, with substantial year-to-year variability. The O<sub>3sub> concentrations associated with the STT-S events appear to be large enough to enhance the measured O<sub>3sub> concentrations during specific months of the year. Months with a statistically significant coincidence between enhanced O<sub>3sub> concentrations and STT-S occur most frequently at the high-elevation sites in the Intermountain West, as well as at the high-elevation sites in the West and East. These sites exhibit a preference for coincidences during the springtime and in some cases, the summer, fall, and late winter. Besides the high-elevation monitoring sites, low-elevation monitoring sites across the entire US experience enhanced O<sub>3sub> concentrations coincident with STT-S events.