The impact of tropopause fold event on surface ozone concentration over Tibetan Plateau in July

Tropopause fold events are one of the major processes in stratosphere-troposphere exchange (STE) in the mid-latitudes. The Tibetan Plateau (TP) is a hotspot of STE in the world. It has been proved that the tropopause fold events over the TP could impact on tropospheric ozone concentration in summer, yet most of these studies only focus on tropopause fold events at individual stations. In this study, we use ozone soundings data over Minle County (38.41 degrees N, 100.65 degrees E) and surface observations in the TP to verify the effect of tropopause fold events on surface ozone concentration. The stratospheric ozone tracers (O3S) simulation by the WACCM model and the passive tracers simulation by the WRF model indicate that the tropopause fold event observed on 11 July 2020 contributed to surface ozone in the northern regions of TP. In addition, we identified all the tropopause fold events that occurred over the TP in each July from 2015 to 2020 and quantified their impacts on surface ozone concentration. The results show that the average increase in surface ozone concentration is 15.94 ppbv during the period affected by the tropopause fold events. The site most affected by tropopause fold events is Shannan City, followed by Nyingchi City. This study revealed the importance of the influence of tropopause fold event on surface ozone concentration in the TP in summer.