- 1Lamont-Doherty Earth Observatory of Columbia University, New York, NY, USA (jaewonl@ldeo.columbia.edu)
- 2NOAA Chemical Sciences Laboratory, Boulder, CO, USA (Amy.Butler@noaa.gov)
- 3NOAA Physical Sciences Laboratory, Boulder, CO, USA (john.albers@noaa.gov)
- 4School of Earth and Environmental Sciences, University of St Andrews, St Andrews, UK (shl21@st-andrews.ac.uk)
Sudden stratospheric warmings (SSWs) can significantly impact tropospheric weather systems. Previous studies suggest that SSWs may also influence stratosphere-to-troposphere transport (STT), but their spatial and temporal distribution and mechanisms are not fully understood. The complex relationships between SSWs and the El Niño-Southern Oscillation (ENSO) have also made it difficult to isolate the effects of SSWs on STT. From an idealized ENSO simulation with the WACCM4 model using a stratospheric origin ozone tracer, we investigate the effect of SSWs on the STT of ozone under different ENSO phases. We find a significant increase in lower tropospheric ozone from the SSW onset up to 3 months later over the Arctic, North America, and Europe, regardless of the ENSO phase. This study highlights the significant influence of SSWs on STT on a subseasonal scale. Our results also emphasize the need to consider SSWs when addressing the ENSO impact on STT.
How to cite: Lee, J., Butler, A., Albers, J., Wu, Y., and Lee, S.: Impact of Sudden Stratospheric Warmings on the Stratosphere-to-Troposphere Transport of Ozone, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-3360, https://doi.org/10.5194/egusphere-egu25-3360, 2025.