Multiyear Composite View of Ozone Enhancements and Stratosphere‐to‐Troposphere Transport in Dry Intrusions of Northern Hemisphere Extratropical Cyclones

Abstract We examine the role of extratropical cyclones in stratosphere‐to‐troposphere (STT) exchange with cyclone‐centric composites of O3retrievals from the Microwave Limb Sounder (MLS) and the Tropospheric Emission Spectrometer (TES), contrasting them to composites obtained with the Modern‐Era Retrospective‐analysis for Research and Applications (MERRA and MERRA‐2) reanalyses and the GEOS‐Chem chemical transport model. We identify 15,978 extratropical cyclones in the northern hemisphere (NH) for 2005–2012. The lowermost stratosphere (261 hPa) and middle troposphere (424 hPa) composites feature a 1,000 km wide O3enhancement in the dry intrusion (DI) airstream to the southwest of the cyclone center, coinciding with a lowered tropopause, enhanced potential vorticity, and decreased H2O. MLS composites at 261 hPa show that the DI O3enhancements reach a 210 ppbv maximum in April. At 424 hPa, TES composites display maximum O3enhancements of 27 ppbv in May. The magnitude and seasonality of these enhancements are captured by MERRA and MERRA‐2, but GEOS‐Chem is a factor of 2 too low. The MERRA‐2 composites show that the O3‐rich DI forms a vertically aligned structure between 300 and 800 hPa, wrapping cyclonically with the warm conveyor belt. In winter and spring DIs, O3is enhanced by 100 ppbv or 100–130% at 300 hPa, with significant enhancements below 500 hPa (6–20 ppbv or 15–30%). We estimate that extratropical cyclones result in a STT flux of 119 ± 56 Tg O3 yr−1, accounting for 42 ± 20% of the NH extratropical O3STT flux. The STT flux in cyclones displays a strong dependence on westerly 300 hPa wind speeds.