2024 Data (Information)
The Evolutions and Large-scale Mechanisms of Summer Stratospheric Ozone Intrusion across Global Hotspots, version 2
Stratospheric ozone intrusions can have a significant impact on regional near-surface ozone levels. Especially in summer, intrusions can contribute to extreme ozone events because of preexisting high ozone levels near the surface and cause serious health issues. Considering the increasing trend of surface ozone level, an understanding of stratospheric ozone intrusion is necessary. From a 19-year Whole Atmosphere Community Climate Model, version 6 (WACCM6) simulation and a stratospheric origin ozone tracer, we identify the global hotspots of stratospheric intrusions based on extreme tracer concentrations near the surface: North America, Africa, the Mediterranean, and the Middle East. We investigate the common underlying large-scale mechanisms of the stratospheric intrusions over the identified hotspots from the lower stratosphere to the lower troposphere. From the trajectory analysis, we find that the upper-level jet drives isentropic mixing near the jet axis and initiates stratospheric ozone intrusion. Subsequently, climatological descent at the lower troposphere brings the ozone down to the surface, which explains the spatial preference of summertime stratospheric intrusion events.
Files
- MCA_O3ad_O3Sad_850hPa_NA_JJA_daily.nc application/netcdf 596 KB Download File
- MCA_O3ad_O3Sad_850hPa_MD_JJA_daily.nc application/netcdf 425 KB Download File
- MCA_O3ad_O3Sad_850hPa_Af_JJA_daily.nc application/netcdf 425 KB Download File
- MCA_O3ad_O3Sad_850hPa_ME_JJA_daily.nc application/netcdf 425 KB Download File
- MD_m1_500hPa_-3day_back_trajectory.nc application/netcdf 7.18 MB Download File
- ME_m1_500hPa_-3day_back_trajectory.nc application/netcdf 7.63 MB Download File
- NA_m1_500hPa_-3day_back_trajectory.nc application/netcdf 9.11 MB Download File
- O3S_99-_frequency_NH_FigS1.nc application/netcdf 1.7 MB Download File
- Hovmoller_O3S_composite_Fig3.nc application/netcdf 12.8 KB Download File
- vertical_transport_decomposition_Fig6.docx application/vnd.openxmlformats-officedocument.wordprocessingml.document 26 KB Download File
- OMEGA_500_850hPa_Summer_Climatology.nc application/netcdf 444 KB Download File
- U_200hPa_composite_Fig4.nc application/netcdf 875 KB Download File
- Relative_lat_jet_core_ME.nc application/netcdf 11.7 MB Download File
- Relative_lat_jet_core_MD.nc application/netcdf 11 MB Download File
- Relative_lat_jet_core_Af.nc application/netcdf 14.9 MB Download File
- Relative_lat_jet_core_NA.nc application/netcdf 14 MB Download File
- Extreme_ozone_event_frequency_850hPa_Fig1.nc application/netcdf 930 KB Download File
- Af_m1_500hPa_-3day_back_trajectory.nc application/netcdf 9.76 MB Download File
More About This Work
- Academic Units
- Earth and Environmental Sciences
- Published Here
- January 30, 2024
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Notes
The data for each figure of “The Evolutions and Large-scale Mechanisms of Summer Stratospheric Ozone Intrusion across Global Hotspots” submitted is included. The file's title includes a variable description and which figure it leads to. The MCA result includes patterns and PC timeseries for O3S and O3 up to the 10th mode. Only the leading mode is used for the analysis and to make Figs. 2 and S3. Also, it can be used to extract the event days for further analysis. Back trajectory results are used to make the left column of Fig. 4. It includes the 3-dimensional location of the tracers. The relative location files are for the center and the right column of Fig. 4. Also, it is used to conduct a significance test in section 3.3. The vertical transport decomposition file is for Fig. 6. The exact name and units of the variables are included in the attribute of each file. Compared to the first version, we added data for Fig. 7, 500-850 hPa averaged global summer climatological omega.