| Autor: |
Stauffer RM; Universities Space Research Association c/o Atmospheric Chemistry and Dynamics Lab, NASA/Goddard Space Flight Center, Greenbelt, Maryland, USA., Thompson AM; NASA/Goddard Space Flight Center, Greenbelt, Maryland, USA., Witte JC; Science Systems and Applications, Inc., Lanham, Maryland, USA. |
| Abstrakt: |
Our previous studies employing the self-organizing map (SOM) clustering technique to ozonesonde data have found significant links among meteorological and chemical regimes, and the shape of the ozone (O 3 ) profile from the troposphere to the lower stratosphere. These studies, which focused on specific northern hemisphere mid-latitude geographical regions, demonstrated the advantages of SOM clustering by quantifying O 3 profile variability and the O 3 /meteorological correspondence. We expand SOM to a global set of ozonesonde profiles spanning 1980-present from 30 sites to summarize the connections among O 3 profiles, meteorology, and chemistry, using the Modern-Era Retrospective Analysis for Research and Applications, version 2 (MERRA-2) reanalysis and other ancillary data. Four clusters of O 3 mixing ratio profiles from the surface to the upper troposphere/lower stratosphere (UT/LS) are generated for each site, which show dominant profile shapes and typical seasonality (or lack thereof) that generally correspond to latitude (i.e. Tropical, Subtropical, Mid-Latitude, Polar). Examination of MERRA-2 output reveals a clear relationship among SOM clusters and covarying meteorological fields (geopotential height, potential vorticity, and tropopause height) for Polar and Mid-latitude sites. However, these relationships break down within ±30° latitude. Carbon monoxide satellite data, along with velocity potential, a proxy for convection, calculated from MERRA-2 wind fields assist characterization of the Tropical and Subtropical sites, where biomass burning and convective transport linked to the Madden-Julian Oscillation (MJO) dominate O 3 variability. In addition to geophysical characterization of O 3 profile variability, these results can be used to evaluate chemical transport model output and satellite measurements of O 3 . |
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