Articles | Volume 17, issue 4
https://doi.org/10.5194/acp-17-2943-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-17-2943-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
US surface ozone trends and extremes from 1980 to 2014: quantifying the roles of rising Asian emissions, domestic controls, wildfires, and climate
Atmospheric and Oceanic Sciences, Princeton University, Princeton, NJ
08540, USA
NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA
Larry W. Horowitz
NOAA Geophysical Fluid Dynamics Laboratory, Princeton, NJ 08540, USA
Richard Payton
US Environmental Protection Agency, Region 8, Air Program, Denver, CO 80202, USA
Arlene M. Fiore
Lamont-Doherty Earth-Observatory and Department of Earth and
Environmental Sciences, Columbia University, Palisades, NY 10964, USA
Gail Tonnesen
US Environmental Protection Agency, Region 8, Air Program, Denver, CO 80202, USA
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Discussed (final revised paper)
Latest update: 14 Dec 2024
Short summary
US ozone pollution responds to varying global-to-regional precursor emissions and climate, with implications for designing effective air quality control policies. Asian anthropogenic emissions of ozone precursors tripled since 1990, contributing 65 % to western US ozone increases in spring, outpacing ozone decreases attained via 50 % US emission controls. In the eastern US, if emissions had not declined, more frequent hot extremes since 1990 would have worsened the highest ozone events in summer.
US ozone pollution responds to varying global-to-regional precursor emissions and climate, with...
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