An Unusual Winter Ozone Event in Colorado

Abstract Surface ozone (O 3 ) mixing ratios exceeding the National Ambient Air Quality Standard were measured at rural monitors along the Colorado Front Range on 17 April 2020 during the COVID‐19 lockdown. This unusual episode followed back‐to‐back upslope snowstorms and coincided with the presence of a deep stratospheric intrusion, but ground‐based lidar and ozonesonde measurements show that little, if any, of the O 3 ‐rich lower stratospheric air reached the surface. Instead, the statically stable lower stratospheric air suppressed the growth of the daytime boundary layer and trapped nitrogen oxides (NO x = NO + NO 2 ) and volatile organic compounds (VOCs) emitted by motor vehicles and oil and natural gas (O&NG) operations near the ground where the clear skies and extensive snow cover triggered a short‐lived photochemical episode similar to those observed in the O&NG producing basins of northeastern Utah and southwestern Wyoming. In this study, we use a combination of lidar, ozonesonde, and surface measurements, together with the WRF‐Chem and Goddard Earth Observing System composition forecast models, to describe the stratospheric intrusion and characterize the boundary layer structure, HYSPLIT back trajectories to show the low‐level transport of O 3 and its precursors to the exceedance sites, and surface measurements of NO x and VOCs together with a 0‐D box model to investigate the roles of urban and O&NG emissions and the COVID‐19 quarantine in the O 3 production. The box model showed the O 3 production to be NO x saturated, such that the NO x reductions associated with COVID‐19 exacerbated the event rather than mitigating it.

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Publication Details

Journal
Journal of Geophysical Research Atmospheres
Published
2025-07-26
DOI
https://doi.org/10.1029/2025jd043695
Primary Topic
Atmospheric chemistry and aerosols
Type
article
Field-Weighted Citation Impact
0.00

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article

An Unusual Winter Ozone Event in Colorado

C. Warneke, R. J. Alvarez, Rajesh Kumar, B. J. Johnson et al.
Journal of Geophysical Research Atmospheres
Atmospheric chemistry and aerosols
article

An Unusual Winter Ozone Event in Colorado

C. Warneke, R. J. Alvarez, Rajesh Kumar, B. J. Johnson, Ann M. Middlebrook, Michael A. Robinson, Irina V. Petropavlovskikh, K. C. Aikin, Patrick Cullis, Jessica B. Gilman, Alan Brewer, Detlev Helmig, Matthew Mitchell Coggon, K. Emma Knowland, Gabriele G. Pfister, Pamela S. Rickly, Jeff Peischl, Christoph J. Senff, Brandi McCarty, Aaron Lamplugh, Andrew W. Rollins, Sunil Baidar, Steven S. S Brown, Georgios I. Gkatzelis, A. O. Langford, Scott P. Sandberg
article en

Abstract

Abstract Surface ozone (O 3 ) mixing ratios exceeding the National Ambient Air Quality Standard were measured at rural monitors along the Colorado Front Range on 17 April 2020 during the COVID‐19 lockdown. This unusual episode followed back‐to‐back upslope snowstorms and coincided with the presence of a deep stratospheric intrusion, but ground‐based lidar and ozonesonde measurements show that little, if any, of the O 3 ‐rich lower stratospheric air reached the surface. Instead, the statically stable lower stratospheric air suppressed the growth of the daytime boundary layer and trapped nitrogen oxides (NO x = NO + NO 2 ) and volatile organic compounds (VOCs) emitted by motor vehicles and oil and natural gas (O&NG) operations near the ground where the clear skies and extensive snow cover triggered a short‐lived photochemical episode similar to those observed in the O&NG producing basins of northeastern Utah and southwestern Wyoming. In this study, we use a combination of lidar, ozonesonde, and surface measurements, together with the WRF‐Chem and Goddard Earth Observing System composition forecast models, to describe the stratospheric intrusion and characterize the boundary layer structure, HYSPLIT back trajectories to show the low‐level transport of O 3 and its precursors to the exceedance sites, and surface measurements of NO x and VOCs together with a 0‐D box model to investigate the roles of urban and O&NG emissions and the COVID‐19 quarantine in the O 3 production. The box model showed the O 3 production to be NO x saturated, such that the NO x reductions associated with COVID‐19 exacerbated the event rather than mitigating it.

Journal of Geophysical Research AtmospheresVol. 130(14)
NSF National Center for Atmospheric Research (US), Goddard Space Flight Center (US), Colorado Department of Public Health and Environment (US), Cooperative Institute for Research in Environmental Sciences (US), Forschungszentrum Jülich (DE), University of Colorado Boulder (US), Research Applications (United States) (US), NOAA Chemical Sciences Laboratory (US), Morgan State University (US)
National Science Foundation, National Oceanic and Atmospheric Administration, Earth Sciences Division
Openalex Percentile: Top 77%
Atmospheric chemistry and aerosols
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