Lockdown led to less smoggy ozone

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Researchers recorded on average a seven per cent drop in Northern Hemisphere ozone levels, between 1-8 kilometers above Earth’s surface, from April to August 2020. The gas at this altitude is considered ‘bad’ ozone, largely a pollutant generated by human industry and transportation, and a component of smog. However the study did not measure ozone at ground level, and some studies in congested cities reported ozone concentrations increased by 10 to 30 per cent - which the authors say can be explained by the complex chemistry of ozone. New Zealand and Australian scientists provided data to this study.

Media release

From: American Geophysical Union

During spring and summer of 2020, ozone at 1-8 kilometers (0.6-5 miles) above Earth’s surface fell by 7% on average across the Northern Hemisphere, a new study finds. The decrease is likely explained by curtailed transportation due to COVID-19 quarantines, according to the report, published in Geophysical Research Letters, AGU’s journal for high-impact, short-format reports with immediate implications spanning all Earth and space sciences.

Worldwide, surface traffic emissions went down by 14% and air-traffic emissions by 40% on average in 2020.

The new study analyzed data from weather balloons and remote sensing instruments from 45 stations. Many of the observatories saw similar ozone decreases in this layer of the atmosphere, to levels which had not been recorded in two decades.

“This is a remarkably large ozone reduction, over a very big region,” said Wolfgang Steinbrecht, an atmospheric scientist at Deutscher Wetterdienst’s (the German weather service’s) Hohenpeissenberg Meteorological Observatory, and lead-author of the study. “The last time we’ve seen such low free tropospheric ozone in Hohenpeissenberg was 1976.”

About 90% of Earth’s ozone is produced naturally through sunlight driven reactions in the stratosphere, a layer of the atmosphere about 10-50 kilometers (6-30 miles) above Earth’s surface, separated from the ground level atmosphere by jet streams. This “good” ozone absorbs harmful ultraviolet light and is essential to life on Earth.

Ozone in the atmosphere from the ground to about 10 kilometers (6 miles), the layer called the troposphere, is largely a pollutant generated by human industry and transportation, and a component of smog. This “bad” ozone is created by chemical reactions with nitrogen oxides (NOx) produced in fossil fuel combustion and with volatile organic compounds mostly produced by plants. Breathing ozone in high enough concentrations inflames the lungs, worsens existing health conditions like asthma, emphysema and bronchitis and can increase the risk of heart attack and stroke.

The results of the new study contrast with ground level findings from recent studies in congested cities, which reported ozone concentrations increasing by 10 to 30% in some urban locations as nitrogen oxides decreased during quarantines. This can be explained by the complicated chemistry of ozone and other pollutants, Steinbrecht said. In heavily polluted air, nitrogen oxides can destroy ozone, so, counterintuitively, decreasing nitrogen oxides can lead to more ozone.

The new study did not measure ozone at ground level. The measured change in ozone at 1-8 kilometers altitude may be reflected by similar decreases in some cities, but it is unlikely to have notable impacts for people on the ground or stratospheric ozone, Steinbrecht said. The new study did not detect similar changes of stratospheric ozone and the authors do not anticipate the decrease in ozone in the lower atmosphere will impact the ozone hole.

“The implications for human heath are probably a lot smaller than all the other COVID-19 implications I would think,” Steinbrecht said. But the quarantine provides an excellent test case for atmospheric models. Simulations of 2020 conditions by NCAR’s latest Community Atmosphere Model (CAM6.3), which includes atmospheric chemistry, fit the observed ozone data well, according to Steinbrecht.

“Ozone is the poster child for the troposphere because we understand it well,” Steinbrecht said. “The COVID-19 lockdowns are an unplanned global scale atmospheric experiment. They show how complex the atmosphere can react to emission changes. We can learn many things from this, for example, what internationally coordinated emission controls could achieve for air-quality worldwide.”

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Media Release American Geophysical Union, Web page
Journal/
conference:
Geophysical Research Letters
Research:Paper
Organisation/s: National Institute of Water and Atmospheric Research (NIWA), Bureau of Meteorology, University of Wollongong, Deutscher Wetterdienst, Germany
Funder: Deutscher Wetterdienst funds the ozone program at Hohenpeißenberg and makes research like this possible. NOAA GML supported additional launches in Boulder and Trinidad Head in April and May 2020. NOAA and NASA’s Upper Atmosphere Composition Observations (UACO) Program support the SHADOZ ozone soundings at Hilo, Pago-Pago (American Samoa) and Suva (Fiji). UACO also provides partial support for the Boulder FTIR and the Table Mountain Lidar. The NDACC FTIR stations Bremen, Ny.Ålesund, Izaña, Kiruna, and Zugspitze have been supported by the German Bundesministerium für Wirtschaft und Energie (BMWi) via DLR under grants 50EE1711A, 50EE1711B, and 50EE1711D. Izaña, Kiruna, and Zugspitze have also been supported by the Helmholtz Society via the research program ATMO. The FTIR measurements in Bremen and Ny-Ålesund receive additional support by the Senate of Bremen, the FTIR measurements in Ny-Ålesund also by AWI Bremerhaven. The University of Bremen further acknowledges funding by DFG (German research foundation) TRR 172 – Project Number 268020496 – within the Transregional Collaborative Research Center “ArctiC Amplification: Climate Relevant Atmospheric and SurfaCe Processes, and Feedback Mechanisms (AC)3”. The University of Liège contribution has been supported primarily by the Fonds de la Recherche Scientifique - FNRS under grant J.0147.18, as well as by the CAMS project. EM is a senior research associate of the F.R.S.-FNRS. The Toronto FTIR measurements were supported by Environment and Climate Change Canada, the Natural Sciences and Engineering Research Council of Canada (NSERC), and the NSERC CREATE Training Program in Technologies for Exo-Planetary Science. The University of the Wollongong thanks the Australian Research Council that has provided significant support over the years for the NDACC site at Wollongong, most recently as part of project DP160101598. Part of this research work was carried out at the Jet Propulsion Laboratory, California Institute of Technology, under a contract with the National Aeronautics and Space Administration (80NM0018D004). The National Center for Atmospheric Research is sponsored by the National Science Foundation. The NCAR FTS observation programs at Thule, GR and Boulder, CO are supported under contract by the National Aeronautics and Space Administration (NASA). The Thule work is also supported by the NSF Office of Polar Programs (OPP). We wish to thank the Danish Meteorological Institute for support at the Thule site and NOAA for support of the MLO site. Key results for this manuscript were generated using Copernicus Atmosphere Monitoring Service Information from the European Community. No author reports a financial (or other) conflict of interest.
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