Multi-decadal surface ozone trends at globally distributed remote locations

Author:

Cooper Owen R.1,Schultz Martin G.2,Schröder Sabine2,Chang Kai-Lan1,Gaudel Audrey1,Benítez Gerardo Carbajal3,Cuevas Emilio4,Fröhlich Marina5,Galbally Ian E.6,Molloy Suzie6,Kubistin Dagmar7,Lu Xiao8,McClure-Begley Audra9,Nédélec Philippe10,O’Brien Jason11,Oltmans Samuel J.12,Petropavlovskikh Irina9,Ries Ludwig13,Senik Irina14,Sjöberg Karin15,Solberg Sverre16,Spain Gerard T.17,Spangl Wolfgang5,Steinbacher Martin18,Tarasick David19,Thouret Valerie10,Xu Xiaobin20

Affiliation:

1. CIRES, University of Colorado/NOAA Chemical Sciences Laboratory, Boulder, US

2. Jülich Supercomputing Centre (JSC), Forschungszentrum Jülich, Jülich, DE

3. Atmospheric Watch & Geophysics – Research and Development Management, SMN, AR

4. Izaña Atmospheric Research Centre, AEMET, Santa Cruz de Tenerife, ES

5. Umweltbundesamt/Federal Environment Agency, AT

6. Climate Science Centre, CSIRO, Aspendale, Victoria, AU

7. Deutscher Wetterdienst, Hohenpeissenberg Meteorological Observatory, Hohenpeissenberg, DE

8. Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric and Oceanic Sciences, School of Physics, Peking University, Beijing, CN

9. CIRES, University of Colorado/NOAA Global Monitoring Laboratory, Boulder, US

10. Laboratoire d’Aérologie, Université de Toulouse, CNRS, UPS, FR

11. Air Quality Research Division, Environment and Climate Change Canada, Toronto, Ontario, CA

12. NOAA Global Monitoring Laboratory, Boulder, Colorado, US

13. German Environment Agency, GAW Global Observatory Zugspitze/Hohenpeissenberg, Zugspitze, DE

14. Kislovodsk High Mountain Station of Obukhov Institute of Atmospheric Physics RAS, RU

15. Swedish Environmental Research Inst., Göteborg, SE

16. Norwegian Institute for Air Research, NILU, Kjeller, NO

17. School of Physics, National University of Ireland Galway, Galway, IE

18. Empa, Swiss Federal Laboratories for Materials Science and Technology, Duebendorf, CH

19. Environment and Climate Change Canada, 4905 Dufferin Street, Downsview, ON, M3H 5T4 CA

20. Key Laboratory for Atmospheric Chemistry, Institute of Atmospheric Composition, Chinese Academy of Meteorological Sciences, China Meteorological Administration, Beijing, CN

Abstract

Extracting globally representative trend information from lower tropospheric ozone observations is extremely difficult due to the highly variable distribution and interannual variability of ozone, and the ongoing shift of ozone precursor emissions from high latitudes to low latitudes. Here we report surface ozone trends at 27 globally distributed remote locations (20 in the Northern Hemisphere, 7 in the Southern Hemisphere), focusing on continuous time series that extend from the present back to at least 1995. While these sites are only representative of less than 25% of the global surface area, this analysis provides a range of regional long-term ozone trends for the evaluation of global chemistry-climate models. Trends are based on monthly mean ozone anomalies, and all sites have at least 20 years of data, which improves the likelihood that a robust trend value is due to changes in ozone precursor emissions and/or forced climate change rather than naturally occurring climate variability. Since 1995, the Northern Hemisphere sites are nearly evenly split between positive and negative ozone trends, while 5 of 7 Southern Hemisphere sites have positive trends. Positive trends are in the range of 0.5–2 ppbv decade–1, with ozone increasing at Mauna Loa by roughly 50% since the late 1950s. Two high elevation Alpine sites, discussed by previous assessments, exhibit decreasing ozone trends in contrast to the positive trend observed by IAGOS commercial aircraft in the European lower free-troposphere. The Alpine sites frequently sample polluted European boundary layer air, especially in summer, and can only be representative of lower free tropospheric ozone if the data are carefully filtered to avoid boundary layer air. The highly variable ozone trends at these 27 surface sites are not necessarily indicative of free tropospheric trends, which have been overwhelmingly positive since the mid-1990s, as shown by recent studies of ozonesonde and aircraft observations.

Publisher

University of California Press

Subject

Atmospheric Science,Geology,Geotechnical Engineering and Engineering Geology,Ecology,Environmental Engineering,Oceanography

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