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Multi-decadal surface ozone trends at globally distributed remote locations

Authors :
Owen R. Cooper
Martin G. Schultz
Sabine Schroeder
Kai-Lan Chang
Audrey Gaudel
Gerardo Carbajal Benítez
Emilio Cuevas
Marina Fröhlich
Ian E. Galbally
Suzie Molloy
Dagmar Kubistin
Xiao Lu
Audra McClure-Begley
Philippe Nédélec
Jason O'Brien
Samuel J. Oltmans
Irina Petropavlovskikh
Ludwig Ries
Irina Senik
Karin Sjöberg
Sverre Solberg
Gerard T. Spain
Wolfgang Spangl
Martin Steinbacher
David Tarasick
Valerie Thouret
Xiaobin Xu
Source :
Elementa: Science of the Anthropocene, Vol 8, Iss 1 (2020)
Publication Year :
2020
Publisher :
BioOne, 2020.

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.

Details

Language :
English
ISSN :
23251026
Volume :
8
Issue :
1
Database :
Directory of Open Access Journals
Journal :
Elementa: Science of the Anthropocene
Publication Type :
Academic Journal
Accession number :
edsdoj.b3343ff258494b51a04315aa3e59b124
Document Type :
article
Full Text :
https://doi.org/10.1525/elementa.420