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Climate and air quality impacts due to mitigation of non-methane near-term climate forcers

Authors :
Robert J. Allen
Steven Turnock
Pierre Nabat
David Neubauer
Ulrike Lohmann
Dirk Olivie
Naga Oshima
Martine Michou
Tongwen Wu
Jie Zhang
Toshihiko Takemura
Michael Schulz
Kostas Tsigaridis
Susanne E. Bauer
Louisa Emmons
Larry Horowitz
Vaishali Naik
Twan van Noije
Tommi Bergman
Jean-Francois Lamarque
Prodromos Zanis
Ina Tegen
Daniel M. Westervelt
Philippe Le Sager
Peter Good
Sungbo Shim
Fiona O'Connor
Dimitris Akritidis
Aristeidis K. Georgoulias
Makoto Deushi
Lori T. Sentman
Shinichiro Fujimori
William J. Collins
Publication Year :
2020
Publisher :
Copernicus GmbH, 2020.

Abstract

Over the next few decades, policies that optimally address both climate change and air quality are essential. Although targeting near-term climate forcers (NTCFs), defined here as aerosols, tropospheric ozone and precursor gases (but not methane), should improve air quality, NTCF reductions will also impact climate. How future policies affect the abundance of NTCFs and their impact on climate and air quality remains uncertain. Here, we quantify the 2015–2055 climate and air quality effects of non-methane NTCFs using state-of-the-art chemistry-climate model simulations conducted for the Aerosol and Chemistry Model Intercomparison Project (AerChemMIP). Simulations are driven by two future scenarios featuring similar increases in greenhouse gases (GHGs) but with weak versus strong levels of air quality control measures. Unsurprisingly, we find significant improvements in air quality under NTCF mitigation (strong versus weak air quality controls). Surface ozone (O3) and fine particulate matter (PM2.5) decrease by −15 % and −25 %, respectively, over global land surfaces, with larger reductions in some regions including south and southeast Asia. Non-methane NTCF mitigation, however, leads to additional climate change due to the removal of aerosol which causes a net warming effect, including global mean surface temperature and precipitation increases of 0.24 K and 1.1 %, respectively, with similar increases in extreme weather indices. Regionally, the largest warming and wetting trends occur over Asia, including central and north Asia (0.56 K and 2.1 %), south Asia (0.48 K and 4.6 %) and east Asia (0.44 K and 4.7 %). Relatively large warming and wetting of the Arctic also occurs at 0.41 K and 2.1 %, respectively. Similar surface warming occurs in model simulations with aerosol-only mitigation, implying weak cooling due to ozone reductions. Our findings suggest that future policies that aggressively target non-methane NTCF reductions will improve air quality, but will lead to additional surface warming, particularly in Asia and the Arctic. Policies that address other NTCFs including methane, as well as carbon dioxide emissions, must also be adopted to meet mitigation goals.

Details

Database :
OpenAIRE
Accession number :
edsair.doi...........955622a67a3af5589613aa83d61be934
Full Text :
https://doi.org/10.5194/acp-2019-1209