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Impact of methane and black carbon mitigation on forcing and temperature: a multi-model scenario analysis

Authors :
Smith, Steven J.
Chateau, Jean
Dorheim, Kalyn
Drouet, Laurent
Durand-Lasserve, Olivier
Fricko, Oliver
Fujimori, Shinichiro
Hanaoka, Tatsuya
Harmsen, Mathijs
Hilaire, Jérôme
Keramidas, Kimon
Klimont, Zbigniew
Luderer, Gunnar
Moura, Maria Cecilia P.
Riahi, Keywan
Rogelj, Joeri
Sano, Fuminori
van Vuuren, Detlef P.
Wada, Kenichi
Smith, Steven J.
Chateau, Jean
Dorheim, Kalyn
Drouet, Laurent
Durand-Lasserve, Olivier
Fricko, Oliver
Fujimori, Shinichiro
Hanaoka, Tatsuya
Harmsen, Mathijs
Hilaire, Jérôme
Keramidas, Kimon
Klimont, Zbigniew
Luderer, Gunnar
Moura, Maria Cecilia P.
Riahi, Keywan
Rogelj, Joeri
Sano, Fuminori
van Vuuren, Detlef P.
Wada, Kenichi
Source :
Climatic Change vol.163 (2020) p.1427-1442 [ISSN 0165-0009]
Publication Year :
2020

Abstract

The relatively short atmospheric lifetimes of methane (CH4) and black carbon (BC) have focused attention on the potential for reducing anthropogenic climate change by reducing Short-Lived Climate Forcer (SLCF) emissions. This paper examines radiative forcing and global mean temperature results from the Energy Modeling Forum (EMF)-30 multi-model suite of scenarios addressing CH4 and BC mitigation, the two major short-lived climate forcers. Central estimates of temperature reductions in 2040 from an idealized scenario focused on reductions in methane and black carbon emissions ranged from 0.18–0.26 °C across the nine participating models. Reductions in methane emissions drive 60% or more of these temperature reductions by 2040, although the methane impact also depends on auxiliary reductions that depend on the economic structure of the model. Climate model parameter uncertainty has a large impact on results, with SLCF reductions resulting in as much as 0.3–0.7 °C by 2040. We find that the substantial overlap between a SLCF-focused policy and a stringent and comprehensive climate policy that reduces greenhouse gas emissions means that additional SLCF emission reductions result in, at most, a small additional benefit of ~ 0.1 °C in the 2030–2040 time frame.

Details

Database :
OAIster
Journal :
Climatic Change vol.163 (2020) p.1427-1442 [ISSN 0165-0009]
Notes :
DOI: 10.1007/s10584-020-02794-3, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1445815627
Document Type :
Electronic Resource