Methane removal and the proportional reductions in surface temperature and ozone

Author:

Abernethy S.12ORCID,O'Connor F. M.3ORCID,Jones C. D.3ORCID,Jackson R. B.24ORCID

Affiliation:

1. Department of Applied Physics, Stanford University, Stanford 94305, USA

2. Department of Earth System Science, Stanford University, Stanford 94305, USA

3. Met Office Hadley Centre, FitzRoy Road, Exeter EX1 3PB, UK

4. Woods Institute for the Environment and Precourt Institute for Energy, Stanford University, Stanford 94305, USA

Abstract

Mitigating climate change requires a diverse portfolio of technologies and approaches, including negative emissions or removal of greenhouse gases. Previous literature focuses primarily on carbon dioxide removal, but methane removal may be an important complement to future efforts. Methane removal has at least two key benefits: reducing temperature more rapidly than carbon dioxide removal and improving air quality by reducing surface ozone concentration. While some removal technologies are being developed, modelling of their impacts is limited. Here, we conduct the first simulations using a methane emissions-driven Earth System Model to quantify the climate and air quality co-benefits of methane removal, including different rates and timings of removal. We define a novel metric, the effective cumulative removal, and use it to show that each effective petagram of methane removed causes a mean global surface temperature reduction of 0.21 ± 0.04°C and a mean global surface ozone reduction of 1.0 ± 0.2 parts per billion. Our results demonstrate the effectiveness of methane removal in delaying warming thresholds and reducing peak temperatures, and also allow for direct comparisons between the impacts of methane and carbon dioxide removal that could guide future research and climate policy. This article is part of a discussion meeting issue 'Rising methane: is warming feeding warming? (part 1)'.

Funder

Gordon and Betty Moore Foundation

Stanford Woods Institute for the Environment

European Union's Horizon 2020 CRESCENDO project

Stanford Data Science Scholars

Joint UK BEIS/Defra Met Office Hadley Centre Climate Programme

National Sciences and Engineering Research Council of Canada

Publisher

The Royal Society

Subject

General Physics and Astronomy,General Engineering,General Mathematics

Reference64 articles.

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3. The Global Methane Budget 2000–2017

4. Myhre G et al 2013 Anthropogenic and natural radiative forcing. In Climate change 2013: The Physical Science Basis. Contribution of Working Group I to the Fifth Assessment Report of the Intergovernmental Panel on Climate Change . Cambridge University Press.

5. Influences of hydroxyl radicals (OH) on top-down estimates of the global and regional methane budgets

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