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Methane and the Paris Agreement temperature goals.
Cain, Michelle; Jenkins, Stuart; Allen, Myles R; Lynch, John; Frame, David J; Macey, Adrian H; Peters, Glen P.
Afiliação
  • Cain M; Centre for Environmental and Agricultural Informatics, School of Water, Energy and Environment, Cranfield University, Cranfield MK43 0AL, UK.
  • Jenkins S; Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, UK.
  • Allen MR; Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, UK.
  • Lynch J; Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, UK.
  • Frame DJ; Environmental Change Institute, School of Geography and the Environment, University of Oxford, UK.
  • Macey AH; Atmospheric, Oceanic and Planetary Physics, Department of Physics, University of Oxford, UK.
  • Peters GP; New Zealand Climate Change Research Institute, Te Herenga Waka, Victoria University of Wellington, Wellington 6012, New Zealand.
Philos Trans A Math Phys Eng Sci ; 380(2215): 20200456, 2022 Jan 24.
Article em En | MEDLINE | ID: mdl-34865531
ABSTRACT
Meeting the Paris Agreement temperature goal necessitates limiting methane (CH4)-induced warming, in addition to achieving net-zero or (net-negative) carbon dioxide (CO2) emissions. In our model, for the median 1.5°C scenario between 2020 and 2050, CH4 mitigation lowers temperatures by 0.1°C; CO2 increases it by 0.2°C. CO2 emissions continue increasing global mean temperature until net-zero emissions are reached, with potential for lowering temperatures with net-negative emissions. By contrast, reducing CH4 emissions starts to reverse CH4-induced warming within a few decades. These differences are hidden when framing climate mitigation using annual 'CO2-equivalent' emissions, including targets based on aggregated annual emission rates. We show how the different warming responses to CO2 and CH4 emissions can be accurately aggregated to estimate warming by using 'warming-equivalent emissions', which provide a transparent and convenient method to inform policies and measures for mitigation, or demonstrate progress towards a temperature goal. The method presented (GWP*) uses well-established climate science concepts to relate GWP100 to temperature, as a simple proxy for a climate model. The use of warming-equivalent emissions for nationally determined contributions and long-term strategies would enhance the transparency of stocktakes of progress towards a long-term temperature goal, compared to the use of standard equivalence methods. This article is part of a discussion meeting issue 'Rising methane is warming feeding warming? (part 2)'.
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Texto completo: 1 Base de dados: MEDLINE Assunto principal: Efeito Estufa / Metano Idioma: En Ano de publicação: 2022 Tipo de documento: Article

Texto completo: 1 Base de dados: MEDLINE Assunto principal: Efeito Estufa / Metano Idioma: En Ano de publicação: 2022 Tipo de documento: Article