Articles | Volume 8, issue 2
https://doi.org/10.5194/esd-8-235-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/esd-8-235-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Accounting for the climate–carbon feedback in emission metrics
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, Université Paris-Saclay, CEA – CNRS – UVSQ, 91191 Gif-sur-Yvette, France
Center for International Climate and Environmental Research – Oslo (CICERO), 0349 Oslo, Norway
now at: International Institute for Applied Systems Analysis (IIASA), 2361 Laxenburg, Austria
Glen P. Peters
Center for International Climate and Environmental Research – Oslo (CICERO), 0349 Oslo, Norway
Jan S. Fuglestvedt
Center for International Climate and Environmental Research – Oslo (CICERO), 0349 Oslo, Norway
William J. Collins
Department of Meteorology, University of Reading, Reading, RG6 6BB, UK
Drew T. Shindell
Nicholas School of the Environment, Duke University, Durham, NC 27708, USA
Philippe Ciais
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL, Université Paris-Saclay, CEA – CNRS – UVSQ, 91191 Gif-sur-Yvette, France
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Latest update: 14 Dec 2024
Short summary
Emission metrics such as GWP or GTP are used to put non-CO2 species on a
CO2-equivalentscale. In the fifth IPCC report the metrics are inconsistent, as the climate–carbon feedback is included only for CO2 but not for non-CO2 species. Here, we simulate a new impulse response function for the feedback, and we use it to correct the metrics. For instance, 1 g of CH4 is equivalent to 31 g of CO2 (instead of 28 g) following the corrected GWP100 metric. It is 34 g if other factors are also updated.
Emission metrics such as GWP or GTP are used to put non-CO2 species on a
CO2-equivalentscale....
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