27
views
0
recommends
+1 Recommend
0 collections
    0
    shares
      • Record: found
      • Abstract: found
      • Article: found
      Is Open Access

      How necessary and feasible are reductions of methane emissions from livestock to support stringent temperature goals?

      research-article

      Read this article at

      Bookmark
          There is no author summary for this article yet. Authors can add summaries to their articles on ScienceOpen to make them more accessible to a non-specialist audience.

          Abstract

          Agriculture is the largest single source of global anthropogenic methane (CH 4) emissions, with ruminants the dominant contributor. Livestock CH 4 emissions are projected to grow another 30% by 2050 under current policies, yet few countries have set targets or are implementing policies to reduce emissions in absolute terms. The reason for this limited ambition may be linked not only to the underpinning role of livestock for nutrition and livelihoods in many countries but also diverging perspectives on the importance of mitigating these emissions, given the short atmospheric lifetime of CH 4. Here, we show that in mitigation pathways that limit warming to 1.5°C, which include cost-effective reductions from all emission sources, the contribution of future livestock CH 4 emissions to global warming in 2050 is about one-third of that from future net carbon dioxide emissions. Future livestock CH 4 emissions, therefore, significantly constrain the remaining carbon budget and the ability to meet stringent temperature limits. We review options to address livestock CH 4 emissions through more efficient production, technological advances and demand-side changes, and their interactions with land-based carbon sequestration. We conclude that bringing livestock into mainstream mitigation policies, while recognizing their unique social, cultural and economic roles, would make an important contribution towards reaching the temperature goal of the Paris Agreement and is vital for a limit of 1.5°C.

          This article is part of a discussion meeting issue 'Rising methane: is warming feeding warming? (part 1)'.

          Related collections

          Most cited references120

          • Record: found
          • Abstract: not found
          • Article: not found

          Food in the Anthropocene: the EAT–Lancet Commission on healthy diets from sustainable food systems

            Bookmark
            • Record: found
            • Abstract: found
            • Article: not found

            Reducing food’s environmental impacts through producers and consumers

            Food's environmental impacts are created by millions of diverse producers. To identify solutions that are effective under this heterogeneity, we consolidated data covering five environmental indicators; 38,700 farms; and 1600 processors, packaging types, and retailers. Impact can vary 50-fold among producers of the same product, creating substantial mitigation opportunities. However, mitigation is complicated by trade-offs, multiple ways for producers to achieve low impacts, and interactions throughout the supply chain. Producers have limits on how far they can reduce impacts. Most strikingly, impacts of the lowest-impact animal products typically exceed those of vegetable substitutes, providing new evidence for the importance of dietary change. Cumulatively, our findings support an approach where producers monitor their own impacts, flexibly meet environmental targets by choosing from multiple practices, and communicate their impacts to consumers.
              Bookmark
              • Record: found
              • Abstract: found
              • Article: not found

              Irreversible climate change due to carbon dioxide emissions.

              The severity of damaging human-induced climate change depends not only on the magnitude of the change but also on the potential for irreversibility. This paper shows that the climate change that takes place due to increases in carbon dioxide concentration is largely irreversible for 1,000 years after emissions stop. Following cessation of emissions, removal of atmospheric carbon dioxide decreases radiative forcing, but is largely compensated by slower loss of heat to the ocean, so that atmospheric temperatures do not drop significantly for at least 1,000 years. Among illustrative irreversible impacts that should be expected if atmospheric carbon dioxide concentrations increase from current levels near 385 parts per million by volume (ppmv) to a peak of 450-600 ppmv over the coming century are irreversible dry-season rainfall reductions in several regions comparable to those of the "dust bowl" era and inexorable sea level rise. Thermal expansion of the warming ocean provides a conservative lower limit to irreversible global average sea level rise of at least 0.4-1.0 m if 21st century CO(2) concentrations exceed 600 ppmv and 0.6-1.9 m for peak CO(2) concentrations exceeding approximately 1,000 ppmv. Additional contributions from glaciers and ice sheet contributions to future sea level rise are uncertain but may equal or exceed several meters over the next millennium or longer.
                Bookmark

                Author and article information

                Contributors
                Journal
                Philos Trans A Math Phys Eng Sci
                Philos Trans A Math Phys Eng Sci
                RSTA
                roypta
                Philosophical transactions. Series A, Mathematical, physical, and engineering sciences
                The Royal Society
                1364-503X
                1471-2962
                November 15, 2021
                September 27, 2021
                September 27, 2021
                : 379
                : 2210 , Discussion meeting issue ‘Rising methane: is warming feeding warming? (part 1)’ organised and edited by Euan G. Nisbet, Anna E. Jones, John A. Pyle FRS and Ute M. Skiba
                : 20200452
                Affiliations
                [ 1 ] Australian National University, , Canberra, Australia
                [ 2 ] New Zealand Agricultural Greenhouse Gas Research Centre (NZAGRC), , Palmerston North, New Zealand
                [ 3 ] New South Wales Department of Primary Industries/University of New England, , Armidale, Australia
                [ 4 ] Department of Global Development, College of Agriculture and Life Sciences, and Cornell Atkinson Centre for Sustainability, Cornell University, , Ithaca, USA
                Author notes

                One contribution of 12 to a discussion meeting issue ‘ Rising methane: is warming feeding warming? (part 1)’.

                Author information
                http://orcid.org/0000-0002-6631-7188
                http://orcid.org/0000-0002-3858-959X
                http://orcid.org/0000-0002-4140-7152
                http://orcid.org/0000-0002-7741-5090
                http://orcid.org/0000-0002-0386-9671
                http://orcid.org/0000-0002-5461-6738
                Article
                rsta20200452
                10.1098/rsta.2020.0452
                8480228
                34565223
                104fd056-a46b-40f1-8353-d2c87f166008
                © 2021 The Authors.

                Published by the Royal Society under the terms of the Creative Commons Attribution License http://creativecommons.org/licenses/by/4.0/, which permits unrestricted use, provided the original author and source are credited.

                History
                : June 2, 2021
                Categories
                1005
                1006
                12
                68
                Articles
                Research Articles
                Custom metadata
                November 15, 2021

                agriculture,methane,marginal warming,land use,sequestration,paris agreement

                Comments

                Comment on this article