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Climate change research and action must look beyond 2100.
Lyon, Christopher; Saupe, Erin E; Smith, Christopher J; Hill, Daniel J; Beckerman, Andrew P; Stringer, Lindsay C; Marchant, Robert; McKay, James; Burke, Ariane; O'Higgins, Paul; Dunhill, Alexander M; Allen, Bethany J; Riel-Salvatore, Julien; Aze, Tracy.
Afiliação
  • Lyon C; Department of Natural Resource Sciences, McGill University, Ste Anne de Bellevue, Quebec, Canada.
  • Saupe EE; School of Earth and Environment, University of Leeds, Leeds, UK.
  • Smith CJ; Department of Earth Sciences, University of Oxford, Oxford, UK.
  • Hill DJ; School of Earth and Environment, University of Leeds, Leeds, UK.
  • Beckerman AP; International Institute for Applied Systems Analysis (IIASA), Laxenburg, Austria.
  • Stringer LC; School of Earth and Environment, University of Leeds, Leeds, UK.
  • Marchant R; Ecology and Evolutionary Biology, School of Biosciences, University of Sheffield, Sheffield, UK.
  • McKay J; Department of Environment and Geography, University of York, York, UK.
  • Burke A; Department of Environment and Geography, University of York, York, UK.
  • O'Higgins P; School of Chemical and Process Engineering, University of Leeds, Leeds, UK.
  • Dunhill AM; Département d'Anthropologie, Université de Montréal, Montréal, Quebec, Canada.
  • Allen BJ; Department of Archaeology and Hull York Medical School, University of York, York, UK.
  • Riel-Salvatore J; School of Earth and Environment, University of Leeds, Leeds, UK.
  • Aze T; School of Earth and Environment, University of Leeds, Leeds, UK.
Glob Chang Biol ; 28(2): 349-361, 2022 01.
Article em En | MEDLINE | ID: mdl-34558764
ABSTRACT
Anthropogenic activity is changing Earth's climate and ecosystems in ways that are potentially dangerous and disruptive to humans. Greenhouse gas concentrations in the atmosphere continue to rise, ensuring that these changes will be felt for centuries beyond 2100, the current benchmark for projection. Estimating the effects of past, current, and potential future emissions to only 2100 is therefore short-sighted. Critical problems for food production and climate-forced human migration are projected to arise well before 2100, raising questions regarding the habitability of some regions of the Earth after the turn of the century. To highlight the need for more distant horizon scanning, we model climate change to 2500 under a suite of emission scenarios and quantify associated projections of crop viability and heat stress. Together, our projections show global climate impacts increase significantly after 2100 without rapid mitigation. As a result, we argue that projections of climate and its effects on human well-being and associated governance and policy must be framed beyond 2100.
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Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Mudança Climática / Gases de Efeito Estufa Tipo de estudo: Prognostic_studies Limite: Humans Idioma: En Ano de publicação: 2022 Tipo de documento: Article

Texto completo: 1 Coleções: 01-internacional Base de dados: MEDLINE Assunto principal: Mudança Climática / Gases de Efeito Estufa Tipo de estudo: Prognostic_studies Limite: Humans Idioma: En Ano de publicação: 2022 Tipo de documento: Article