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dc.contributor.authorMeinshausen, Malte
dc.contributor.authorSchleussner, Carl-Friedrich
dc.contributor.authorBeyer, Kathleen
dc.contributor.authorBodeker, Greg
dc.contributor.authorBoucher, Olivier
dc.contributor.authorCanadell, Josep G.
dc.contributor.authorDaniel, John S.
dc.contributor.authorDiongue-Niang, Aïda
dc.contributor.authorDriouech, Fatima
dc.contributor.authorFischer, Erich
dc.contributor.authorForster, Piers
dc.contributor.authorGrose, Michael
dc.contributor.authorHansen, Gerrit
dc.contributor.authorHausfather, Zeke
dc.contributor.authorIlyina, Tatiana
dc.contributor.authorKikstra, Jarmo S.
dc.contributor.authorKimutai, Joyce
dc.contributor.authorKing, Andrew D.
dc.contributor.authorLee, June-Yi
dc.contributor.authorLennard, Chris
dc.contributor.authorLissner, Tabea
dc.contributor.authorNauels, Alexander
dc.contributor.authorPeters, Glen Philip
dc.contributor.authorPirani, Anna
dc.contributor.authorPlattner, Gian-Kasper
dc.contributor.authorPörtner, Hans
dc.contributor.authorRogelj, Joeri
dc.contributor.authorRojas, Maisa
dc.contributor.authorRoy, Joyashree
dc.contributor.authorSamset, Bjørn Hallvard
dc.contributor.authorSanderson, Benjamin
dc.contributor.authorSéférian, Roland
dc.contributor.authorSeneviratne, Sonia
dc.contributor.authorSmith, Christopher J.
dc.contributor.authorSzopa, Sophie
dc.contributor.authorThomas, Adelle
dc.contributor.authorUrge-Vorsatz, Diana
dc.contributor.authorVelders, Guus J. M.
dc.contributor.authorYokohata, Tokuta
dc.contributor.authorZiehn, Tilo
dc.contributor.authorNicholls, Zebedee
dc.date.accessioned2024-09-23T12:08:54Z
dc.date.available2024-09-23T12:08:54Z
dc.date.created2024-06-24T13:11:18Z
dc.date.issued2024
dc.identifier.citationGeoscientific Model Development. 2024, 17 (11), 4533-4559.en_US
dc.identifier.issn1991-959X
dc.identifier.urihttps://hdl.handle.net/11250/3153764
dc.description.abstractIn every Intergovernmental Panel on Climate Change (IPCC) Assessment cycle, a multitude of scenarios are assessed, with different scope and emphasis throughout the various Working Group reports and special reports, as well as their respective chapters. Within the reports, the ambition is to integrate knowledge on possible climate futures across the Working Groups and scientific research domains based on a small set of “framing pathways” such as the so-called representative concentration pathways (RCPs) in the Fifth IPCC Assessment Report (AR5) and the shared socioeconomic pathway (SSP) scenarios in the Sixth Assessment Report (AR6). This perspective, initiated by discussions at the IPCC Bangkok workshop in April 2023 on the “Use of Scenarios in AR6 and Subsequent Assessments”, is intended to serve as one of the community contributions to highlight the needs for the next generation of framing pathways that is being advanced under the Coupled Model Intercomparison Project (CMIP) umbrella, which will influence or even predicate the IPCC AR7 consideration of framing pathways. Here we suggest several policy research objectives that such a set of framing pathways should ideally fulfil, including mitigation needs for meeting the Paris Agreement objectives, the risks associated with carbon removal strategies, the consequences of delay in enacting that mitigation, guidance for adaptation needs, loss and damage, and for achieving mitigation in the wider context of societal development goals. Based on this context, we suggest that the next generation of climate scenarios for Earth system models should evolve towards representative emission pathways (REPs) and suggest key categories for such pathways. These framing pathways should address the most critical mitigation policy and adaptation plans that need to be implemented over the next 10 years. In our view, the most important categories are those relevant in the context of the Paris Agreement long-term goal, specifically an immediate action (low overshoot) 1.5 °C pathway and a delayed action (high overshoot) 1.5 °C pathway. Two other key categories are a pathway category approximately in line with current (as expressed by 2023) near- and long-term policy objectives, as well as a higher-emission category that is approximately in line with “current policies” (as expressed by 2023). We also argue for the scientific and policy relevance in exploring two “worlds that could have been”. One of these categories has high-emission trajectories well above what is implied by current policies and the other has very-low-emission trajectories which assume that global mitigation action in line with limiting warming to 1.5 °C without overshoot had begun in 2015. Finally, we note that the timely provision of new scientific information on pathways is critical to inform the development and implementation of climate policy. Under the Paris Agreement, for the second global stocktake, which will occur in 2028, and to inform subsequent development of nationally determined contributions (NDCs) up to 2040, scientific inputs are required by 2027. These needs should be carefully considered in the development timeline of community modelling activities, including those under CMIP7.en_US
dc.language.isoengen_US
dc.publisherCopernicus Publicationsen_US
dc.rightsNavngivelse 4.0 Internasjonal*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no*
dc.titleA perspective on the next generation of Earth system model scenarios: Towards representative emission pathways (REPs)en_US
dc.title.alternativeA perspective on the next generation of Earth system model scenarios: Towards representative emission pathways (REPs)en_US
dc.typePeer revieweden_US
dc.typeJournal articleen_US
dc.description.versionpublishedVersionen_US
dc.source.pagenumber4533-4559en_US
dc.source.volume17en_US
dc.source.journalGeoscientific Model Developmenten_US
dc.source.issue11en_US
dc.identifier.doi10.5194/gmd-17-4533-2024
dc.identifier.cristin2278368
dc.relation.projectEC/H2020/101003687en_US
dc.relation.projectEC/H2020/821003en_US
dc.relation.projectEC/H2020/101056306en_US
dc.relation.projectEC/H2020/101003536en_US
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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