Reduced Complexity Model Intercomparison Project Phase 2: Synthesizing Earth System Knowledge for Probabilistic Climate Projections

dc.bibliographicCitation.firstPagee2020EF001900eng
dc.bibliographicCitation.issue6eng
dc.bibliographicCitation.volume9eng
dc.contributor.authorNicholls, Z.
dc.contributor.authorMeinshausen, M.
dc.contributor.authorLewis, J.
dc.contributor.authorCorradi, M. Rojas
dc.contributor.authorDorheim, K.
dc.contributor.authorGasser, T.
dc.contributor.authorGieseke, R.
dc.contributor.authorHope, A.P.
dc.contributor.authorLeach, N.J.
dc.contributor.authorMcBride, L.A.
dc.contributor.authorQuilcaille, Y.
dc.contributor.authorRogelj, J.
dc.contributor.authorSalawitch, R.J.
dc.contributor.authorSamset, B.H.
dc.contributor.authorSandstad, M.
dc.contributor.authorShiklomanov, A.
dc.contributor.authorSkeie, R.B.
dc.contributor.authorSmith, C.J.
dc.contributor.authorSmith, S.J.
dc.contributor.authorSu, X.
dc.contributor.authorTsutsui, J.
dc.contributor.authorVega-Westhoff, B.
dc.contributor.authorWoodard, D.L.
dc.date.accessioned2022-01-19T10:58:29Z
dc.date.available2022-01-19T10:58:29Z
dc.date.issued2021
dc.description.abstractOver the last decades, climate science has evolved rapidly across multiple expert domains. Our best tools to capture state-of-the-art knowledge in an internally self-consistent modeling framework are the increasingly complex fully coupled Earth System Models (ESMs). However, computational limitations and the structural rigidity of ESMs mean that the full range of uncertainties across multiple domains are difficult to capture with ESMs alone. The tools of choice are instead more computationally efficient reduced complexity models (RCMs), which are structurally flexible and can span the response dynamics across a range of domain-specific models and ESM experiments. Here we present Phase 2 of the Reduced Complexity Model Intercomparison Project (RCMIP Phase 2), the first comprehensive intercomparison of RCMs that are probabilistically calibrated with key benchmark ranges from specialized research communities. Unsurprisingly, but crucially, we find that models which have been constrained to reflect the key benchmarks better reflect the key benchmarks. Under the low-emissions SSP1-1.9 scenario, across the RCMs, median peak warming projections range from 1.3 to 1.7°C (relative to 1850-1900, using an observationally based historical warming estimate of 0.8°C between 1850-1900 and 1995-2014). Further developing methodologies to constrain these projection uncertainties seems paramount given the international community's goal to contain warming to below 1.5°C above preindustrial in the long-term. Our findings suggest that users of RCMs should carefully evaluate their RCM, specifically its skill against key benchmarks and consider the need to include projections benchmarks either from ESM results or other assessments to reduce divergence in future projections.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/7851
dc.identifier.urihttps://doi.org/10.34657/6892
dc.language.isoengeng
dc.publisherHoboken, NJ : Wiley-Blackwelleng
dc.relation.doihttps://doi.org/10.1029/2020EF001900
dc.relation.essn2328-4277
dc.relation.ispartofseriesEarth's future 9 (2021), Nr. 6eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectclimateeng
dc.subjectmodel intercomparisoneng
dc.subjectprobabilistic projectionseng
dc.subjectRCMIPeng
dc.subjectreduced complexity climate modeleng
dc.subject.ddc550eng
dc.titleReduced Complexity Model Intercomparison Project Phase 2: Synthesizing Earth System Knowledge for Probabilistic Climate Projectionseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleEarth's futureeng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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