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Projected Changes and Time of Emergence of Temperature Extremes Over Australia in CMIP5 and CMIP6

dc.contributor.authorDeng, Xuen
dc.contributor.authorPerkins-Kirkpatrick, Sarah E.en
dc.contributor.authorAlexander, Lisa V.en
dc.contributor.authorStark, Clairen
dc.date.accessioned2025-06-11T21:40:32Z
dc.date.available2025-06-11T21:40:32Z
dc.date.issued2022en
dc.description.abstractThis study focuses on the projections and time of emergence (TOE) for temperature extremes over Australian regions in the phase 6 of Coupled Model Intercomparison Project (CMIP6) models. The model outputs are based on the Shared Socioeconomic Pathways (SSPs) from the Tier 1 experiments (i.e., SSP1-2.6, SSP2-4.5, SSP3-7.0, and SSP5-8.5) in the Scenario Model Intercomparison Project (ScenarioMIP), which is compared with the Representative Concentration Pathways (RCPs) in CMIP5 (i.e., RCP2.6, RCP4.5, and RCP8.5). Furthermore, two large ensembles (LEs) in CMIP6 are used to investigate the effects of internal variability on the projected changes and TOE. As shown in the temporal evolution and spatial distribution, the strongest warming levels are projected under the highest future scenario and the changes for some extremes follow a “warm-get-warmer” pattern over Australia. Over subregions, tropical Australia usually shows the highest warming. Compared to the RCPs in CMIP5, the multi-model medians in SSPs are higher for some indices and commonly exhibit wider spreads, likely related to the different forcings and higher climate sensitivity in a subset of the CMIP6 models. Based on a signal-to-noise framework, we confirm that the emergence patterns differ greatly for different extreme indices and the large uncertainty in TOE can result from the inter-model ranges of both signal and noise, for which internal variability contributes to the determination of the signal. We further demonstrate that the internally generated variations influence the noise. Our findings can provide useful information for mitigation strategies and adaptation planning over Australia.en
dc.description.sponsorshipWe acknowledge two reviewers for their helpful comments. We thank Edward Hawkins for valuable suggestions, and appreciate Rachael Isphording for providing the code to create a mask file covering Australia. This research/project was undertaken with the assistance of resources and services from the National Computational Infrastructure (NCI), which is supported by the Australian Government. We thank the World Climate Research Programme's Working Group on Coupled Modelling, which is responsible for CMIP and coordinated CMIP5 and CMIP6. We further acknowledge the climate modeling groups for producing and making available their model output, the Earth System Grid Federation (ESGF) for archiving the data and providing access, and the multiple funding agencies who support CMIP and ESGF. S.E.P‐K. is supported by the Australian Research Council (ARC) grant FT170100106 and the Centre of Excellence for Climate Extremes (CLEX) grant CE170100023. L.V.A. is supported by the ARC grants CE170100023 and FT210100459. We acknowledge two reviewers for their helpful comments. We thank Edward Hawkins for valuable suggestions, and appreciate Rachael Isphording for providing the code to create a mask file covering Australia. This research/project was undertaken with the assistance of resources and services from the National Computational Infrastructure (NCI), which is supported by the Australian Government. We thank the World Climate Research Programme's Working Group on Coupled Modelling, which is responsible for CMIP and coordinated CMIP5 and CMIP6. We further acknowledge the climate modeling groups for producing and making available their model output, the Earth System Grid Federation (ESGF) for archiving the data and providing access, and the multiple funding agencies who support CMIP and ESGF. S.E.P-K. is supported by the Australian Research Council (ARC) grant FT170100106 and the Centre of Excellence for Climate Extremes (CLEX) grant CE170100023. L.V.A. is supported by the ARC grants CE170100023 and FT210100459.en
dc.description.statusPeer-revieweden
dc.format.extent24en
dc.identifier.otherORCID:/0000-0001-9443-4915/work/171154960en
dc.identifier.scopus85139126789en
dc.identifier.urihttp://www.scopus.com/inward/record.url?scp=85139126789&partnerID=8YFLogxKen
dc.identifier.urihttps://hdl.handle.net/1885/733759103
dc.language.isoenen
dc.rightsPublisher Copyright: © 2022. The Authors.en
dc.sourceEarth's Futureen
dc.titleProjected Changes and Time of Emergence of Temperature Extremes Over Australia in CMIP5 and CMIP6en
dc.typeJournal articleen
dspace.entity.typePublicationen
local.contributor.affiliationDeng, Xu; University of New South Walesen
local.contributor.affiliationPerkins-Kirkpatrick, Sarah E.; University of New South Walesen
local.contributor.affiliationAlexander, Lisa V.; University of New South Walesen
local.contributor.affiliationStark, Clair; University of New South Walesen
local.identifier.citationvolume10en
local.identifier.doi10.1029/2021EF002645en
local.identifier.pure475f5fe0-6779-4b61-ab95-ab6127b9ff02en
local.identifier.urlhttps://www.scopus.com/pages/publications/85139126789en
local.type.statusPublisheden

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