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dc.contributor.authorRehfeld, Kira
dc.contributor.authorHébert, Raphaël
dc.contributor.authorLora, Juan M.
dc.contributor.authorLofverstrom, Marcus
dc.contributor.authorBrierley, Chris M.
dc.date.accessioned2020-07-20T19:08:26Z
dc.date.available2020-07-20T19:08:26Z
dc.date.issued2020-05-25
dc.identifier.citationRehfeld, K., Hébert, R., Lora, J. M., Lofverstrom, M., and Brierley, C. M.: Variability of surface climate in simulations of past and future, Earth Syst. Dynam., 11, 447–468, https://doi.org/10.5194/esd-11-447-2020, 2020.en_US
dc.identifier.issn2190-4979
dc.identifier.doi10.5194/esd-11-447-2020
dc.identifier.urihttp://hdl.handle.net/10150/641899
dc.description.abstractIt is virtually certain that the mean surface temperature of the Earth will continue to increase under realistic emission scenarios, yet comparatively little is known about future changes in climate variability. This study explores changes in climate variability over the large range of climates simulated by the Coupled Model Intercomparison Project Phase 5 and 6 (CMIP5/6) and the Paleoclimate Modeling Intercomparison Project Phase 3 (PMIP3), including time slices of the Last Glacial Maximum, the mid-Holocene, and idealized experiments (1 % CO2 and abrupt4 x CO2). These states encompass climates within a range of 12 degrees C in global mean temperature change. We examine climate variability from the perspectives of local interannual change, coherent climate modes, and through compositing extremes. The change in the interannual variability of precipitation is strongly dependent upon the local change in the total amount of precipitation. At the global scale, temperature variability is inversely related to mean temperature change on intra-seasonal to multidecadal timescales. This decrease is stronger over the oceans, while there is increased temperature variability over subtropical land areas (40 degrees S-40 degrees N) in warmer simulations. We systematically investigate changes in the standard deviation of modes of climate variability, including the North Atlantic Oscillation, the El Niflo-Southern Oscillation, and the Southern Annular Mode, with global mean temperature change. While several climate modes do show consistent relationships (most notably the Atlantic Zonal Mode), no generalizable pattern emerges. By compositing extreme precipitation years across the ensemble, we demonstrate that the same large-scale modes influencing rainfall variability in Mediterranean climates persist throughout paleoclimate and future simulations. The robust nature of the response of climate variability, between cold and warm climates as well as across multiple timescales, suggests that observations and proxy reconstructions could provide a meaningful constraint on climate variability in future projections.en_US
dc.language.isoenen_US
dc.publisherCOPERNICUS GESELLSCHAFT MBHen_US
dc.rightsCopyright © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.en_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/en_US
dc.titleVariability of surface climate in simulations of past and futureen_US
dc.typeArticleen_US
dc.contributor.departmentUniv Arizona, Dept Geoscien_US
dc.identifier.journalEARTH SYSTEM DYNAMICSen_US
dc.description.noteOpen access journalen_US
dc.description.collectioninformationThis item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.en_US
dc.eprint.versionFinal published versionen_US
dc.source.journaltitleEarth System Dynamics
dc.source.volume11
dc.source.issue2
dc.source.beginpage447
dc.source.endpage468
refterms.dateFOA2020-07-20T19:08:27Z


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Copyright © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.
Except where otherwise noted, this item's license is described as Copyright © Author(s) 2020. This work is distributed under the Creative Commons Attribution 4.0 License.