Matches in SemOpenAlex for { <https://semopenalex.org/work/W2330453050> ?p ?o ?g. }
- W2330453050 endingPage "265" @default.
- W2330453050 startingPage "251" @default.
- W2330453050 abstract "CR Climate Research Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsSpecials CR 62:251-265 (2015) - DOI: https://doi.org/10.3354/cr01276 Climate projections for southern Australian cool-season rainfall: insights from a downscaling comparison Michael R. Grose1,*, Aurel F. Moise2, Bertrand Timbal2, Jack J. Katzfey1, Marie Ekström3, Penny H. Whetton1 1Climate Adaptation Flagship, CSIRO Marine and Atmospheric Research, 107-121 Station St, Aspendale, VIC 3195, Australia 2Centre for Australian Weather and Climate Research, Bureau of Meteorology, GPO Box 1289, Melbourne, VIC 3001, Australia 3CSIRO Land and Water, PO Box 1666, Canberra ACT 2601, Australia *Corresponding author: michael.grose@csiro.au ABSTRACT: The projected drying of the extra-tropics under a warmer climate has large implications for natural systems and water security in southern Australia. The downscaling of global climate models can provide insight into regional patterns of rainfall change in the mid-latitudes in the typically wetter cool season. The comparison of statistical and dynamical downscaling model outputs reveals regions of consistent potential added value in the climate-change signal over the 21st century that are largely related to finer resolution. These differences include a stronger and more regionalised rainfall decrease on west coasts in response to a shift in westerly circulation and a different response further from the coast where other influences are important. These patterns have a plausible relationship with topography and regional drivers that are not resolved by coarse global models. However, the comparison of statistical and dynamical downscaling reveals where the method and the configuration of each method makes a difference to the projection. This is an important source of uncertainty for regional rainfall projections. In particular, the simulated change in atmospheric circulation over the century is different in the dynamical downscaling compared to the global climate model inputs, related in part to a different response to patterns of surface warming. The dynamical downscaling places the border between regions with rainfall increase and decrease further north in winter and spring compared to the global climate models and therefore has a different rainfall projection for southeast mainland Australia in winter and for Tasmania in spring. KEY WORDS: Downscaling · Regional climate models · Precipitation · Climate projections Full text in pdf format PreviousCite this article as: Grose MR, Moise AF, Timbal B, Katzfey JJ, Ekström M, Whetton PH (2015) Climate projections for southern Australian cool-season rainfall: insights from a downscaling comparison. Clim Res 62:251-265. https://doi.org/10.3354/cr01276 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in CR Vol. 62, No. 3. Online publication date: February 26, 2015 Print ISSN: 0936-577X; Online ISSN: 1616-1572 Copyright © 2015 Inter-Research." @default.
- W2330453050 created "2016-06-24" @default.
- W2330453050 creator A5020270379 @default.
- W2330453050 creator A5031597916 @default.
- W2330453050 creator A5040534407 @default.
- W2330453050 creator A5052438161 @default.
- W2330453050 creator A5066848880 @default.
- W2330453050 creator A5068199624 @default.
- W2330453050 date "2015-02-26" @default.
- W2330453050 modified "2023-09-27" @default.
- W2330453050 title "Climate projections for southern Australian cool-season rainfall: insights from a downscaling comparison" @default.
- W2330453050 cites W1583121184 @default.
- W2330453050 cites W174598607 @default.
- W2330453050 cites W1940804098 @default.
- W2330453050 cites W1969753629 @default.
- W2330453050 cites W1972946271 @default.
- W2330453050 cites W1972974564 @default.
- W2330453050 cites W1985869031 @default.
- W2330453050 cites W1996629671 @default.
- W2330453050 cites W2000818058 @default.
- W2330453050 cites W2001318089 @default.
- W2330453050 cites W2001944101 @default.
- W2330453050 cites W2009902605 @default.
- W2330453050 cites W2014953946 @default.
- W2330453050 cites W2030223774 @default.
- W2330453050 cites W2039322240 @default.
- W2330453050 cites W2048667284 @default.
- W2330453050 cites W2058977482 @default.
- W2330453050 cites W2061272784 @default.
- W2330453050 cites W2062217294 @default.
- W2330453050 cites W2066242004 @default.
- W2330453050 cites W2079269412 @default.
- W2330453050 cites W2082574912 @default.
- W2330453050 cites W2082666236 @default.
- W2330453050 cites W2084711589 @default.
- W2330453050 cites W2092128325 @default.
- W2330453050 cites W2093141926 @default.
- W2330453050 cites W2095779753 @default.
- W2330453050 cites W2097403132 @default.
- W2330453050 cites W2102145495 @default.
- W2330453050 cites W2121745948 @default.
- W2330453050 cites W2121879697 @default.
- W2330453050 cites W2131912939 @default.
- W2330453050 cites W2133575566 @default.
- W2330453050 cites W2142463025 @default.
- W2330453050 cites W2156909167 @default.
- W2330453050 cites W2168193659 @default.
- W2330453050 cites W2172191993 @default.
- W2330453050 cites W2324750235 @default.
- W2330453050 doi "https://doi.org/10.3354/cr01276" @default.
- W2330453050 hasPublicationYear "2015" @default.
- W2330453050 type Work @default.
- W2330453050 sameAs 2330453050 @default.
- W2330453050 citedByCount "12" @default.
- W2330453050 countsByYear W23304530502015 @default.
- W2330453050 countsByYear W23304530502016 @default.
- W2330453050 countsByYear W23304530502017 @default.
- W2330453050 countsByYear W23304530502018 @default.
- W2330453050 countsByYear W23304530502020 @default.
- W2330453050 crossrefType "journal-article" @default.
- W2330453050 hasAuthorship W2330453050A5020270379 @default.
- W2330453050 hasAuthorship W2330453050A5031597916 @default.
- W2330453050 hasAuthorship W2330453050A5040534407 @default.
- W2330453050 hasAuthorship W2330453050A5052438161 @default.
- W2330453050 hasAuthorship W2330453050A5066848880 @default.
- W2330453050 hasAuthorship W2330453050A5068199624 @default.
- W2330453050 hasBestOaLocation W23304530501 @default.
- W2330453050 hasConcept C111368507 @default.
- W2330453050 hasConcept C122523270 @default.
- W2330453050 hasConcept C127313418 @default.
- W2330453050 hasConcept C132651083 @default.
- W2330453050 hasConcept C13280743 @default.
- W2330453050 hasConcept C141452985 @default.
- W2330453050 hasConcept C168754636 @default.
- W2330453050 hasConcept C205649164 @default.
- W2330453050 hasConcept C39432304 @default.
- W2330453050 hasConcept C41156917 @default.
- W2330453050 hasConcept C49204034 @default.
- W2330453050 hasConceptScore W2330453050C111368507 @default.
- W2330453050 hasConceptScore W2330453050C122523270 @default.
- W2330453050 hasConceptScore W2330453050C127313418 @default.
- W2330453050 hasConceptScore W2330453050C132651083 @default.
- W2330453050 hasConceptScore W2330453050C13280743 @default.
- W2330453050 hasConceptScore W2330453050C141452985 @default.
- W2330453050 hasConceptScore W2330453050C168754636 @default.
- W2330453050 hasConceptScore W2330453050C205649164 @default.
- W2330453050 hasConceptScore W2330453050C39432304 @default.
- W2330453050 hasConceptScore W2330453050C41156917 @default.
- W2330453050 hasConceptScore W2330453050C49204034 @default.
- W2330453050 hasIssue "3" @default.
- W2330453050 hasLocation W23304530501 @default.
- W2330453050 hasOpenAccess W2330453050 @default.
- W2330453050 hasPrimaryLocation W23304530501 @default.
- W2330453050 hasRelatedWork W1806772866 @default.
- W2330453050 hasRelatedWork W2012923864 @default.
- W2330453050 hasRelatedWork W2015475130 @default.
- W2330453050 hasRelatedWork W2038909984 @default.
- W2330453050 hasRelatedWork W2096043785 @default.