Possible future changes in South East Australian frost frequency: an inter-comparison of statistical downscaling approaches

dc.contributor.authorCrimp, Steven
dc.contributor.authorJin, Huidong
dc.contributor.authorKokic, Philip
dc.contributor.authorBakar, Khandoker (Shuvo)
dc.contributor.authorNicholls, Neville
dc.date.accessioned2021-01-14T02:43:42Z
dc.date.issued2018
dc.date.updated2020-11-02T04:18:45Z
dc.description.abstractAnthropogenic climate change has already been shown to effect the frequency, intensity, spatial extent, duration and seasonality of extreme climate events. Understanding these changes is an important step in determining exposure, vulnerability and focus for adaptation. In an attempt to support adaptation decision-making we have examined statistical modelling techniques to improve the representation of global climate model (GCM) derived projections of minimum temperature extremes (frosts) in Australia. We examine the spatial changes in minimum temperature extreme metrics (e.g. monthly and seasonal frost frequency etc.), for a region exhibiting the strongest station trends in Australia, and compare these changes with minimum temperature extreme metrics derived from 10 GCMs, from the Coupled Model Inter-comparison Project Phase 5 (CMIP 5) datasets, and via statistical downscaling. We compare the observed trends with those derived from the “raw” GCM minimum temperature data as well as examine whether quantile matching (QM) or spatio-temporal (spTimerQM) modelling with Quantile Matching can be used to improve the correlation between observed and simulated extreme minimum temperatures. We demonstrate, that the spTimerQM modelling approach provides correlations with observed daily minimum temperatures for the period August to November of 0.22. This represents an almost fourfold improvement over either the “raw” GCM or QM results. The spTimerQM modelling approach also improves correlations with observed monthly frost frequency statistics to 0.84 as opposed to 0.37 and 0.81 for the “raw” GCM and QM results respectively. We apply the spatio-temporal model to examine future extreme minimum temperature projections for the period 2016 to 2048. The spTimerQM modelling results suggest the persistence of current levels of frost risk out to 2030, with the evidence of continuing decadal variation.en_AU
dc.description.sponsorshipthis research was made possible via financial support from the Australian Grains Research and Development Corporation (GRDCen_AU
dc.format.mimetypeapplication/pdfen_AU
dc.identifier.issn0930-7575en_AU
dc.identifier.urihttp://hdl.handle.net/1885/219357
dc.language.isoen_AUen_AU
dc.publisherSpringeren_AU
dc.rights© Springer-Verlag GmbH Germany, part of Springer Nature 2018en_AU
dc.sourceClimate Dynamicsen_AU
dc.subjectFrosten_AU
dc.subjectDaily minimum temperaturesen_AU
dc.subjectSpatio-temporal modellingen_AU
dc.subjectQuantile matchingen_AU
dc.subjectFuture projectionsen_AU
dc.titlePossible future changes in South East Australian frost frequency: an inter-comparison of statistical downscaling approachesen_AU
dc.typeJournal articleen_AU
local.bibliographicCitation.issue1-2en_AU
local.contributor.affiliationCrimp, Steven, College of Science, ANUen_AU
local.contributor.affiliationJin, Huidong, CSIRO Division of Mathematical and Information Sciencesen_AU
local.contributor.affiliationKokic, Philip, College of Science, ANUen_AU
local.contributor.affiliationBakar, Khandoker (Shuvo), College of Arts and Social Sciences, ANUen_AU
local.contributor.affiliationNicholls, Neville, Monash Universityen_AU
local.contributor.authoremailu1048596@anu.edu.auen_AU
local.contributor.authoruidCrimp, Steven, u1048596en_AU
local.contributor.authoruidKokic, Philip, a242749en_AU
local.contributor.authoruidBakar, Khandoker (Shuvo), u1011434en_AU
local.description.embargo2099-12-31
local.description.notesImported from ARIESen_AU
local.identifier.absfor040105 - Climatology (excl. Climate Change Processes)en_AU
local.identifier.absseo960399 - Climate and Climate Change not elsewhere classifieden_AU
local.identifier.ariespublicationa383154xPUB9690en_AU
local.identifier.citationvolume52en_AU
local.identifier.doi10.1007/s00382-018-4188-1en_AU
local.identifier.scopusID2-s2.0-85044939025
local.identifier.uidSubmittedBya383154en_AU
local.type.statusPublished Versionen_AU

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