Flood risk and climate change: global and regional perspectives

dc.bibliographicCitation.firstPage1eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.journalTitleHydrological Sciences Journaleng
dc.bibliographicCitation.volume59eng
dc.contributor.authorKundzewicz, Z.W.
dc.contributor.authorKanae, S.
dc.contributor.authorSeneviratne, S.I.
dc.contributor.authorHandmer, J.
dc.contributor.authorNicholls, N.
dc.contributor.authorPeduzzi, P.
dc.contributor.authorMechler, R.
dc.contributor.authorBouwer, L.M.
dc.contributor.authorArnell, N.
dc.contributor.authorMach, K.
dc.contributor.authorMuir-Wood, R.
dc.contributor.authorBrakenridge, G.R.
dc.contributor.authorKron, W.
dc.contributor.authorBenito, G.
dc.contributor.authorHonda, Y.
dc.contributor.authorTakahashi, K.
dc.contributor.authorSherstyukov, B.
dc.date.accessioned2020-11-20T17:21:08Z
dc.date.available2020-11-20T17:21:08Z
dc.date.issued2014
dc.description.abstractA holistic perspective on changing rainfall-driven flood risk is provided for the late 20th and early 21st centuries. Economic losses from floods have greatly increased, principally driven by the expanding exposure of assets at risk. It has not been possible to attribute rain-generated peak streamflow trends to anthropogenic climate change over the past several decades. Projected increases in the frequency and intensity of heavy rainfall, based on climate models, should contribute to increases in precipitation-generated local flooding (e.g. flash flooding and urban flooding). This article assesses the literature included in the IPCC SREX report and new literature published since, and includes an assessment of changes in flood risk in seven of the regions considered in the recent IPCC SREX report-Africa, Asia, Central and South America, Europe, North America, Oceania and Polar regions. Also considering newer publications, this article is consistent with the recent IPCC SREX assessment finding that the impacts of climate change on flood characteristics are highly sensitive to the detailed nature of those changes and that presently we have only low confidence1 in numerical projections of changes in flood magnitude or frequency resulting from climate change.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://doi.org/10.34657/4580
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/5951
dc.language.isoengeng
dc.publisherMilton Park : Taylor and Francis Ltd.eng
dc.relation.doihttps://doi.org/10.1080/02626667.2013.857411
dc.relation.issn0262-6667
dc.rights.licenseNon-commercial re-use, distribution, and reproduction in any medium, provided the original work is properly attributed, cited, and is not altered, transformed, or built upon in any way, is permittedeng
dc.subject.ddc550eng
dc.subject.otherattributioneng
dc.subject.otherclimate changeeng
dc.subject.otherfloodseng
dc.subject.otherglobal changeeng
dc.subject.otheruncertaintyeng
dc.subject.otherClimate changeeng
dc.subject.otherLosseseng
dc.subject.otherRaineng
dc.subject.otherAnthropogenic climate changeseng
dc.subject.otherattributioneng
dc.subject.otherFlash floodingeng
dc.subject.otherFlood characteristicseng
dc.subject.otherFlood magnitudeseng
dc.subject.otherGlobal changeeng
dc.subject.otherHolistic perspectiveseng
dc.subject.otheruncertaintyeng
dc.subject.otherFloodseng
dc.subject.otherclimate changeeng
dc.subject.otherfloodeng
dc.subject.otherglobal changeeng
dc.subject.otherpeak floweng
dc.subject.otherpolar regioneng
dc.subject.otherprecipitation (climatology)eng
dc.subject.otherrainfalleng
dc.subject.otherrisk assessmenteng
dc.subject.otherstreamfloweng
dc.subject.otheruncertainty analysiseng
dc.subject.otherAfricaeng
dc.subject.otherAsiaeng
dc.subject.otherCentral Americaeng
dc.subject.otherEuropeeng
dc.subject.otherNorth Americaeng
dc.subject.otherSouth Americaeng
dc.titleFlood risk and climate change: global and regional perspectiveseng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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