Adaptation required to preserve future high-end river flood risk at present levels

dc.bibliographicCitation.firstPageeaao1914eng
dc.bibliographicCitation.issue1eng
dc.bibliographicCitation.volume4eng
dc.contributor.authorWillner, S.N.
dc.contributor.authorLevermann, A.
dc.contributor.authorZhao, F.
dc.contributor.authorFrieler, K.
dc.date.accessioned2020-07-27T12:26:33Z
dc.date.available2020-07-27T12:26:33Z
dc.date.issued2018
dc.description.abstractEarth’s surface temperature will continue to rise for another 20 to 30 years even with the strongest carbon emission reduction currently considered. The associated changes in rainfall patterns can result in an increased flood risk worldwide. We compute the required increase in flood protection to keep high-end fluvial flood risk at present levels. The analysis is carried out worldwide for subnational administrative units. Most of the United States, Central Europe, and Northeast and West Africa, as well as large parts of India and Indonesia, require the strongest adaptation effort. More than half of the United States needs to at least double their protection within the next two decades. Thus, the need for adaptation to increased river flood is a global problem affecting industrialized regions as much as developing countries.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/5144
dc.identifier.urihttps://doi.org/10.34657/3773
dc.language.isoengeng
dc.publisherWashington : American Association for the Advancement of Science (A A A S)eng
dc.relation.doihttps://doi.org/10.1126/sciadv.aao1914
dc.relation.ispartofseriesScience Advances 4 (2018), Nr. 1eng
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subjectCarboneng
dc.subjectDeveloping countrieseng
dc.subjectEmission controleng
dc.subjectFlood controleng
dc.subjectCarbon emission reductionseng
dc.subjectCentral Europeeng
dc.subjectFlood protectioneng
dc.subjectGlobal problemseng
dc.subjectRainfall patternseng
dc.subjectRiver floodseng
dc.subjectSurface temperatureseng
dc.subjectWest Africaeng
dc.subjectFloodseng
dc.subject.ddc550eng
dc.titleAdaptation required to preserve future high-end river flood risk at present levelseng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleScience Advanceseng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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