Freshwater resources under success and failure of the Paris climate agreement

dc.bibliographicCitation.firstPage205eng
dc.bibliographicCitation.issue2eng
dc.bibliographicCitation.journalTitleEarth System Dynamics : ESDeng
dc.bibliographicCitation.lastPage217eng
dc.bibliographicCitation.volume10eng
dc.contributor.authorHeinke, Jens
dc.contributor.authorMüller, Christoph
dc.contributor.authorLannerstad, Mats
dc.contributor.authorGerten, Dieter
dc.contributor.authorLucht, Wolfgang
dc.date.accessioned2021-09-29T04:52:52Z
dc.date.available2021-09-29T04:52:52Z
dc.date.issued2019
dc.description.abstractPopulation growth will in many regions increase the pressure on water resources and likely increase the number of people affected by water scarcity. In parallel, global warming causes hydrological changes which will affect freshwater supply for human use in many regions. This study estimates the exposure of future population to severe hydrological changes relevant from a freshwater resource perspective at different levels of global mean temperature rise above pre-industrial level (ΔTglob). The analysis is complemented by an assessment of water scarcity that would occur without additional climate change due to population change alone; this is done to identify the population groups that are faced with particularly high adaptation challenges. The results are analysed in the context of success and failure of implementing the Paris Agreement to evaluate how climate mitigation can reduce the future number of people exposed to severe hydrological change. The results show that without climate mitigation efforts, in the year 2100 about 4.9 billion people in the SSP2 population scenario would more likely than not be exposed to severe hydrological change, and about 2.1 billion of them would be faced with particularly high adaptation challenges due to already prevailing water scarcity. Limiting warming to 2 °C by a successful implementation of the Paris Agreement would strongly reduce these numbers to 615 million and 290 million, respectively. At the regional scale, substantial water-related risks remain at 2 °C, with more than 12% of the population exposed to severe hydrological change and high adaptation challenges in Latin America and the Middle East and north Africa region. Constraining δTglob to 1.5 °C would limit this share to about 5% in these regions. ©2019 Author(s).eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/6930
dc.identifier.urihttps://doi.org/10.34657/5977
dc.language.isoengeng
dc.publisherGöttingen : Copernicus Publ.eng
dc.relation.doihttps://doi.org/10.5194/esd-10-205-2019
dc.relation.essn2190-4987
dc.relation.issn2190-4979
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.otherFailure (mechanical)eng
dc.subject.otherGlobal warmingeng
dc.subject.otherWatereng
dc.subject.otherWater resourceseng
dc.subject.otherClimate agreementeng
dc.subject.otherClimate mitigationseng
dc.subject.otherFresh water resourceseng
dc.subject.otherFreshwater supplyeng
dc.subject.otherGlobal-mean temperatureeng
dc.subject.otherHydrological changeseng
dc.subject.otherMiddle East and North Africaeng
dc.subject.otherPre-industrial levelseng
dc.subject.otherPopulation statisticseng
dc.subject.otherclimate changeeng
dc.subject.otherenvironmental policyeng
dc.subject.otherfreshwatereng
dc.subject.otherglobal warmingeng
dc.subject.otherpolicy implementationeng
dc.subject.otherresource assessmenteng
dc.subject.otherresource scarcityeng
dc.subject.otherwater resourceeng
dc.subject.otherwater supplyeng
dc.subject.otherLatin Americaeng
dc.subject.otherMiddle Easteng
dc.subject.otherNorth Africaeng
dc.titleFreshwater resources under success and failure of the Paris climate agreementeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
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