Water scarcity hotspots travel downstream due to human interventions in the 20th and 21st century

dc.bibliographicCitation.firstPage15697eng
dc.bibliographicCitation.journalTitleNature Communicationseng
dc.bibliographicCitation.lastPage2215eng
dc.bibliographicCitation.volume8eng
dc.contributor.authorVeldkamp, T.I.E.
dc.contributor.authorWada, Y.
dc.contributor.authorAerts, J.C.J.H.
dc.contributor.authorDöll, P.
dc.contributor.authorGosling, S.N.
dc.contributor.authorLiu, J.
dc.contributor.authorMasaki, Y.
dc.contributor.authorOki, T.
dc.contributor.authorOstberg, S.
dc.contributor.authorPokhrel, Y.
dc.contributor.authorSatoh, Y.
dc.contributor.authorKim, H.
dc.contributor.authorWard, P.J.
dc.date.accessioned2020-07-27T12:26:36Z
dc.date.available2020-07-27T12:26:36Z
dc.date.issued2017
dc.description.abstractWater scarcity is rapidly increasing in many regions. In a novel, multi-model assessment, we examine how human interventions (HI: land use and land cover change, man-made reservoirs and human water use) affected monthly river water availability and water scarcity over the period 1971-2010. Here we show that HI drastically change the critical dimensions of water scarcity, aggravating water scarcity for 8.8% (7.4-16.5%) of the global population but alleviating it for another 8.3% (6.4-15.8%). Positive impacts of HI mostly occur upstream, whereas HI aggravate water scarcity downstream; HI cause water scarcity to travel downstream. Attribution of water scarcity changes to HI components is complex and varies among the hydrological models. Seasonal variation in impacts and dominant HI components is also substantial. A thorough consideration of the spatially and temporally varying interactions among HI components and of uncertainties is therefore crucial for the success of water scarcity adaptation by HI.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/5161
dc.identifier.urihttps://doi.org/10.34657/3790
dc.language.isoengeng
dc.publisherLondon : Nature Publishing Groupeng
dc.relation.doihttps://doi.org/10.1038/ncomms15697
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc550eng
dc.subject.otherriver watereng
dc.subject.otherwatereng
dc.subject.otheradaptive managementeng
dc.subject.otherenvironmental impact assessmenteng
dc.subject.otherhuman activityeng
dc.subject.otherhydrological modelingeng
dc.subject.otherresource scarcityeng
dc.subject.otherriver watereng
dc.subject.otherseasonal variationeng
dc.subject.othertwentieth centuryeng
dc.subject.othertwenty first centuryeng
dc.subject.otherwater availabilityeng
dc.subject.otherArticleeng
dc.subject.otherclimate changeeng
dc.subject.otherfluid intakeeng
dc.subject.otherhumaneng
dc.subject.otherhydrologyeng
dc.subject.otherland useeng
dc.subject.otherreservoireng
dc.subject.otherseasonal variationeng
dc.subject.othertraveleng
dc.subject.otheruncertaintyeng
dc.subject.otherwater availabilityeng
dc.subject.otherwater scarcityeng
dc.subject.otherwater supplyeng
dc.titleWater scarcity hotspots travel downstream due to human interventions in the 20th and 21st centuryeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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