Comparing impacts of climate change on streamflow in four large African river basins

dc.bibliographicCitation.firstPage1305eng
dc.bibliographicCitation.issue4eng
dc.bibliographicCitation.journalTitleHydrology and Earth System Scienceseng
dc.bibliographicCitation.volume18eng
dc.contributor.authorAich, V.
dc.contributor.authorLiersch, S.
dc.contributor.authorVetter, T.
dc.contributor.authorHuang, S.
dc.contributor.authorTecklenburg, J.
dc.contributor.authorHoffmann, P.
dc.contributor.authorKoch, H.
dc.contributor.authorFournet, S.
dc.contributor.authorKrysanova, V.
dc.contributor.authorMüller, E.N.
dc.contributor.authorHattermann, F.F.
dc.date.accessioned2020-08-01T15:36:10Z
dc.date.available2020-08-01T15:36:10Z
dc.date.issued2014
dc.description.abstractThis study aims to compare impacts of climate change on streamflow in four large representative African river basins: the Niger, the Upper Blue Nile, the Oubangui and the Limpopo. We set up the eco-hydrological model SWIM (Soil and Water Integrated Model) for all four basins individually. The validation of the models for four basins shows results from adequate to very good, depending on the quality and availability of input and calibration data. <br><br> For the climate impact assessment, we drive the model with outputs of five bias corrected Earth system models of Coupled Model Intercomparison Project Phase 5 (CMIP5) for the representative concentration pathways (RCPs) 2.6 and 8.5. This climate input is put into the context of climate trends of the whole African continent and compared to a CMIP5 ensemble of 19 models in order to test their representativeness. Subsequently, we compare the trends in mean discharges, seasonality and hydrological extremes in the 21st century. The uncertainty of results for all basins is high. Still, climate change impact is clearly visible for mean discharges but also for extremes in high and low flows. The uncertainty of the projections is the lowest in the Upper Blue Nile, where an increase in streamflow is most likely. In the Niger and the Limpopo basins, the magnitude of trends in both directions is high and has a wide range of uncertainty. In the Oubangui, impacts are the least significant. Our results confirm partly the findings of previous continental impact analyses for Africa. However, contradictory to these studies we find a tendency for increased streamflows in three of the four basins (not for the Oubangui). Guided by these results, we argue for attention to the possible risks of increasing high flows in the face of the dominant water scarcity in Africa. In conclusion, the study shows that impact intercomparisons have added value to the adaptation discussion and may be used for setting up adaptation plans in the context of a holistic approach.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/5279
dc.identifier.urihttps://doi.org/10.34657/3908
dc.language.isoengeng
dc.publisherGöttingen : Copernicus GmbHeng
dc.relation.doihttps://doi.org/10.5194/hess-18-1305-2014
dc.relation.issn1027-5606
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subject.ddc550eng
dc.subject.otherClimate changeeng
dc.subject.otherDigital storageeng
dc.subject.otherEarth (planet)eng
dc.subject.otherStream floweng
dc.subject.otherWatershedseng
dc.subject.otherClimate change impacteng
dc.subject.otherClimate impact assessmenteng
dc.subject.otherCoupled Model Intercomparison Projecteng
dc.subject.otherEarth system modeleng
dc.subject.otherEco-hydrological modelseng
dc.subject.otherHolistic approacheng
dc.subject.otherHydrological extremeseng
dc.subject.otherIntegrated modelingeng
dc.subject.otherClimate modelseng
dc.subject.otherclimate changeeng
dc.subject.otherclimate effecteng
dc.subject.othercomparative studyeng
dc.subject.othermodel validationeng
dc.subject.otherriver basineng
dc.subject.otherstreamfloweng
dc.subject.othertwenty first centuryeng
dc.subject.otherAfricaeng
dc.titleComparing impacts of climate change on streamflow in four large African river basinseng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorPIKeng
wgl.subjectUmweltwissenschafteneng
wgl.typeZeitschriftenartikeleng
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