Please use this identifier to cite or link to this item: http://dx.doi.org/10.18419/opus-11225
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dc.contributor.authorRiegger, Johannes-
dc.date.accessioned2021-01-13T15:34:24Z-
dc.date.available2021-01-13T15:34:24Z-
dc.date.issued2020de
dc.identifier.issn1607-7938-
dc.identifier.issn1027-5606-
dc.identifier.other1744777632-
dc.identifier.urihttp://elib.uni-stuttgart.de/handle/11682/11242-
dc.identifier.urihttp://nbn-resolving.de/urn:nbn:de:bsz:93-opus-ds-112426de
dc.identifier.urihttp://dx.doi.org/10.18419/opus-11225-
dc.description.abstractThe combined use of GRACE mass anomalies and observed river discharge for the first time allows us to quantify the water storage volumes drainable by gravity on global scales. Modelling of catchment and river network storages in a cascade with different dynamics reveals the time lag between total mass and runoff is caused by a non-zero river network storage. This allows catchment and river network storage volumes to be distinguished and is thus of great importance for water resources management.en
dc.language.isoende
dc.relation.uridoi:10.5194/hess-24-1447-2020de
dc.rightsinfo:eu-repo/semantics/openAccessde
dc.subject.ddc620de
dc.subject.ddc624de
dc.titleQuantification of drainable water storage volumes on landmasses and in river networks based on GRACE and river runoff using a cascaded storage approach - first application on the Amazonen
dc.typearticlede
ubs.fakultaetBau- und Umweltingenieurwissenschaftende
ubs.institutInstitut für Wasser- und Umweltsystemmodellierungde
ubs.publikation.seiten1447-1465de
ubs.publikation.sourceHydrology and earth system sciences 24 (2020), pp. 1447-1465de
ubs.publikation.typZeitschriftenartikelde
Appears in Collections:02 Fakultät Bau- und Umweltingenieurwissenschaften

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