Please use this identifier to cite or link to this item: http://doi.org/10.25358/openscience-9986
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dc.contributor.authorTorbenson, Max C. A.-
dc.contributor.authorStahle, David W.-
dc.contributor.authorHoward, Ian M.-
dc.contributor.authorBlackstock, Joshua M.-
dc.contributor.authorCleaveland, Malcolm K.-
dc.contributor.authorStagge, James H.-
dc.date.accessioned2024-01-26T10:10:43Z-
dc.date.available2024-01-26T10:10:43Z-
dc.date.issued2023-
dc.identifier.urihttps://openscience.ub.uni-mainz.de/handle/20.500.12030/10004-
dc.description.abstractWe present four reconstruction estimates of Arkansas River baseflow and streamflow using a total of 78 tree-ring chronologies for three streamflow gages, geographically spanning the headwaters in Colorado to near the confluence of the Arkansas-Mississippi rivers. The estimates represent different seasonal windows, which are dictated by the shared limiting forcing of precipitation on seasonal tree growth and soil moisture—and subsequently on the variability of Arkansas River discharge. Flow extremes that were higher and lower than what has been observed in the instrumental era are recorded in each of the four reconstructions. Years of concurrent, cross-basin (all sites) low flow appear more frequently during the 20th and 21st Centuries compared to any period since 1600 A.D., however, no significant trend in cross-basin low flow is observed. As the most downstream major tributary of the Mississippi River, the Arkansas River directly influences flood risk in the Lower Mississippi River Valley. Estimates of extreme high flow in downstream reconstructions coincide with specific years of historic flooding documented in New Orleans, Louisiana, just upstream of the Mississippi River Delta. By deduction, Mississippi River flooding in years of low Arkansas River flow imply exceptional flooding contributions from the Upper Mississippi River catchments.en_GB
dc.language.isoengde
dc.rightsCC BY-NC-ND*
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/*
dc.subject.ddc550 Geowissenschaftende_DE
dc.subject.ddc550 Earth sciencesen_GB
dc.titlePre-instrumental perspectives on Arkansas River cross-watershed flow variabilityen_GB
dc.typeZeitschriftenaufsatzde
dc.identifier.doihttp://doi.org/10.25358/openscience-9986-
jgu.type.contenttypeScientific articlede
jgu.type.dinitypearticleen_GB
jgu.type.versionPublished versionde
jgu.type.resourceTextde
jgu.organisation.departmentFB 09 Chemie, Pharmazie u. Geowissensch.de
jgu.organisation.number7950-
jgu.organisation.nameJohannes Gutenberg-Universität Mainz-
jgu.rights.accessrightsopenAccess-
jgu.journal.titleJournal of the American Water Resources Associationde
jgu.journal.volume59de
jgu.journal.issue1de
jgu.pages.start1de
jgu.pages.end15de
jgu.publisher.year2023-
jgu.publisher.nameWiley-Blackwellde
jgu.publisher.placeHoboken, NJde
jgu.publisher.issn1093-474Xde
jgu.organisation.placeMainz-
jgu.subject.ddccode550de
dc.date.updated2023-11-13T08:55:56Z-
jgu.publisher.doi10.1111/1752-1688.13068de
elements.object.id148980-
elements.object.labelspaleoclimatology-
elements.object.labelstree rings-
elements.object.labelsflow separation-
elements.object.labelsextremes-
elements.object.labels0406 Physical Geography and Environmental Geoscience-
elements.object.labels0905 Civil Engineering-
elements.object.labels0907 Environmental Engineering-
elements.object.labelsEnvironmental Engineering-
elements.object.labels37 Earth sciences-
elements.object.labels40 Engineering-
elements.object.typejournal-article-
jgu.organisation.rorhttps://ror.org/023b0x485-
Appears in collections:JGU-Publikationen

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