Fluviomorphic trajectories for dryland ephemeral stream channels following extreme flash floods

dc.contributor.authorLotsari Eliisa
dc.contributor.authorHouse Kyle
dc.contributor.authorAlho Petteri
dc.contributor.authorBaker Victor R.
dc.contributor.organizationfi=maantiede|en=Geography |
dc.contributor.organizationfi=maantieteen ja geologian laitos|en=Department of Geography and Geology|
dc.contributor.organization-code1.2.246.10.2458963.20.17647764921
dc.contributor.organization-code1.2.246.10.2458963.20.23186815876
dc.converis.publication-id393491432
dc.converis.urlhttps://research.utu.fi/converis/portal/Publication/393491432
dc.date.accessioned2025-08-27T22:24:58Z
dc.date.available2025-08-27T22:24:58Z
dc.description.abstract<p>Ephemeral alluvial streams pose globally significant flood hazards to human habitation in drylands, but sparse data for these regions limit understanding of the character and impacts of extreme flooding. In this study, we document decadal changes in dryland ephemeral channel patterns at two sites in the lower Colorado River Basin (southwestern United States) that were ravaged by extraordinary flash floods in the 1970s: Bronco Creek, Arizona (1971), and Eldorado Canyon, Nevada (1974). We refer to these two floods as ‘fluviomorphic erasure events’, because they produced blank slates for the channels that were gradually moulded by more frequent but much smaller flood events. We studied georectified aerial photos that span ~60 years at each site to show that both study sites recovered to their pre-flood condition after ~25 years. We employ channel network metrics: stream-link area (SLA), geometric braiding index and junction-node density. Each metric decreased during the short-duration extreme flood erasure events. Subsequently, a fluviomorphic trajectory at a decadal tempo returned the channels to pre-flood values. The SLA decreased at rates of 3.6%–4.1% per year in the decade following the floods. The extreme flood events decreased the pre-flood geometric braiding index at the two sites by 56%–68%, and it took 15–24 years for this index to recover to pre-flood values. In contrast, it took 30–35 years for the channels to recover to a uniform pre-flood channel form, as indicated by the spatial distribution of bars and junction nodes. Our results document baseline examples of ephemeral stream channel evolution trajectories, as future climatic change will likely accelerate increases in the magnitudes and frequencies of extreme floods and geomorphic erasure events. <br></p><p>© 2024 The Authors. Earth Surface Processes and Landforms published by John Wiley & Sons Ltd. This article has been contributed to by U.S. Government employees and their work is in the public domain in the USA.</p>
dc.format.pagerange2628
dc.format.pagerange2650
dc.identifier.eissn1096-9837
dc.identifier.jour-issn0197-9337
dc.identifier.olddbid202128
dc.identifier.oldhandle10024/185155
dc.identifier.urihttps://www.utupub.fi/handle/11111/46072
dc.identifier.urlhttps://doi.org/10.1002/esp.5847
dc.identifier.urnURN:NBN:fi-fe2025082785619
dc.language.isoen
dc.okm.affiliatedauthorAlho, Petteri
dc.okm.affiliatedauthorLotsari, Eliisa
dc.okm.discipline1171 Geosciencesen_GB
dc.okm.discipline1171 Geotieteetfi_FI
dc.okm.internationalcopublicationinternational co-publication
dc.okm.internationalityInternational publication
dc.okm.typeA1 ScientificArticle
dc.publisherJohn Wiley and Sons Ltd
dc.publisher.countryUnited Kingdomen_GB
dc.publisher.countryBritanniafi_FI
dc.publisher.country-codeGB
dc.relation.doi10.1002/esp.5847
dc.relation.ispartofjournalEarth Surface Processes and Landforms
dc.relation.issue9
dc.relation.volume49
dc.source.identifierhttps://www.utupub.fi/handle/10024/185155
dc.titleFluviomorphic trajectories for dryland ephemeral stream channels following extreme flash floods
dc.year.issued2024

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