Please use this identifier to cite or link to this item: https://doi.org/10.21256/zhaw-20966
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dc.contributor.authorTonolla, Diego-
dc.contributor.authorGeilhausen, Martin-
dc.contributor.authorDöring, Michael-
dc.date.accessioned2020-12-03T10:50:16Z-
dc.date.available2020-12-03T10:50:16Z-
dc.date.issued2020-10-10-
dc.identifier.issn0197-9337de_CH
dc.identifier.issn1096-9837de_CH
dc.identifier.urihttps://digitalcollection.zhaw.ch/handle/11475/20966-
dc.descriptionThis is the peer reviewed version which has been published in final form at https://doi.org/10.1002/esp.5017 . This article may be used for non-commercial purposes in accordance with Wiley Terms and Conditions for Use of Self-Archived Versions.de_CH
dc.description.abstractHydropower alteration of the natural flow and sediment regime can severely degrade hydromorphology, thereby threatening biodiversity and overall ecosystem processes of rivers and their floodplains. Using sequences of aerial images, we quantified seven decades (1938/1942–2013) of spatiotemporal changes in channel and floodplain morphology, as well as changes in the physical habitats, of three floodplain river reaches of the Swiss pre‐Alps, two hydropower‐regulated and one near‐natural. In the Sarine River floodplain, within the first decades of hydropower impairment, the magnitude and frequency of flood events (Q2, Q10, Q30) decreased substantially. As a result, the area of pioneer floodplain habitats that depend on flood activity and sediment dynamic, such as bare sediments, decreased dramatically by approximately 95%. However, by 2013 vegetated areas had generally increased in comparison to the pre‐regulation period in 1943, indicating general vegetative colonization. Between 1943 and 2013, the active channel underwent essential narrowing (up to 62% width reduction in the residual flow reach) and habitat turnover rates were very low (5% of the total floodplain area changed habitat type five to six times). In contrast, from the 1950s onwards, the near‐natural floodplain of the Sense River experienced recurrent narrowing and widening, and frequent changes between bare and vegetated areas, reflecting the shifting habitat mosaic concept typical for natural floodplains. In the three reaches investigated, we found that the active floodplain width and erosion of vegetated areas were primarily controlled by medium to large floods (Q10, Q30), which combined with reduced time intervals between ordinary floods ≥ Q2 most likely mobilized streambed sediments and limited the ability of vegetation to establish itself on bare gravel bars within the parafluvial zone. These findings can contribute to restoration action plans such as controlled flooding and sediment replenishments in the Sarine and other floodplain rivers of the Alps.de_CH
dc.language.isoende_CH
dc.publisherWileyde_CH
dc.relation.ispartofEarth Surface Processes and Landformsde_CH
dc.rightsLicence according to publishing contractde_CH
dc.subjectHydropower impactsde_CH
dc.subjectRiver and floodplain restorationde_CH
dc.subjectAltered flow and sediment regimede_CH
dc.subjectAerial image analysesde_CH
dc.subjectGeomorphic changesde_CH
dc.subjectActive floodplainde_CH
dc.subject.ddc333: Bodenwirtschaft und Ressourcende_CH
dc.subject.ddc551: Geologie und Hydrologiede_CH
dc.titleSeven decades of hydrogeomorphological changes in a near‐natural (Sense River) and a hydropower‐regulated (Sarine River) pre‐Alpine river floodplain in Western Switzerlandde_CH
dc.typeBeitrag in wissenschaftlicher Zeitschriftde_CH
dcterms.typeTextde_CH
zhaw.departementLife Sciences und Facility Managementde_CH
zhaw.organisationalunitInstitut für Umwelt und Natürliche Ressourcen (IUNR)de_CH
dc.identifier.doi10.1002/esp.5017de_CH
dc.identifier.doi10.21256/zhaw-20966-
zhaw.funding.euNode_CH
zhaw.issue1de_CH
zhaw.originated.zhawYesde_CH
zhaw.pages.end266de_CH
zhaw.pages.start252de_CH
zhaw.publication.statusacceptedVersionde_CH
zhaw.volume46de_CH
zhaw.embargo.end2021-10-11de_CH
zhaw.publication.reviewPeer review (Publikation)de_CH
zhaw.funding.snf153972de_CH
zhaw.webfeedÖkohydrologiede_CH
zhaw.funding.zhawNachhaltiges Auenmanagement und Wasserkraft - HyApp NRP70de_CH
zhaw.author.additionalNode_CH
zhaw.display.portraitYesde_CH
Appears in collections:Publikationen Life Sciences und Facility Management

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Tonolla, D., Geilhausen, M., & Döring, M. (2020). Seven decades of hydrogeomorphological changes in a near‐natural (Sense River) and a hydropower‐regulated (Sarine River) pre‐Alpine river floodplain in Western Switzerland. Earth Surface Processes and Landforms, 46(1), 252–266. https://doi.org/10.1002/esp.5017
Tonolla, D., Geilhausen, M. and Döring, M. (2020) ‘Seven decades of hydrogeomorphological changes in a near‐natural (Sense River) and a hydropower‐regulated (Sarine River) pre‐Alpine river floodplain in Western Switzerland’, Earth Surface Processes and Landforms, 46(1), pp. 252–266. Available at: https://doi.org/10.1002/esp.5017.
D. Tonolla, M. Geilhausen, and M. Döring, “Seven decades of hydrogeomorphological changes in a near‐natural (Sense River) and a hydropower‐regulated (Sarine River) pre‐Alpine river floodplain in Western Switzerland,” Earth Surface Processes and Landforms, vol. 46, no. 1, pp. 252–266, Oct. 2020, doi: 10.1002/esp.5017.
TONOLLA, Diego, Martin GEILHAUSEN und Michael DÖRING, 2020. Seven decades of hydrogeomorphological changes in a near‐natural (Sense River) and a hydropower‐regulated (Sarine River) pre‐Alpine river floodplain in Western Switzerland. Earth Surface Processes and Landforms. 10 Oktober 2020. Bd. 46, Nr. 1, S. 252–266. DOI 10.1002/esp.5017
Tonolla, Diego, Martin Geilhausen, and Michael Döring. 2020. “Seven Decades of Hydrogeomorphological Changes in a near‐Natural (Sense River) and a Hydropower‐Regulated (Sarine River) Pre‐Alpine River Floodplain in Western Switzerland.” Earth Surface Processes and Landforms 46 (1): 252–66. https://doi.org/10.1002/esp.5017.
Tonolla, Diego, et al. “Seven Decades of Hydrogeomorphological Changes in a near‐Natural (Sense River) and a Hydropower‐Regulated (Sarine River) Pre‐Alpine River Floodplain in Western Switzerland.” Earth Surface Processes and Landforms, vol. 46, no. 1, Oct. 2020, pp. 252–66, https://doi.org/10.1002/esp.5017.


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