Hydrometeorological controls and erosive response of an extreme alpine debris flow (Articolo in rivista)

Type
Label
  • Hydrometeorological controls and erosive response of an extreme alpine debris flow (Articolo in rivista) (literal)
Anno
  • 2009-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1002/hyp.7362 (literal)
Alternative label
  • Marchi, L., Cavalli, M., Sangati, M., Borga, M. (2009)
    Hydrometeorological controls and erosive response of an extreme alpine debris flow
    in Hydrological processes (Print)
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • Marchi, L., Cavalli, M., Sangati, M., Borga, M. (literal)
Pagina inizio
  • 2714 (literal)
Pagina fine
  • 2727 (literal)
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  • 23 (literal)
Rivista
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  • in print (literal)
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  • 14 (literal)
Note
  • Scopu (literal)
  • Google Scholar (literal)
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Lorenzo Marchi: CNR IRPI, Padova, Italy Marco Cavalli: CNR IRPI, Padova, Italy Marco Sangati: Department of Land and Agroforest Environments, University of Padova, Italy Marco Borga: Department of Land and Agroforest Environments, University of Padova, Italy (literal)
Titolo
  • Hydrometeorological controls and erosive response of an extreme alpine debris flow (literal)
Abstract
  • On 29 August, 2003, an intense convective storm system affected the Fella River basin, in the eastern Italian Alps, producing rainfall peaks of approximately 390 mm in 12 h. The storm triggered an unusually large debris flow in the ungauged Rio Cucco basin (0.65 km2), with a volume of approximately 78 000 m3. The analysis of the time evolution of the rainstorm over the basin has been based on rainfall estimates from radar observations and data recorded by a raingauge network. Detailed geomorphological field surveys, carried out both before and after the flood of August 2003, and the application of a distributed hydrological model have enabled assessment of flood response, estimation of erosion volumes and sediment supply to the channel network. The accounts of two eyewitnesses have provided useful elements for reconstructing the time evolution and the flow processes involved in the event. Liquid peak discharge estimates cluster around 20 m3 s-1 km-2, placing this event on the flood envelope curve for the eastern Italian Alps. The hydrological analysis has shown that the major controls of the flood response were the exceptional cumulated rainfall amount, required to exceed the large initial losses, and the large rainfall intensities at hourly temporal scales, required to generate high flood response at the considered basin scale. Observations on the deposits accumulated on the alluvial fan indicate that, although the dominant flow process was a debris flow, sheetflood also contributed to fan aggradation and fluvial reworking had an important role in winnowing debris-flow lobes and redistributing sediment on the fan surface. This points out to the large discharge values during the recession phase of the flood, implying an important role for subsurface flow on runoff generation of this extreme flash flood event. (literal)
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