Unravelling the impacts to the built environment caused by floods in a river heavily perturbed by volcanic eruptions

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datacite.alternateIdentifier.citationJOURNAL OF SOUTH AMERICAN EARTH SCIENCES,Vol.102,,2020
datacite.alternateIdentifier.doi10.1016/j.jsames.2020.102655
datacite.creatorBasso Baez, Sebastian
datacite.creatorMazzorana, Bruno
datacite.creatorUlloa, Hector
datacite.creatorBahamondes, Diego
datacite.creatorRuiz Villanueva, Virginia
datacite.creatorSanhueza, Daniel
datacite.creatorIroume, Andres
datacite.creatorPicco, Lorenzo
datacite.date2020
datacite.subject.englishFlood
datacite.subject.englishHazard
datacite.subject.englishCascade processes
datacite.subject.englishBridge clogging
datacite.subject.englishImpact
datacite.subject.englishModelling
datacite.subject.englishChaiten volcano
datacite.titleUnravelling the impacts to the built environment caused by floods in a river heavily perturbed by volcanic eruptions
dc.date.accessioned2021-04-30T16:58:26Z
dc.date.available2021-04-30T16:58:26Z
dc.description.abstractExplosive volcanic eruptions generate a range of physical processes with great hazard potential. Subsequent fluvial processes have major effects on channel and valley-floor geometry, potentially resulting in extreme sediment and large wood (LW) yields. The associated impacts can be severe, both immediately and in the longer term as river channels are permanently reworking the large volumes of their own sediment. The city of Chaiten (Lake District, Chile) is a unique case, since sediment- and wood-laden flows in the Blanco River may still pose, even 11 years after the paroxysmal eruption of the Chaiten volcano, large urban sectors at risk. Thoroughly assessing the flood hazard and the generated impact for such urban settings is, hence, of utmost importance. To achieve this goal, we designed a workflow integrating the following tasks: (i) hydrologic modelling at catchment scale employing the HEC-HMS model to obtain flood hydrographs for a 30 and 100 years flood, respectively, (ii) estimation of the sediment fluxes to establish reliable boundary conditions for (iii) the subsequent extensive 2D flood modelling with the model Iber in the unconfined floodplain and delta of the Blanco River including also the effects of possible clogging of the 'Austral Road' bridge with transported LW, (iv) quantification of a series of building performance indicators for a set of 13 residential buildings as a basis for subsequent vulnerability and risk assessment. We found that, even without a new volcanic eruption as a potent hazard trigger, vast urban sectors are still exposed to flooding, in particular if LW gets entrapped at the 'Austral Road' bridge and channel outbursts occur as a consequence of the reduced conveyance and backwater rise. Our results indicate a great spatial variability of flood impacts, being worst in the urban areas either located closely to the channel outburst locations or where overland flow locally channelizes on concave floodplain topographies. Based on our findings we outline provisional recommendations for risk mitigation and informed land use planning.
dc.identifier.urihttp://repositoriodigital.uct.cl/handle/10925/3697
dc.language.isoen
dc.publisherPERGAMON-ELSEVIER SCIENCE LTD
dc.sourceJOURNAL OF SOUTH AMERICAN EARTH SCIENCES
oaire.resourceTypeArticle
uct.catalogadorWOS
uct.indizacionSCI
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