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dc.contributor.authorRauter, Matthias
dc.contributor.authorViroulet, Sylvain
dc.contributor.authorGylfadóttir, Sigríður Sif
dc.contributor.authorFellin, Wolfgang
dc.contributor.authorLøvholt, Finn
dc.date.accessioned2022-05-09T15:55:50Z
dc.date.available2022-05-09T15:55:50Z
dc.date.created2022-02-04T12:00:29Z
dc.date.issued2022
dc.identifier.citationNature Communications. 2022, 13 (1), .
dc.identifier.issn2041-1723
dc.identifier.urihttps://hdl.handle.net/11250/2994866
dc.description.abstractSubaerial landslides and volcano flank collapses can generate tsunamis with devastating consequences. The lack of comprehensive models incorporating both the landslide and the wave mechanics represents a gap in providing consistent predictions of real events. Here, we present a novel three-dimensional granular landslide and tsunami model and apply it to the 2014 Lake Askja landslide tsunami. For the first time, we consistently simulate small-scale laboratory experiments as well as full scale catastrophic events with the same model. The model captures the complete event chain from the landslide dynamics to the wave generation and inundation. Unique and complete field data, along with the limited geographic extent of Lake Askja enabled a rigorous validation. The model gives deep insights into the physical landslide processes and improves our understanding and prediction capabilities of frequent and catastrophic landslide tsunamis.
dc.language.isoeng
dc.titleGranular porous landslide tsunami modelling – the 2014 Lake Askja flank collapse
dc.typePeer reviewed
dc.typeJournal article
dc.description.versionpublishedVersion
dc.source.pagenumber13
dc.source.volume13
dc.source.journalNature Communications
dc.source.issue1
dc.identifier.doi10.1038/s41467-022-28296-7
dc.identifier.cristin1997759
dc.relation.projectEC/H2020/721403
cristin.ispublishedtrue
cristin.fulltextoriginal
cristin.qualitycode2


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