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Mostrando ítems 1-4 de 4

    • Aeolian Remobilisation of the 2011-Cordón Caulle Tephra-Fallout Deposit: Example of an Important Process in the Life Cycle of Volcanic Ash 

      Dominguez, Lucia; Bonadonna, Costanza; Forte, Pablo; Jarvis, Paul Antony; Cioni, Raffaello; Mingari, Leonardo; Bran, Donaldo Eduardo; Panebianco, Juan Esteban (Frontiers Media SA, 2020-01-14)
      Although volcanic eruptions represent short periods in the whole history of a volcano, the large amount of loose pyroclastic material produced, combined with aeolian processes, can lead to continuous, long-lasting reworking ...

    • Aeolian Remobilisation of Volcanic Ash: Outcomes of a Workshop in the Argentinian Patagonia 

      Jarvis, Paul Antony; Bonadonna, Constanza; Dominguez, Lucía; Forte, Pablo; Frischknecht, Corine; Bran, Donaldo Eduardo; Aguilar, Rigoberto; Beckett, Frances; Elissondo, Manuela; Gillies, John; Kueppers, Ulrich; Merrison, Jonathan; Varley, Nick; Wallace, Kristi L. (Frontiers Media, 2020-11-27)
      During explosive volcanic eruptions, large quantities of tephra can be dispersed and deposited over wide areas. Following deposition, subsequent aeolian remobilisation of ash can potentially exacerbate primary impacts on ...

    • The influence of local environmental and socio-economic conditions on the impacts of ash storms 

      Forte, Pablo; Dominguez, Lucia; Bonadonna, Constanza; Lamberti, Maria Clara; Gregg, Chris E.; Bran, Donaldo Eduardo; Castro, Jonathan M. (2018-09-02)
      Volcanic ash wind-induced remobilization events have increasingly been reported in different areas around the worl during the last decades

    • Tormentas de ceniza volcánica en Patagonia : un peligro latente y subestimado 

      Forte, Pablo; Dominguez, Lucia; Bonadonna, Lucia; Lamberti, María Clara; Gregg, Chris E.; Bran, Donaldo Eduardo; Castro, Jonathan M. (2018-04)
      Una tormenta de ceniza volcánica puede definirse como un evento de remobilización masiva de ceniza volcánica (<2mm) a partir de la acción eólica (via suspensión, saltación y reptaje). Pero, ¿a qué nos referimos exactamente ...