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  • 1
    Publication Date: 2020-11-09
    Description: Kinetic energy models are tools able to provide an estimate to the inundation area of pyroclastic density currents (PDCs). We present here a novel strategy that allows improving these models in order to consider the occurrence of channelization processes of pyroclastic material. In this strategy, the inundation area associated with a basal collapse process, represented by a root conoid that interacts with the topography, is complemented with the inundation zones derived from the inclusion of secondary source points located in the expected zones of pyroclast channelization (represented by branch conoids). For that, we adopt a tree branch-like structure and appropriate assumptions for setting the position and the initial characteristics of the secondary source points. Two widely used kinetic models are modified by applying this strategy: the energy cone and the box model, giving place to two open-source and freely downloadable codes (ECMapProb and BoxMapProb). We tested these branching formulations by comparing their results with those derived from the traditional formulations of these kinetic energy models, with other numerical solvers, and with the invasion area of real PDC deposits. We show the capability of the presented strategy of improving the accuracy of kinetic models without adding new, unconstrained input parameters or significantly increasing the computational cost, allowing the assessment of volcanic hazards using a probabilistic approach. The application of this strategy represents a time-effective alternative to the use of more sophisticated models for describing PDC transport and deposition.
    Description: Published
    Description: Catania
    Description: 5V. Processi eruttivi e post-eruttivi
    Keywords: pyroclastic density currents ; box model
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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  • 2
    Publication Date: 2020-11-09
    Description: The formation of pyroclastic density currents (PDC) at Stromboli has been described several times. PDCs are associated with paroxysms, lava emissions and commonly confined into the Sciara del Fuoco (SdF). At least during 1906, 1930 and 1944 paroxysms PDCs were produced on the flanks of Stromboli, out of the SdF. PDCs flowed in valleys cut on the volcano flanks and reached the sea producing vast deltas. In 1930 two flows reached the Stromboli village causing victims. During the 3 July paroxysm, pyroclastic material was emplaced on steep slopes right above the village of Ginostra and small avalanches of incandescent rocks were produced. In light of recent events, PDCs were produced also inside the SdF, reached the sea and continued to flow over the water for several hundred meters. PDCs potentially represent the most dangerous manifestation of volcanic activity at Stromboli and need a proper hazard assessment.
    Description: Published
    Description: Catania
    Description: 6V. Pericolosità vulcanica e contributi alla stima del rischio
    Keywords: Stromboli ; pyroclastic density currents
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: Conference paper
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