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A revisit of the role of gas entrapment on the stability conditions of explosive volcanic columns
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20 |
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Wind entrainment in jets with reversing buoyancy: implications for volcanic plumes
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19 |
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Transition from stable column to partial collapse during the 79 cal CE P3 Plinian eruption of Mt. Pelée volcano (Lesser Antilles)
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18 |
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Impact of wind direction variability on hazard assessment in Martinique (Lesser Antilles): The example of the 13.5 ka cal BP Bellefontaine Plinian eruption of Mount Pelée volcano
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17 |
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Volcanic hazard assessment for tephra fallout in Martinique
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11 |
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Dynamique des éruptions pliniennes: réévaluation de l’aléa volcanique en Martinique
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6 |
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Unsuspected explosive activity of Montagne Pelée (Lesser Antilles) during the 25–10 ka period
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4 |
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Fragmentation behavior of young pyroclasts from Mt. Pelée, Martinique
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3 |
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Tephra fallout and dispersal modeling of phreatic eruptions: Implications for volcanic hazard assessment in Martinique and Guadeloupe (Lesser Antilles)
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1 |
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Preliminary impact assessment of effusive eruptions at Etna volcano
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0 |
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The Past 20,000 Years of Plinian Explosive Activity at Mt Pelée Volcano (Lesser Antilles)
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0 |
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The dynamics of turbulent jets with reversing buoyancy rising in a crossflow: Implications for the collapse of explosive volcanic columns in a windy atmosphere
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0 |
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Tephra fallout hazard assessment for a hydrovolcanic eruptive scenario in Mayotte
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0 |
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Pyroclast textures and fragmentation efficiency-constraining the range of eruptive dynamics of Mt. Pelée volcano, Martinique
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0 |
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Near real-time retrieval of weak plume source parameters: Insights from physical modeling and Meteosat data
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0 |
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Impact of sedimentation and particle fragmentation on the collapse of explosive volcanic eruption columns.
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0 |
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Experimental determination of fragmentation efficiency for Plinian and Pelean eruptions of Mt. Pelée, Martinique
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0 |
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Dynamics of tephra fallout and column collapse during Plinian eruptions of Mt. Pelée volcano (Lesser Antilles): The 2.5 ka cal BCE P5 eruption
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0 |
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Combined effects of gas entrapment and reduced entrainment on the collapse of explosive volcanic eruptions columns
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0 |