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The 50 more cited publications

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