Modelling has been used in the study of volcanic systems for more than 100 years, building
upon the approach first applied by Sir James Hall in 1815. Informed by observations of …

We introduce a novel analytical expression that allows for fast assessment of mass flow rate
of both vertically‐rising and bent‐over volcanic plumes as a function of their height, while …

This study compares and evaluates one-dimensional (1D) and three-dimensional (3D)
numerical models of volcanic eruption columns in a set of different inter-comparison …

Discharge of surface‐derived meltwater at the submerged base of Greenland's marine‐
terminating glaciers creates subglacial discharge plumes that rise along the glacier/ocean …

Accurate forecasting of volcanic particle (tephra) dispersal and fallout requires a reliable
estimation of key Eruption Source Parameters (ESPs) such as the Mass Eruption Rate (QM) …

Meltwater and sediment-laden plumes at tidewater glaciers, resulting from the localized
subglacial discharge of surface melt, influence submarine melting of the glacier and the …

Abstract The 2011 Cordón Caulle eruption represents an ideal case study for the
characterization of long‐lasting plumes that are strongly affected by wind. The climactic …

Characteristics of laboratory-scale bubble-driven buoyant plumes in a stably stratified
quiescent fluid are studied using large-eddy simulation (LES). As a bubble plume entrains …

In the framework of the IAVCEI (International Association of Volcanology and Chemistry of
the Earth Interior) intercomparison study on volcanic plume models, we present three …

Carbon budgets of hydrothermal plumes result from the balance between carbon sinks
through plume chemoautotrophic processes and carbon release via microbial respiration …