Previous measurements and numerical simulations of buoyant turbulent plumes that
develop from area sources provide convincing evidence that entrainment varies locally in …

Turbulent negatively buoyant jets occur when the buoyancy of a jet opposes its source
momentum. In these flows, the fluid will rise until it reaches a stagnation point and a return …

Aluto volcano, in the Main Ethiopian Rift, is a peralkaline caldera system, which comprises
conglomerations of rhyolite (obsidian) lavas and enigmatic pumice cones. Recent work at …

Explosive volcanic eruptions commonly undergo a transition from stable plume to collapsing
fountain with associated destructive pyroclastic density currents. A major goal in physical …

We present simultaneous two-dimensional measurements of the velocity and buoyancy
fields on a central vertical plane in two-dimensional line plumes: a free plume distant from …

A fundamental study has been conducted to understand the mean and turbulence
characteristics and their role in mixing processes of starting turbulent plumes initiated by a …

Understanding clast dispersal from subaqueous volcanism is hampered by uncertainty in
the source and extent of seafloor deposits. Extensive sampling in situ of seafloor deposits …

The flow formed by the discharge of inclined turbulent negatively round buoyant jets is
common in environmental flow phenomena, especially in the case of brine disposal. The …

In this paper, a state-of the art numerical weather prediction (NWP) model is used to
simulate the near-field plume of a Plinian-type volcanic eruption. The NWP model is run at …

We present three‐dimensional numerical simulations of eruption clouds from circular to
linear fissure vents to investigate the control of vent shape on the height and stability of …