In the present investigation, we report data from direct numerical simulations of elliptical, finite release, Boussinesq gravity currents propagating down a uniform slope. The study comprises a series of simulations of elliptical gravity currents on a range of slope angles. The shape parameters are varied to study the effects of the initial cross-sectional aspect ratio (Λ0) and mean height to lock radius ratio (Γ) on the dynamics of the gravity current. It is found that the long-time development of the current spatial mass distribution is influenced by its initial shape at smaller slope angles (θ=5∘ and 10∘) whereas the long-time motion of the gravity current is relatively insensitive to its initial shape but is sensitive to the slope angle...
International audienceGravity currents often occur on complex topographies and are therefore subject...
International audienceWe present experimental results on the development of gravity currents moving ...
The advance of the front of a dense gravity current propagating in a rectangular channel and V-shape...
In the present investigation, we report data from direct numerical simulations of elliptical, finite...
We report on the dynamics of circular finite-release Boussinesq gravity currents on a uniform slope....
The present work reports some new aspects of non-axisymmetric gravity currents obtained from laborat...
The present work reports some new aspects of non-axisymmetric gravity currents obtained from laborat...
AbstractGravity currents occur when fluids of different density are brought together. When gravity c...
We present results from experiments and simulations pertaining to finite release gravity currents wi...
[[abstract]]Three-dimensional direct numerical simulations of gravity currents on different bottom s...
Gravity currents are buoyancy driven flows that appear in a variety of situations in nature as well ...
Gravity currents are buoyancy driven flows that appear in a variety of situations in nature as well ...
Planar, Boussinesq, compositional gravity currents formed by the release of a fixed volume of heavie...
Lock-exchange gravity currents propagating up a slope are investigated by large eddy simulations, fo...
The dynamics of lock-release gravity currents flowing up a sloping bottom are investigated by labora...
International audienceGravity currents often occur on complex topographies and are therefore subject...
International audienceWe present experimental results on the development of gravity currents moving ...
The advance of the front of a dense gravity current propagating in a rectangular channel and V-shape...
In the present investigation, we report data from direct numerical simulations of elliptical, finite...
We report on the dynamics of circular finite-release Boussinesq gravity currents on a uniform slope....
The present work reports some new aspects of non-axisymmetric gravity currents obtained from laborat...
The present work reports some new aspects of non-axisymmetric gravity currents obtained from laborat...
AbstractGravity currents occur when fluids of different density are brought together. When gravity c...
We present results from experiments and simulations pertaining to finite release gravity currents wi...
[[abstract]]Three-dimensional direct numerical simulations of gravity currents on different bottom s...
Gravity currents are buoyancy driven flows that appear in a variety of situations in nature as well ...
Gravity currents are buoyancy driven flows that appear in a variety of situations in nature as well ...
Planar, Boussinesq, compositional gravity currents formed by the release of a fixed volume of heavie...
Lock-exchange gravity currents propagating up a slope are investigated by large eddy simulations, fo...
The dynamics of lock-release gravity currents flowing up a sloping bottom are investigated by labora...
International audienceGravity currents often occur on complex topographies and are therefore subject...
International audienceWe present experimental results on the development of gravity currents moving ...
The advance of the front of a dense gravity current propagating in a rectangular channel and V-shape...