Non-Boussinesq gravity currents with a free surface ambient fluid generate a depression advancing with the front. A set of experiments favourable compare with the theoretical results. Results for the shallow-water dam-break problem are quite close to those for the top-lid case (except for the dip of the surface).
Diana Petrolo, M.U. (2018). GRAVITY CURRENTS MOVING INTO AN AMBIENT FLUID WITH OPEN SURFACE.
GRAVITY CURRENTS MOVING INTO AN AMBIENT FLUID WITH OPEN SURFACE
Vittorio Di Federico;
2018
Abstract
Non-Boussinesq gravity currents with a free surface ambient fluid generate a depression advancing with the front. A set of experiments favourable compare with the theoretical results. Results for the shallow-water dam-break problem are quite close to those for the top-lid case (except for the dip of the surface).File in questo prodotto:
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