• 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).
GRAVITY CURRENTS MOVING INTO AN AMBIENT FLUID WITH OPEN SURFACE / Petrolo, D.; Ungarish, M.; Chiapponi, L.; Di Federico, V.; Longo, S.. - ELETTRONICO. - (2018), pp. 1-4. (Intervento presentato al convegno IDRA 2018 tenutosi a Ancona nel 12-14 settembre).
GRAVITY CURRENTS MOVING INTO AN AMBIENT FLUID WITH OPEN SURFACE
D. Petrolo;M. Ungarish;L. Chiapponi;S. Longo
2018-01-01
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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