• 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

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).
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Utilizza questo identificativo per citare o creare un link a questo documento: http://hdl.handle.net/11381/2847218
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