Sediment Transport and Deposition from a Two‐layer Fluid Model of Gravity Currents on Sloping Bottoms

DOI10.1111/1467-9590.00076zbMath1003.86001OpenAlexW2069319388MaRDI QIDQ4784628

Gordon E. Swaters, J. P. Pascal, T. Bryant Moodie

Publication date: 11 December 2002

Published in: Studies in Applied Mathematics (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1111/1467-9590.00076

Mathematics Subject Classification ID

Hydrology, hydrography, oceanography (86A05) Multiphase and multicomponent flows (76Txx)

Related Items (8)

Sediment Transport via Dam-Break Flows over Sloping Erodible Beds ⋮ Dam-break flows with resistance as agents of sediment transport ⋮ Thermally enhanced gravity driven flows ⋮ Weakly Nonhydrostatic Effects in Compositionally-Driven Gravity Flows ⋮ Self‐Similarity and the Evaluation of Long‐Time Nonhydrostatic Effects in Compositionally Driven Gravity Flows in Deep Surroundings ⋮ Thermohaline considerations in surface gravity driven flows ⋮ Evaluation of a simplified approach for simulating gravity currents over slopes of varying angles ⋮ Gravity currents

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