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Field characterization of the negatively buoyant inflow of the Rhône River into Lake Geneva

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Field characterization of the negatively buoyant inflow of the Rhône River into Lake Geneva

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Field characterization of the negatively buoyant inflow of the Rhône River into Lake Geneva

Sediment connectivity in Alpine basins: from isolated storms to turbidity currents in deep peri-Alpine lakes (examples from the Rhône basin and Lake Geneva, Switzerland)

Quasi-stationary flow structure in turbidity currents

Sediment connectivity in the Rhône basin: From an isolated thunderstorm at Illgraben to a tubidity current in deep Lake Geneva

Mass loss of density currents travelling over pourous bed

Geomorphic work by gravity currents with varying initial conditions

Sediment mass movement of a particle-laden turbidity current based on ultrasound velocity profiling and the distribution of sediment concentration

Tributaries affect the thermal response of lakes to climate change

Numerical Modeling of turbidity currents with Ansys CFX and Telemac 3D

EXPERIMENTAL RESULTS ON SEDIMENT ENTRAINMENT BY GRAVITY CURRENTS

EXPERIMENTAL RESULTS ON SEDIMENT ENTRAINMENT BY GRAVITY CURRENTS

Sediment mass movement of a particle-laden turbidity current based on ultrasound velocity profiling and the distribution of sediment concentration

Geomorphic work by gravity currents with varying initial conditions

Numerical Modeling of turbidity currents with Ansys CFX and Telemac 3D

Field characterization of the negatively buoyant inflow of the Rhône River into Lake Geneva

Quasi-stationary flow structure in turbidity currents

Sediment connectivity in the Rhône basin: From an isolated thunderstorm at Illgraben to a tubidity current in deep Lake Geneva

Sediment connectivity in Alpine basins: from isolated storms to turbidity currents in deep peri-Alpine lakes (examples from the Rhône basin and Lake Geneva, Switzerland)

Tributaries affect the thermal response of lakes to climate change

Mass loss of density currents travelling over pourous bed