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Modeling Multi-Fraction Coastal Aeolian Sediment Transport With Horizontal and Vertical Grain-Size Variability
Chenier Formation Through Wave Winnowing and Tides
Depth-Resolved Modelling of Intra-Swash Morphodynamics Induced by Solitary Waves
Novel sediment sampling method provides new insights into vertical grain size variability due to marine and aeolian beach processes
Wave Generation of Gravity-Driven Sediment Flows on a Predominantly Sandy Seabed
Modeling Swash zone sediment transport at Truc Vert beach
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