Dependence of observed runup on a dissipative beach on incident wave frequency and directional spread

Chuan Li1, H Tuba Ozkan-Haller1, Gabriel Garcia-Medina2, Robert A Holman3 and Peter Ruggiero4, (1)Oregon State University, Corvallis, OR, United States, (2)Pacific Northwest National Laboratory, Seattle, WA, United States, (3)Oregon State Univ, Corvallis, OR, United States, (4)Oregon State University, College of Earth, Ocean, and Atmospheric Sciences, Corvallis, OR, United States
Back to: Nearshore Processes III