“…(a) general erosion marking a loss of land surface over large spatial extents (Dalrymple and Kriebel 2005, Shuto and Fujima 2009, Kato et al 2012, Yeh et al 2013, Fraser et al 2013), (b) sustained flow scour near corners and sides around free-standing structures, with scour depth ranging from 0.5 -4.0 m being reported by post-tsunami field surveys (Bricker et al 2012, Tonkin et al 2013), (c) channelized scours in between gaps of larger buildings, as reported by Yeh et al (2013) in the city of Onagawa, Japan during the 2011 Tohoku Earthquake Tsunami, and (d) overtopping scour behind coastal line defenses such as sea walls, where overtopping jets plunging over the structures cause excessive soil erosion (Yeh et al 2004, Kato et al 2012, Mikami et al 2014, Jayaratne et al 2016. All forms of scouring listed above may, when the extreme flow event is persistent and exposes the soil to shear stresses larger than the critical shear stress, result in scouring that could eventually damage structures; only recently, guidelines and standards have started to address this important issue.…”