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Wave run-up and wave overtopping measurements in the field are scarce, since they are very difficult to perform. Wave run-up has been measured in the field using step gauges (e.g. Wenneker et al., 2016), stereophotogrammetry (e.g. De Vries et al., 2011), ultrasonic altimeters (e.g. Matias et al., 2014) or video recordings (e.g. Vousdoukas et al., 2012). More recently, terrestrial laser scanners (LIDARs) have been used to measure the wave run-up in the field as well (e.g. Brodie et al., 2012; Vousdoukas et al., 2014). Wave overtopping measurements in the field are performed even less. Typically wave overtopping measurements in the field are performed using overtopping tanks (e.g. De Rouck et al., 2009). This is a robust method to measure wave overtopping, but at a fixed location and a fixed elevation.

FIELD MEASUREMENTS OF VERY OBLIQUE WAVE RUN-UP AND OVERTOPPING WITH LASER SCANNERS