Journal of Marine Science and Engineering Article Transformation of Infragravity Waves during Hurricane Overwash Katherine Anarde 1,*,† , Jens Figlus 2 , Damien Sous3,4 and Marion Tissier 5 1 Department of Civil and Environmental Engineering, Rice University, Houston, TX 77005, USA 2 Department of Ocean Engineering, Texas A&M University, Galveston, TX 77554, USA; fi
[email protected] 3 Mediterranean Institute of Oceanography (MIO), Université de Toulon, Aix Marseille Université, CNRS, IRD, 83130 La Garde, France;
[email protected] 4 Laboratoire des Sciences de l’Ingénieur Appliquées a la Méchanique et au Génie Electrique—Fédération IPRA, University of Pau & Pays Adour/E2S UPPA, Chaire HPC-Waves, EA4581, 64600 Anglet, France 5 Faculty of Civil Engineering and Geosciences, Environmental Fluid Mechanics Section, Delft University of Technology, 2628CN Delft, The Netherlands;
[email protected] * Correspondence:
[email protected] † Current address: Department of Geological Sciences, University of North Carolina at Chapel Hill, Chapel Hill, NC 27514, USA. Received: 1 July 2020; Accepted: 16 July 2020; Published: 22 July 2020 Abstract: Infragravity (IG) waves are expected to contribute significantly to coastal flooding and sediment transport during hurricane overwash, yet the dynamics of these low-frequency waves during hurricane impact remain poorly documented and understood. This paper utilizes hydrodynamic measurements collected during Hurricane Harvey (2017) across a low-lying barrier-island cut (Texas, U.S.A.) during sea-to-bay directed flow (i.e., overwash). IG waves were observed to propagate across the island for a period of five hours, superimposed on and depth modulated by very-low frequency storm-driven variability in water level (5.6 min to 2.8 h periods).