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Infragravity waves: from driving mechanisms to impacts

Authors :
Bertin, Xavier
De Bakker, Anouk
Van Dongeren, Ap
Coco, Giovanni
Andre, Gael
Ardhuin, Fabrice
Bonneton, Philippe
Bouchette, Frederic
Castelle, Bruno
Crawford, Wayne C.
Davidson, Mark
Deen, Martha
Dodet, Guillaume
Guerin, Thomas
Inch, Kris
Leckler, Fabien
Mccall, Robert
Muller, Heloise
Olabarrieta, Maitane
Roelvink, Dano
Ruessink, Gerben
Sous, Damien
Stutzmann, Eleonore
Tissier, Marion
Bertin, Xavier
De Bakker, Anouk
Van Dongeren, Ap
Coco, Giovanni
Andre, Gael
Ardhuin, Fabrice
Bonneton, Philippe
Bouchette, Frederic
Castelle, Bruno
Crawford, Wayne C.
Davidson, Mark
Deen, Martha
Dodet, Guillaume
Guerin, Thomas
Inch, Kris
Leckler, Fabien
Mccall, Robert
Muller, Heloise
Olabarrieta, Maitane
Roelvink, Dano
Ruessink, Gerben
Sous, Damien
Stutzmann, Eleonore
Tissier, Marion
Source :
Earth-science Reviews (0012-8252) (Elsevier Science Bv), 2018-02 , Vol. 177 , P. 774-799
Publication Year :
2018

Abstract

Infragravity (hereafter IG) waves are surface ocean waves with frequencies below those of wind-generated "short waves" (typically be- low 0.04 Hz). Here we focus on the most common type of IG waves, those induced by the presence of groups in incident short waves. Three related mechanisms explain their generation: (1) the development, shoaling and release of waves bound to the short-wave group envelopes (2) the modulation by these envelopes of the location where short waves break, and (3) the merging of bores (breaking wave front, resembling to a hydraulic jump) inside the surfzone. When reaching shallow water (O(1-10 m)), IG waves can transfer part of their energy back to higher frequencies, a process which is highly dependent on beach slope. On gently sloping beaches, IG waves can dissipate a substantial amount of energy through depth-limited breaking. When the bottom is very rough, such as in coral reef environments, a substantial amount of energy can be dissipated through bottom friction. IG wave energy that is not dissipated is reflected seaward, predominantly for the lowest IG frequencies and on steep bottom slopes. This reflection of the lowest IG frequencies can result in the development of standing (also known as stationary) waves. Reflected IG waves can be refractively trapped so that quasi-periodic along-shore patterns, also referred to as edge waves, can develop. IG waves have a large range of implications in the hydro-sedimentary dynamics of coastal zones. For example, they can modulate cur- rent velocities in rip channels and strongly influence cross-shore and longshore mixing. On sandy beaches, IG waves can strongly impact the water table and associated groundwater flows. On gently sloping beaches and especially under storm conditions, IG waves can dominate cross-shore sediment transport, generally promoting offshore transport inside the surfzone. Under storm conditions, IG waves can also induce overwash and eventually promote dune erosion and barrier

Details

Database :
OAIster
Journal :
Earth-science Reviews (0012-8252) (Elsevier Science Bv), 2018-02 , Vol. 177 , P. 774-799
Notes :
application/pdf, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1286201029
Document Type :
Electronic Resource
Full Text :
https://doi.org/10.1016.j.earscirev.2018.01.002