FN Archimer Export Format
PT J
TI Infragravity waves: from driving mechanisms to impacts
BT 
AF 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
AS 1:1;2:1;3:3;4:4;5:5;6:6;7:7;8:8;9:7;10:9;11:16;12:9;13:2;14:1;15:16;16:5;17:3;18:10;19:11;20:12;21:13;22:14;23:9;24:15;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;15:;16:;17:;18:;19:;20:;21:;22:;23:;24:;
C1 Univ La Rochelle, CNRS, UMR 7266, LIENSs,Inst Littoral & Environm, 2 Rue Olympe Gouges, F-17000 La Rochelle, France.
   Univ Bretagne Occidentale, CNRS, UMR 6554, LETG,GEOMER,IUEM, Technopole Brest Iroise, F-29280 Plouzane, France.
   Deltares, Dept ZKS, POB 177, NL-2600 MH Delft, Netherlands.
   Univ Auckland, Sch Environm, Auckland, New Zealand.
   SHOM, 13 Rue Chatellier, F-29200 Brest, France.
   Univ Brest, CNRS, Lab Oceanog Phys & Spatiale, IFREMER,IRD, F-29200 Plouzane, France.
   Univ Bordeaux, CNRS, UMR EPOC, Bordeaux, France.
   Univ Montpellier II, CNRS, UMR GEOSCI Montpellier, Montpellier, France.
   CNRS, UMR 7154, PRES Sorbonne Paris Cite, Inst Phys Globe Paris, 1 Rue Jussieu, F-75005 Paris, France.
   Bur Rech Geol & Minieres, Risks & Prevent Direct, 3 Ave Claude Guillemin, F-45060 Orleans, France.
   Univ Florida, ESSIE, Civil & Coastal Engn Dept, Gainesville, FL USA.
   IHE, Delft, Netherlands.
   Univ Utrecht, Fac Geosci, Dept Phys Geog, Utrecht, Netherlands.
   Aix Marseille Univ, Univ Toulon, CNRS, IRD,MIO, La Garde, France.
   Delft Univ Technol, Fac Civil Engn & Geosci, Environm Fluid Mech Sect, Stevinweg 1, NL-2628 CN Delft, Netherlands.
   Plymouth Univ, Sch Biol & Marine Sci, Plymouth PL4 8AA, Devon, England.
C2 UNIV LA ROCHELLE, FRANCE
   UBO, FRANCE
   DELTARES, NETHERLANDS
   UNIV AUCKLAND, NEW ZEALAND
   SHOM, FRANCE
   CNRS, FRANCE
   UNIV BORDEAUX, FRANCE
   UNIV MONTPELLIER, FRANCE
   CNRS, FRANCE
   BRGM, FRANCE
   UNIV FLORIDA, USA
   IHE, NETHERLANDS
   UNIV UTRECHT, NETHERLANDS
   UNIV AIX MARSEILLE, FRANCE
   UNIV DELFT, NETHERLANDS
   UNIV PLYMOUTH, UK
UM LOPS
IF 9.53
TC 133
UR https://archimer.ifremer.fr/doc/00417/52876/53800.pdf
LA English
DT Article
DE ;Infragravity waves;Bound wave;Dissipation;Reflection;Sediment transport;Barrier breaching;Seiche;Earth hum
AB 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 breaching. In tidal inlets, IG waves can propagate into the back-barrier lagoon during the food phase and induce large modulations of currents and sediment transport. Their effect appears to be smaller during the ebb phase, due to blocking by countercurrents, particularly in shallow systems. On coral and rocky reefs, IG waves can dominate over short-waves and control the hydro-sedimentary dynamics over the reef flat and in the lagoon. In harbors and semi- enclosed basins, free IG waves can be amplified by resonance and induce large seiches (resonant oscillations). Lastly, free IG waves that are generated in the nearshore can cross oceans and they can also explain the development of the Earth's "hum" (background free oscillations of the solid earth). 
PY 2018
PD FEB
SO Earth-science Reviews
SN 0012-8252
PU Elsevier Science Bv
VL 177
UT 000426409200041
BP 774
EP 799
DI 10.1016/j.earscirev.2018.01.002
ID 52876
ER

EF