FN Archimer Export Format
PT J
TI Infragravity waves across the oceans
BT 
AF RAWAT, Arshad
   ARDHUIN, Fabrice
   BALLU, Valerie
   CRAWFORD, Wayne
   CORELA, Carlos
   AUCAN, Jerome
AS 1:1,2;2:1,3;3:4;4:4,5;5:6;6:7;
FF 1:PDG-ODE-LOS;2:;3:;4:;5:;6:;
C1 IFREMER, Lab Oceanog Spatiale, Brest, France.
   Mauritius Oceanog Inst, Quatre Bornes, Mauritius.
   CNRS IFREMER IRD UBO, UMR 6523, Lab Phys Oceans, Plouzane, France.
   Univ La Rochelle, CNRS, UMR 7266, LIENSs, La Rochelle, France.
   Pres Univ Paris Sorbonne Cite, IPGP, Paris, France.
   Inst Dom Luiz, Lisbon, Portugal.
   IRD, Noumea, New Caledonia.
C2 IFREMER, FRANCE
   MAURITIUS OCEANOG INST, MAURITIUS
   CNRS, FRANCE
   UNIV LA ROCHELLE, FRANCE
   IPGP, FRANCE
   INST DOM LUIZ, PORTUGAL
   IRD, FRANCE
SI BREST
SE PDG-ODE-LOS
   PDG-ODE-LPO
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-p187
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 4.196
TC 25
TU Centre national de la recherche scientifique
   Institut National de l'Information Géographique et Forestière
   Institut de physique du globe
   Institut de recherche pour le développement
   Institut français de recherche pour l'exploitation de la mer
   Université Paris Diderot
   Université Pierre et Marie Curie
   Université de Bretagne Occidentale
   Université de La Rochelle
   Université de La Réunion
UR https://archimer.ifremer.fr/doc/00233/34465/32860.pdf
LA English
DT Article
CR GRAVILUCK
BO L'Atalante
DE ;infragravity waves;DART;global wave model
AB Ocean infragravity (IG) waves are low-frequency waves generated along shorelines by incident seas and swell and with heights of the order of 1 cm in the open ocean. Despite these small amplitudes, they can be of much importance for ice shelf break up and errors in measurements of sea level by future satellite altimeters. A combination of numerical model results and in situ data is used to show that bottom pressure signals in the infragravity frequency band can be dominated by bursts of energy that travel across ocean basins, and can last for several days. Two particularly strong events recorded in 2008 are studied, one in the North-Pacific and the other in the North-Atlantic. It is shown that infragravity waves can travel across whole oceans basins with the signal recorded on the western shores often dominated by IG waves coming from the opposite shore of that same ocean basin.
PY 2014
PD NOV
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 41
IS 22
UT 000346644600026
BP 7957
EP 7963
DI 10.1002/2014GL061604
ID 34465
ER

EF