FN Archimer Export Format
PT J
TI Storm waves focusing and steepening in the Agulhas current: Satellite observations and modeling
BT 
AF QUILFEN, Yves
   YUROVSKAYA, M.
   CHAPRON, Bertrand
   ARDHUIN, Fabrice
AS 1:1;2:2,3;3:1,3;4:4;
FF 1:PDG-ODE-LOPS-SIAM;2:;3:PDG-ODE-LOPS-SIAM;4:;
C1 Univ Brest, IFREMER, CNRS, IRD,LOPS, Brest, France.
   Marine Hydrophys Inst RAS, Sebastopol, Russia.
   Russian State Hydrometeorol Univ, St Petersburg, Russia.
C2 IFREMER, FRANCE
   RUSSIAN ACAD SCI, RUSSIA
   UNIV RUSSIAN STATE HYDROMETEOROL, RUSSIA
   CNRS, FRANCE
SI BREST
SE PDG-ODE-LOPS-SIAM
UM LOPS
IN WOS Ifremer jusqu'en 2018
   copubli-france
   copubli-int-hors-europe
IF 8.218
TC 45
UR https://archimer.ifremer.fr/doc/00451/56289/57867.pdf
LA English
DT Article
DE ;Extreme waves;Wave-current interactions;Satellite altimeter;SAR
AB Strong ocean currents can modify the height and shape of ocean waves, possibly causing extreme sea states in particular conditions. The risk of extreme waves is a known hazard in the shipping routes crossing some of the main current systems. Modeling surface current interactions in standard wave numerical models is an active area of research that benefits from the increased availability and accuracy of satellite observations. We report a typical case of a swell system propagating in the Agulhas current, using wind and sea state measurements from several satellites, jointly with state of the art analytical and numerical modeling of wave-current interactions. In particular, Synthetic Aperture Radar and altimeter measurements are used to show the evolution of the swell train and resulting local extreme waves. A ray tracing analysis shows that the significant wave height variability at scales <~100 km is well associated with the current vorticity patterns. Predictions of the WAVEWATCH III numerical model in a version that accounts for wave-current interactions are consistent with observations, although their effects are still under-predicted in the present configuration. From altimeter measurements, very large significant wave height gradients are shown to be well captured, and also associated with the current vorticity patterns at global scale. 
PY 2018
PD OCT
SO Remote Sensing Of Environment
SN 0034-4257
PU Elsevier Science Inc
VL 216
UT 000445990100039
BP 561
EP 571
DI 10.1016/j.rse.2018.07.020
ID 56289
ER

EF