FN Archimer Export Format
PT J
TI On Doppler Shifts of Breaking Waves
BT 
AF Yurovsky, Yury Yu.
   Kudryavtsev, Vladimir N.
   Grodsky, Semyon A.
   Chapron, Bertrand
AS 1:1,2;2:1,2;3:3;4:4;
FF 1:;2:;3:;4:PDG-ODE-LOPS-SIAM;
C1 Applied Marine Physics Laboratory, Marine Hydrophysical Institute Russian Academy of Sciences, 2 Kapitanskaya, 299011 Sevastopol, Russia
   Satellite Oceanography Laboratory, Russian State Hydrometeorological University, 98 Malookhtinskiy, 195196 St. Petersburg, Russia
   Department of Atmospheric and Oceanic Science, University of Maryland, College Park, MD 20742, USA
   Laboratoire d’Océanographie Physique Spatiale, Institut Français de Recherche pour l’Exploitation de la Mer, 29280 Plouzané, France
C2 RUSSIAN ACAD SCI, RUSSIA
   UNIV RUSSIAN STATE HYDROMETEOROL, RUSSIA
   UNIV MARYLAND, USA
   IFREMER, FRANCE
SI BREST
SE PDG-ODE-LOPS-SIAM
UM LOPS
IN WOS Ifremer UMR
   DOAJ
   copubli-int-hors-europe
IF 5
TC 1
UR https://archimer.ifremer.fr/doc/00835/94677/102084.pdf
LA English
DT Article
DE ;Doppler shift;Ka-band;backscattering;sea surface;wave breaking;whitecap
AB Field-tower-based observations were used to estimate the Doppler velocity of deep water plunging breaking waves. About 1000 breaking wave events observed by a synchronized video camera and dual-polarization Doppler continuous-wave Ka-band radar at incidence angles varying from 25 to 55 degrees and various azimuths were analyzed using computer vision methods. Doppler velocities (DVs) associated with breaking waves were, for the first time, directly compared to whitecap optical velocities measured as the line-of-sight projection of the whitecap velocity vector (LOV). The DV and LOV were found correlated; however, the DV was systematically less than the LOV with the ratio dependent on the incidence angle and azimuth. The largest DVs observed at up-wave and down-wave directions were accompanied by an increase of the cross-section polarization ratio, HH/VV, up to 1, indicating a non-polarized backscattering mechanism. The observed DV was qualitatively reproduced in terms of a combination of fast specular (coherent) and slow non-specular (incoherent) returns from two planar sides of an asymmetric wedge-shaped breaker. The difference in roughness and tilt between breaker sides (the front face was rougher than the rear face) explained the observed DV asymmetry and was consistent with previously reported mean sea surface Doppler centroid data and normalized radar cross-section measurements. 
PY 2023
PD APR
SO Remote Sensing
SN 2072-4292
PU MDPI AG
VL 15
IS 7
UT 000970144900001
DI 10.3390/rs15071824
ID 94677
ER

EF