FN Archimer Export Format
PT J
TI On radar imaging of current features: 1. Model and comparison with observations - art. no. C07016
BT 
AF KUDRYAVTSEV, V
   AKIMOV, D
   JOHANNESSEN, Johnny
   CHAPRON, Bertrand
AS 1:1;2:2;3:3,4;4:5;
FF 1:;2:;3:;4:PDG-DOP-DCB-OPS-LOS;
C1 Inst Marine Hydrophys, Sevastopol, Ukraine.
   Nansen Environm & Remote Sensing Ctr, N-5006 Bergen, Norway.
   Nansen Environm & Remote Sensing Ctr, St Petersburg 19701, Russia.
   Univ Bergen, Inst Geophys, Bergen, Norway.
   Inst Francais Rech Exploitat Mer, F-29280 Plouzane, France.
C2 INST MARINE HYDROPHYS, UKRAINE
   NERSC, NORWAY
   NERSC, RUSSIA
   UNIV BERGEN, NORWAY
   IFREMER, FRANCE
SI BREST
SE PDG-DOP-DCB-OPS-LOS
IN WOS Ifremer jusqu'en 2018
   copubli-europe
   copubli-int-hors-europe
   copubli-sud
IF 2.784
TC 73
UR https://archimer.ifremer.fr/doc/2005/publication-762.pdf
LA English
DT Article
DE ;Breaking waves;Scattering;Radar imaging model;Ocean surface current
AB [1] A new radar imaging model of ocean current features is proposed. The simulated normalized radar cross section ( NRCS) takes into account scattering from "regular'' surfaces ( by means of resonant Bragg scattering and specular reflections) and scattering from breaking waves. The description of background wind waves and their transformation in nonuniform medium is based on solution of the wave action conservation equation. Wave breaking plays a key role in the radar imaging model. Breaking waves scatter radio waves ( thus directly contributing to the NRCS), provide energy dissipation in wind waves ( thus defining the wave spectrum of intermediate scale waves), and generate short surface waves ( thus affecting Bragg scattering). Surface current, surfactants accumulated in the convergence zone, and varying wind field are considered as the main sources for the NRCS manifestations of current features. The latter source can result from transformation of atmospheric boundary layer over the sea surface temperature front. It is shown that modulation of wave breaking significantly influences both radar returns and short wind waves. In the range of short gravity waves related to Ku-X-, and C-bands, the modulation of Bragg waves through wave breaking is the governing mechanism. The model is tested against well-controlled experiments including JOWIP, SARSEX, and CoastWatch-95. A reasonably good agreement between model and observations is obtained.
PY 2005
PD JUN
SO Journal of Geophysical Union - Research C - Oceans
SN 0148-0227
PU American Geophysical Union
VL 110
IS C7
UT 000230919100001
DI 10.1029/2004JC002505
ID 762
ER

EF