FN Archimer Export Format
PT J
TI Simultaneous ocean surface current and wind vectors retrieval with squinted SAR interferometry: Geophysical inversion and performance assessment
BT 
AF MARTIN, Adrien CH
   GOMMENGINGER, Christine P.
   QUILFEN, Yves
AS 1:1;2:1;3:2;
FF 1:;2:;3:PDG-ODE-LOPS-SIAM;
C1 Natl Oceanog Ctr, Marine Phys & Ocean Climate Div, Southampton, Hants, England.
   Univ Brest, IFREMER, CNRS, IRD,LOPS, Brest, France.
C2 NOC, UK
   IFREMER, FRANCE
SI BREST
SE PDG-ODE-LOPS-SIAM
UM LOPS
IN WOS Ifremer jusqu'en 2018
   copubli-europe
IF 8.218
TC 18
UR https://archimer.ifremer.fr/doc/00445/55693/57436.pdf
LA English
DT Article
DE ;Ocean surface current vector;Ocean wind vector;Doppler;Scatterometer;SAR;Along-track interferometry
AB Simultaneous measurements of ocean surface current and wind vectors at the ocean submesoscale (O [1–10 km]) are needed to improve our understanding of upper ocean mixing, air-sea interactions, ocean biophysical processes and large-scale oceanic transports. A new satellite mission concept called SEASTAR aims to do just that. The concept is a Ku-band along-track interferometric Synthetic Aperture Radar (SAR) system with two squinted beams pointing ±45° from broadside and incidence angles around 30°. The paper presents an inversion strategy to retrieve simultaneously ocean surface current and wind vectors and reports on the performance obtained with different wind/current conditions and instrument configurations. Results are based on numerical simulations using a Bayesian approach and existing geophysical model functions (GMFs) of the microwave Normalized Radar Cross Section (NRCS) and Doppler shift. Using the baseline two-look instrument configuration and realistic instrument noise figures (radiometric resolution: kp = 5 and 12%; Δdf = 2 and 5 Hz), the root-mean square errors (RMSE) of the retrieved current and wind vectors are typically better than [0.1 m/s, 10°] for current and [0.5 m/s, 5°] for wind. This inversion setup yields four ambiguous solutions within a current range of ∼1 m/s. The addition of dual polarization (VV, HH) capability helps to discriminate these ambiguities. The retrieval performance depends weakly on geophysical parameters such as wind speed, current velocity or current direction, but is sensitive to wind direction because of its strong effect on current retrieval through the wind-wave induced artifact surface velocity (WASV). Larger retrieval errors are obtained when the wind is aligned with one of the antenna line-of-sight (LoS) directions, although errors remain typically below [0.2 m/s, 25°] for current and [0.5 m/s, 15°] for wind. Improving the retrieval performance regardless of wind direction could be achieved either with lower noise figures on σ0, or with higher incidence angles, or by including an additional third-look direction in azimuth (e.g. to achieve a configuration similar to Metop/ASCAT scatterometers) as per the SEASTAR mission concept submitted to EE10. 
PY 2018
PD OCT
SO Remote Sensing Of Environment
SN 0034-4257
PU Elsevier Science Inc
VL 216
UT 000445990100057
BP 798
EP 808
DI 10.1016/j.rse.2018.06.013
ID 55693
ER

EF