This section aims at giving a overview of the performances WV acquisitions coming from the C-band sensor on board S1A since the begining of the mission. The parameters displayed on this pages are radar parameters: Normalized Radar Cross Section (i.e. Backscatter or sigma0), associated noise, Doppler centroid. For radar parameters input data comes from SLC Level-1 products. Values are averaged on each datatake. Only ocean acquisitions are taken into account with a distance-to-coast filter (i.e. center of images closer than 100km are rejected). Observations below -55° South and above +55° North are filtered out.
For geophysical parameters (wind speed of effective Hs), input data is Level-2 OCN products. The Geophysical model Function (GMF) currently considered is CMOD5n.
1/ VV polarisation
VV polarisation is the nominal configuration for the WV Sentinel-1 acquisitions.
WV Backscatter mean level SLC products
WV NRCS bias with respect to empirical model (GMF CMOD5n)
Comparaison of the NRCS distribution for WV1 (left) and WV2 (right) between observations and model.
Histograms of NRCS coming from SAR observations are superimposed with normalized distribution of NRCS values computes using CMOD5n model and ECMWF forecasts.
Following figures are showing the mean NRCS distribution from SLC products over the time per bin of 3 days. The left figure is showing the 2D histogram on the last 365 days, and the right figure is showing the whole mission.
To perform denoising operation on SLC products, the noise vectors annotated in official products are used. For products IPF2.91 nose vectors are corrupted, the correction applied is te following: S1B WV1= -39.30 dB S1B WV2 =-37.44dB S1A WV1 =-38.13dB S1A WV2 =-36.84dB The left figure is showing the 2D histogram on the last 365 days, and the right figure is showing the whole mission.
The left figure is showing the 2D histogram on the last 365 days, and the right figure is showing the whole mission.
The two following figures are scatter plots to compare the NRCS values from SAR WV observations with GMF NRCS values computed using ECMWF winds forecasts.
Timeseries displayed below are showing the NRCS bias between model (CMOD based) and SAR observations. NRCS from SAR are denoised.
The following scatter plots are showing the wind speed performances of SAR observations befoe any NRCS correction.
The following scatter plots are showing the wind speed performances of SAR observations when the NRCS is corrected using the mean bias found with upper figures.
The strategy of calibration for WV on Sentinel-1 is based only on geophysical ocean calibration. It is inspired from the KNMI's NOC methodology. There is no acquisition over corner reflector on WV. The main rules followed since the begining of the mission by Expert Support Laboratories in the Mission Performances Center are: 1) provide NRCS aligned with NRCS coming from CMOD models and using ECMWF wind forecasts. 2) align as much as possible the values of NRCS annotated in the different products distributed: SLC, GRDH, GRDM, GRDF, OCN.more ...