Mapping subsurface scatterers from SAR backscatter time series

Abstract

The Sentinel-1 Next Generation (Sentinel-1NG) and the Radar Observing System for Europe at L-band (ROSE-L) missions are currently being designed to advance the successful systematic monitoring capabilities of the Sentinel-1 mission. As many Copernicus services will benefit from using the resulting dual-frequency (C- and L-band) SAR data in a synergistic manner, the question arises which orbit configuration serves the Copernicus services best? The first option is to fly ROSE-L in convoy with Sentinel-1 – and later with Sentinel-1NG – to acquire matching dual-frequency SAR imagery just a few minutes apart. The second option is phase the satellites orbits such as to maximise the daily global coverage achieved by all satellites. This contribution is intended to highlight that the second option is clearly preferred by the Copernicus Global Land Monitoring Service and the Copernicus Emergency Management Service that provide amongst other data products near-real-time soil moisture and flood monitoring data serving a broad range of applications (from emergency response to data assimilation). The availability of daily SAR images at either C- or L-band will ensure that also smaller, rapid flood events and highly dynamic soil moisture processes are captured. Furthermore, the availability of L-band data interleaved with the C-band data stacks can be expected to improve the retrievals significantly. These advantages outweigh the modest improvements in retrieval accuracy that can be expected for soil moisture and flood retrieval by reducing the time difference between C- and L-band acquisitions by flying the satellites in convoy.