Geudtner, Dirk (1); Prats, Pau (2); Yague-Martinz, Nestor (2); De Zan, Francesco (3); Breit, Helko (3); Larsen, Yngvar (4); Monti-Guarnieri, Andrea (5); Barat, Itziar (1); Navas-Traver, Ignacio (1); Torres, Ramon (1) 1: European Space Agency (ESA), Netherlands, The; 2: German Aerospace Center (DLR), Microwaves and Radar Institute; 3: German Aerospace Center (DLR), Remote Sensing Technology Institute; 4: Northern Research (Norut); 5: Politechnico di Milano
This paper addresses the cross-SAR interferometry (InSAR) performance verification of the Sentinel-1A&B Constellation using data acquired with the novel Interferometric Wide Swath (IW) mode during the Sentinel-1B Commissioning phase. The IW mode, for the first time, operationally utilizes ScanSAR-type burst imaging with an additional antenna beam steering in azimuth referred to as Terrain Observation with Progressive Scans (TOPS).
The Sentinel-1 mission is implemented through a constellation of identical C-band SAR satellites comprising the current A and B units, which will be eventually replaced by the planned C and D units.
Sentinel-1A was successfully launched on April 3rd, 2014 followed by the successful launch of Sentinel-1B on April 25th, 2016. Both satellites fly in the in the same orbital plane with 180 deg. phased positions.
The Sentinel-1 SAR instrument operating at C-band supports four exclusive imaging modes providing different resolution and coverage: Interferometric Wide Swath (IW), Extra Wide Swath (EW), StripMap (SM), and Wave (WV).
In fact, the IW TOPS mode is the main mode of operations for the systematic monitoring of large land and coastal areas. This systematic IW mode data acquisition enables the build-up of long InSAR IW data time series.
In particular, the 6-day repeat orbit interval along with small orbital baselines enables cross-InSAR coherent change detection applications, such as the monitoring of cryosphere dynamics (e.g. glacier flow) and the mapping of surface deformation, caused, for example, by tectonic processes, volcanic activities, landslides or ground subsidence
The generation of high-quality S-1A/S-1B TOPS IW mode cross-interferograms and coherence maps requires an accurate synchronization of the azimuth scanning patterns (i.e. bursts) and a very stable azimuth antenna pointing to achieve the maximum common Doppler bandwidth. (i.e. azimuth spectral alignment).
To achieve highly accurate burst synchronization, i.e. the instrument burst data acquisition from repeat-pass orbits starts at the same time over the same location on the ground, the S-1 mission exploits the novel concept of position-tag commanding using the orbit position angle and its on-board conversion into sensing time along with an orbital point grid. The calculation of the burst synchronization is based upon the use of the orbital state vectors and the annotated azimuth start time.
Using S-1A/S-1B InSAR scene and long data take pairs, as well as multi-temporal stacks, all acquired during the Sentinel-1B Commissioning phase, we measured only very small offsets and variation of the burst synchronization of 3ms.
The azimuth antenna pointing is very stable for both S-1A and S-1B due the total zero Doppler attitude steering of the spacecraft causing only a very small difference in Doppler centroid of 20Hz when forming S-1A and S-1B, interferograms, respectively. However, during the Commissioning of S-1B, we measured an initial antenna pointing offset (i.e. yaw and pitch) that is equivalent to a mean Doppler centroid difference 200Hz due to a relative star tracker misalignment.
As a result, the common Doppler bandwidth of S-1A/S-1B cross-interferograms was temporarily reduced to 65%. However, at the end of the S-1B Commissioning phase, the S-1B antenna mis-pointing was corrected for to achieve a Doppler centroid frequency of 20Hz, which is equivalent to more than 95% of the common Doppler bandwidth.
In this paper, we discuss the cross-InSAR performance considering the effects of burst synchronization and SAR antenna pointing on the achievable common Doppler bandwidth. In addition, we show analysis results of the Sentinel-1 ground-track repeatability (i.e. orbital tube) performance and the resulting cross-InSAR baselines.
Results of differential cross-interferograms are presented showing the coseismic surface displacement caused by the central Italy earthquake. The high quality of these interferograms (i.e. no phase jumps at burst edges) demonstrates the excellent compatibility and stability of the radar instruments on both satellites, as well as the accurate orbit control of both spacecraft.