Three-dimensional displacement field of the 2015 Mw8.3 Illapel earthquake (Chile) from across- and along-track Sentinel-1 TOPS interferometry

Raphael Grandin (1) , Emilie Klein (2, 3) , Marianne Métois (4) , Christophe Vigny (3)

1 IPGP - Institut de Physique du Globe de Paris
2 IPGS - Institut de physique du globe de Strasbourg
3 LGENS - Laboratoire de géologie de l'ENS
4 LGL-TPE - Laboratoire de Géologie de Lyon - Terre, Planètes, Environnement

Wide-swath imaging has become a standard acquisition mode for radar missions aiming at applying synthetic aperture radar interferometry (InSAR) at global scale with enhanced revisit frequency. Increased swath width, compared to classical Stripmap imaging mode, is achieved at the expense of azimuthal resolution. This makes along-track displacements, and subsequently north-south displacements, difficult to measure using conventional split-beam (multiple-aperture) InSAR or cross-correlation techniques. Alternatively, we show here that the along-track component of ground motion can be deduced from the double difference between backward and forward looking interferograms within regions of burst overlap. “Burst overlap interferometry” takes advantage of the large squint angle diversity of Sentinel-1 (∼1°) to achieve subdecimetric accuracy on the along-track component of ground motion. We demonstrate the efficiency of this method using Sentinel-1 data covering the 2015 Mw8.3 Illapel earthquake (Chile) for which we retrieve the full 3-D displacement field and validate it against observations from a dense network of GPS sensors.

Domaines: Planète et Univers [physics]

Raphael Grandin, Emilie Klein, Marianne Métois, Christophe Vigny. Three-dimensional displacement field of the 2015 Mw8.3 Illapel earthquake (Chile) from across- and along-track Sentinel-1 TOPS interferometry. Geophysical Research Letters, 2016, 43 (6), pp.2552 - 2561. ⟨10.1002/2016GL067954⟩. ⟨hal-01320480v2⟩