Quantification of tidal grounding line migration using Sentinel-1 observations

Abstract

Grounding lines (GLs) are subsurface geophysical features that represent the boundary between grounded ice and floating ice shelves. GLs derived from tidal remote sensing methods such as Differential Interferometric SAR, laser and radar altimetry contain an ephemeral displacement in addition to their true location. Previous works have demonstrated that grounding lines migrate with distances ranging from a few hundred meters to several kilometers heterogeneously and out of phase with ocean tides, implying that the tidal component does not diminish in an interannual time series.

We explore the use of SAR Differential Range Offsets Tracking (DROT) to provide insights into tidal migration of the grounding line. We used a times series from 2019 of LOS offsets from 6-day repeat cycle Sentinel-1 acquisitions over Larsen C Ice Shelf. GL positions from the offset profiles were derived by inverting the 1D elastic beam model using the Cross Entropy-based Importance Sampling for Bayesian Updating (CEBU) algorithm.