These data were aquired with a Terrestrial Radar Interferometer overlooking the grounding zone of Priestley Glacier, Antarctica. The time series contains differential interferograms with a 12h temporal baseline covering an approximately 8 day period in November 2018. Tidal modulation of ice streams and their adjacent ice shelves is a real-world experiment to understand ice-dynamic processes. We observe the dynamics of Priestley Glacier, Antarctica, using Terrestrial Radar Interferometry (TRI) and GNSS. Ocean tides are predominantly diurnal but horizontal GNSS displacements oscillate also semi-diurnally. The oscillations are strongest in the ice shelf and tidal signatures decay near-linearly in the TRI data over >10 km upstream of the grounding line. Tidal flexing is observed >6 km upstream of the grounding line including cm-scale uplift. Tidal grounding line migration is small and <40 % of the ice thickness. The frequency doubling of horizontal displacements relative to the ocean tides is consistent with variable ice-shelf buttressing demonstrated with a visco-elastic Maxwell model. Taken together, this supports previously hypothesized flexural ice softening in the grounding-zone through tides and offers new observational constraints for the role of ice rheology in ice-shelf buttressing.

Time series of unwrapped interferograms with a 12h temporal baseline taken with a Terrestrial Radar Interferometer in November 2018 near the grounding zone of Priestley Glacier, Antarctica- The Zip Archive contains 252 Geotiff raster files in geographic project (EPSG 4326)- Each raster has 8793 x 2593 entries- All digits preceding the *_12.0h.diff.geo.tif file ending relate to time of the acquisition in terms of the decimal day of year 2018- The differential interferograms were unwrapped and converted into line-of-sight displacement in meters