Grounding-zone flow variability of Priestley Glacier, Antarctica, in a diurnal tidal regime
Drews, Reinhard; Wild, Christian T; Marsh, Oliver J. ORCID: https://orcid.org/0000-0001-7874-514X; Rack, Wolfgang; Ehlers, Todd A.; Neckel, Nikals; Helm, Veit. 2021 Grounding-zone flow variability of Priestley Glacier, Antarctica, in a diurnal tidal regime. Geophysical Research Letters, 48 (20), e2021GL093853. 10, pp. https://doi.org/10.1029/2021GL093853
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Abstract/Summary
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 also oscillate 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.
Item Type: | Publication - Article |
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Digital Object Identifier (DOI): | https://doi.org/10.1029/2021GL093853 |
ISSN: | 0094-8276 |
Additional Keywords: | glaciology, ice streams, ice-ocean interactions, ocean tides, surface velocities, geophysics |
Date made live: | 01 Mar 2021 10:43 +0 (UTC) |
URI: | https://nora.nerc.ac.uk/id/eprint/528771 |
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