Preprints
https://doi.org/10.5194/tc-2022-55
https://doi.org/10.5194/tc-2022-55
 
14 Mar 2022
14 Mar 2022
Status: this preprint is currently under review for the journal TC.

Seasonal land ice-flow variability in the Antarctic Peninsula

Karla Boxall1, Frazer D. W. Christie1, Ian C. Willis1, Jan Wuite2, and Thomas Nagler2 Karla Boxall et al.
  • 1Scott Polar Research Institute, University of Cambridge, Cambridge, United Kingdom
  • 2ENVEO IT GmbH, Innsbruck, Austria

Abstract. Recent satellite-remote sensing studies have documented the multi-decadal acceleration of the Antarctic Ice Sheet in response to rapid rates of concurrent ice-sheet retreat and thinning. Unlike the Greenland Ice Sheet, where historical, high temporal resolution satellite and in situ observations have revealed distinct changes in land ice flow across intra-annual timescales, similar seasonal signals have not previously been observed in Antarctica. Here, we use high spatial and temporal resolution Copernicus Sentinel-1A/B synthetic aperture radar observations acquired between 2014 and 2020 to provide the first evidence for seasonal flow variability of the land ice feeding George VI Ice Shelf (GVIIS), Antarctic Peninsula. Our observations reveal a distinct austral summertime (December – February) speedup of ~0.06 ± 0.005 m d-1 (~22 ± 1.8 m yr-1) at, and immediately inland of, the grounding line of the glaciers nourishing the ice shelf, which constitutes a mean acceleration of ~15 % relative to baseline (timeseries-averaged) rates of flow. These findings are corroborated by independent, optically derived velocity observations. Regional contrasts in the onset of ice-flow acceleration and the overall timing of the speedup events across GVIIS fingerprint oceanic forcing as the primary control of this seasonality. Our findings imply that analogous ice-ocean interactions may be ongoing at the grounding lines of other ocean-vulnerable outlet glaciers around Antarctica. Assessing the degree of seasonal ice-flow variability at such locations is important for quantifying Antarctica’s future contribution to global sea-level rise.

Karla Boxall et al.

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on tc-2022-55', Anonymous Referee #1, 08 Apr 2022
  • RC2: 'Comment on tc-2022-55', Ted Scambos, 12 May 2022

Karla Boxall et al.

Karla Boxall et al.

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Latest update: 30 Jun 2022
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Short summary
Using high spatial and temporal resolution satellite imagery, we provide the first evidence for seasonal flow variability of land ice draining to George VI Ice Shelf (GVIIS), Antarctica. Our findings imply that other glaciers in Antarctica may be susceptible to — and currently undergoing — similar ocean-driven ice flow seasonality, especially those fronted by warm-based, CDW-laden ice-shelf cavities such as Pine Island and Thwaites glaciers.