Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry

Short-term tidal grounding line (GL) migration in Antarctica can impact ice dynamics at the ice sheet margins and obscures assessments of long-term GL advance or retreat. However, the magnitude of tidally-induced GL migration is poorly known, and the spatial pattern and modes of variability are not...

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Main Authors: Freer, Bryony I. D., Marsh, Oliver J., Hogg, Anna E., Fricker, Helen Amanda, Padman, Laurie
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-2022-265
https://tc.copernicus.org/preprints/tc-2022-265/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd108630 2023-05-15T13:38:41+02:00 Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry Freer, Bryony I. D. Marsh, Oliver J. Hogg, Anna E. Fricker, Helen Amanda Padman, Laurie 2023-02-24 application/pdf https://doi.org/10.5194/tc-2022-265 https://tc.copernicus.org/preprints/tc-2022-265/ eng eng doi:10.5194/tc-2022-265 https://tc.copernicus.org/preprints/tc-2022-265/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-2022-265 2023-02-27T17:22:57Z Short-term tidal grounding line (GL) migration in Antarctica can impact ice dynamics at the ice sheet margins and obscures assessments of long-term GL advance or retreat. However, the magnitude of tidally-induced GL migration is poorly known, and the spatial pattern and modes of variability are not well characterised. Here we develop and apply a technique that uses ICESat-2 repeat-track laser altimetry to locate the inland limit of tidal ice shelf flexure for each sampled tide, enabling the magnitude and temporal variability of tidal GL migration to be resolved. We demonstrate its application at an ice plain north of Bungenstockrücken, in a region of the southern Ronne Ice Shelf subject to large ocean tides. We observe a 1,300 km 2 area of ephemeral grounding over which the GL migrates by up to 15 km between low and high tide, and identify four distinct modes of migration: “linear”, “asymmetric”, “threshold” and “hysteresis”. The short-term movement of the GL dominates any long-term migration signal in this location, and the distribution of GL positions and modes contains information about spatial variability in the ice-bed interface. We discuss the impact of extreme tidal GL migration on ice shelf-ocean-subglacial systems in Antarctica and make recommendations for how GLs should be more precisely defined and documented in future by the community. Text Antarc* Antarctic Antarctica Ice Sheet Ice Shelf Ronne Ice Shelf Copernicus Publications: E-Journals Antarctic Bungenstockrücken ENVELOPE(-69.000,-69.000,-81.500,-81.500) Ronne Ice Shelf ENVELOPE(-61.000,-61.000,-78.500,-78.500)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Short-term tidal grounding line (GL) migration in Antarctica can impact ice dynamics at the ice sheet margins and obscures assessments of long-term GL advance or retreat. However, the magnitude of tidally-induced GL migration is poorly known, and the spatial pattern and modes of variability are not well characterised. Here we develop and apply a technique that uses ICESat-2 repeat-track laser altimetry to locate the inland limit of tidal ice shelf flexure for each sampled tide, enabling the magnitude and temporal variability of tidal GL migration to be resolved. We demonstrate its application at an ice plain north of Bungenstockrücken, in a region of the southern Ronne Ice Shelf subject to large ocean tides. We observe a 1,300 km 2 area of ephemeral grounding over which the GL migrates by up to 15 km between low and high tide, and identify four distinct modes of migration: “linear”, “asymmetric”, “threshold” and “hysteresis”. The short-term movement of the GL dominates any long-term migration signal in this location, and the distribution of GL positions and modes contains information about spatial variability in the ice-bed interface. We discuss the impact of extreme tidal GL migration on ice shelf-ocean-subglacial systems in Antarctica and make recommendations for how GLs should be more precisely defined and documented in future by the community.
format Text
author Freer, Bryony I. D.
Marsh, Oliver J.
Hogg, Anna E.
Fricker, Helen Amanda
Padman, Laurie
spellingShingle Freer, Bryony I. D.
Marsh, Oliver J.
Hogg, Anna E.
Fricker, Helen Amanda
Padman, Laurie
Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry
author_facet Freer, Bryony I. D.
Marsh, Oliver J.
Hogg, Anna E.
Fricker, Helen Amanda
Padman, Laurie
author_sort Freer, Bryony I. D.
title Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry
title_short Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry
title_full Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry
title_fullStr Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry
title_full_unstemmed Modes of Antarctic tidal grounding line migration revealed by ICESat-2 laser altimetry
title_sort modes of antarctic tidal grounding line migration revealed by icesat-2 laser altimetry
publishDate 2023
url https://doi.org/10.5194/tc-2022-265
https://tc.copernicus.org/preprints/tc-2022-265/
long_lat ENVELOPE(-69.000,-69.000,-81.500,-81.500)
ENVELOPE(-61.000,-61.000,-78.500,-78.500)
geographic Antarctic
Bungenstockrücken
Ronne Ice Shelf
geographic_facet Antarctic
Bungenstockrücken
Ronne Ice Shelf
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ronne Ice Shelf
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Ice Shelf
Ronne Ice Shelf
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2022-265
https://tc.copernicus.org/preprints/tc-2022-265/
op_doi https://doi.org/10.5194/tc-2022-265
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