Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ...

Drainage of supraglacial lakes to the ice-sheet bed can occur when a hydrofracture propagates downward, driven by the weight of the water in the lake. For supraglacial lakes in the grounding zones of Antarctic glaciers, the mechanics of drainage is complicated by their proximity to the grounding lin...

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Bibliographic Details
Main Authors: Zhang, Hanwen, Katz, Richard F., Stevens, Laura A.
Format: Article in Journal/Newspaper
Language:unknown
Published: arXiv 2023
Subjects:
Online Access:https://dx.doi.org/10.48550/arxiv.2311.01249
https://arxiv.org/abs/2311.01249
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author Zhang, Hanwen
Katz, Richard F.
Stevens, Laura A.
author_facet Zhang, Hanwen
Katz, Richard F.
Stevens, Laura A.
author_sort Zhang, Hanwen
collection DataCite
description Drainage of supraglacial lakes to the ice-sheet bed can occur when a hydrofracture propagates downward, driven by the weight of the water in the lake. For supraglacial lakes in the grounding zones of Antarctic glaciers, the mechanics of drainage is complicated by their proximity to the grounding line. Recently, a series of supraglacial lake-drainage events through hydrofractures was observed in the Amery Ice Shelf grounding zone, East Antarctica. The lake depth at drainage varied considerably between events, raising questions about the mechanisms that induce hydrofracture, even at low lake depths. Here we use a modelling approach to investigate the contribution of tidally driven flexure to hydrofracture propagation. We model the viscoelastic response of a marine ice sheet to tides, the stresses that are induced, and the contribution of tidal stresses to hydrofracture propagation. Our results show that ocean tides and lake-water pressure together control supraglacial lake drainage through hydrofractures in ... : 23 pages, 10 figures ...
format Article in Journal/Newspaper
genre Amery Ice Shelf
Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
genre_facet Amery Ice Shelf
Antarc*
Antarctic
Antarctica
East Antarctica
Ice Sheet
Ice Shelf
geographic Amery
Amery Ice Shelf
Antarctic
East Antarctica
Low Lake
geographic_facet Amery
Amery Ice Shelf
Antarctic
East Antarctica
Low Lake
id ftdatacite:10.48550/arxiv.2311.01249
institution Open Polar
language unknown
long_lat ENVELOPE(-94.063,-94.063,56.565,56.565)
ENVELOPE(71.000,71.000,-69.750,-69.750)
ENVELOPE(142.677,142.677,-66.993,-66.993)
op_collection_id ftdatacite
op_doi https://doi.org/10.48550/arxiv.2311.01249
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
publishDate 2023
publisher arXiv
record_format openpolar
spelling ftdatacite:10.48550/arxiv.2311.01249 2025-01-16T18:52:40+00:00 Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ... Zhang, Hanwen Katz, Richard F. Stevens, Laura A. 2023 https://dx.doi.org/10.48550/arxiv.2311.01249 https://arxiv.org/abs/2311.01249 unknown arXiv Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Geophysics physics.geo-ph FOS Physical sciences article Article Preprint CreativeWork 2023 ftdatacite https://doi.org/10.48550/arxiv.2311.01249 2024-04-02T10:26:14Z Drainage of supraglacial lakes to the ice-sheet bed can occur when a hydrofracture propagates downward, driven by the weight of the water in the lake. For supraglacial lakes in the grounding zones of Antarctic glaciers, the mechanics of drainage is complicated by their proximity to the grounding line. Recently, a series of supraglacial lake-drainage events through hydrofractures was observed in the Amery Ice Shelf grounding zone, East Antarctica. The lake depth at drainage varied considerably between events, raising questions about the mechanisms that induce hydrofracture, even at low lake depths. Here we use a modelling approach to investigate the contribution of tidally driven flexure to hydrofracture propagation. We model the viscoelastic response of a marine ice sheet to tides, the stresses that are induced, and the contribution of tidal stresses to hydrofracture propagation. Our results show that ocean tides and lake-water pressure together control supraglacial lake drainage through hydrofractures in ... : 23 pages, 10 figures ... Article in Journal/Newspaper Amery Ice Shelf Antarc* Antarctic Antarctica East Antarctica Ice Sheet Ice Shelf DataCite Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750) Antarctic East Antarctica Low Lake ENVELOPE(142.677,142.677,-66.993,-66.993)
spellingShingle Geophysics physics.geo-ph
FOS Physical sciences
Zhang, Hanwen
Katz, Richard F.
Stevens, Laura A.
Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ...
title Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ...
title_full Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ...
title_fullStr Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ...
title_full_unstemmed Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ...
title_short Viscoelastic mechanics of tidally induced lake drainage in the Amery grounding zone ...
title_sort viscoelastic mechanics of tidally induced lake drainage in the amery grounding zone ...
topic Geophysics physics.geo-ph
FOS Physical sciences
topic_facet Geophysics physics.geo-ph
FOS Physical sciences
url https://dx.doi.org/10.48550/arxiv.2311.01249
https://arxiv.org/abs/2311.01249