Subglacial lake activity beneath the ablation zone of the Greenland Ice Sheet

<p>Hydrologically active subglacial lakes can drain large volumes of water and sediment along subglacial pathways, affecting the motion and mass balance of ice masses and impacting downstream sediment dynamics. To date, only eight active lakes have been reported beneath the Greenland Ice Sheet...

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Main Authors: Y. Fan, C.-Q. Ke, X. Shen, Y. Xiao, S. J. Livingstone, A. J. Sole
Format: Article
Language:English
Published: Copernicus Publications 2023-04-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/17/1775/2023/tc-17-1775-2023.pdf
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author Y. Fan
Y. Fan
Y. Fan
C.-Q. Ke
C.-Q. Ke
C.-Q. Ke
X. Shen
X. Shen
X. Shen
Y. Xiao
Y. Xiao
Y. Xiao
S. J. Livingstone
A. J. Sole
author_facet Y. Fan
Y. Fan
Y. Fan
C.-Q. Ke
C.-Q. Ke
C.-Q. Ke
X. Shen
X. Shen
X. Shen
Y. Xiao
Y. Xiao
Y. Xiao
S. J. Livingstone
A. J. Sole
author_sort Y. Fan
collection DOAJ
description <p>Hydrologically active subglacial lakes can drain large volumes of water and sediment along subglacial pathways, affecting the motion and mass balance of ice masses and impacting downstream sediment dynamics. To date, only eight active lakes have been reported beneath the Greenland Ice Sheet (GrIS), and thus the understanding of their spatial distribution and dynamic processes is still lacking. Here, using ICESat-2 (Ice, Cloud, and land Elevation Satellite-2) ATL11 data, we identify 18 active subglacial lakes, 16 of which have not been previously reported. Multi-temporal ArcticDEM (digital elevation model of the Arctic) strip maps were used to extend the time series to verify lakes and determine their drainage history. The identification of active subglacial lakes beneath the GrIS is complicated by the occurrence of supraglacial lakes, which also fill and drain and are hypothesized to be almost co-located. We therefore used the temporal pattern of ice-surface elevation change to discriminate subglacial lakes and utilized the ability of ICESat-2 to penetrate through surface water to correct the elevation provided by the ATL11 data. A significant localized elevation anomaly (<span class="inline-formula">−16.03</span>–10.30 m yr<span class="inline-formula"><sup>−1</sup></span>) was measured in all detected subglacial lakes after correction, revealing that six subglacial lakes are twinned with supraglacial lakes. The active subglacial lakes have large upstream hydrological catchments and are located near or below the equilibrium line. Lakes have a median area of 1.20 km<span class="inline-formula"><sup>2</sup></span>, and 12 lakes exhibited positive elevation-change rates during the ICESat-2 period. These observations illustrate the potential for combining ICESat-2 and the ArcticDEM to differentiate small subglacial lakes in the ablation zone and beneath supraglacial lakes.</p>
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spelling doaj.art-0b88a14ba491487b95a980a6b6638eee2023-04-26T09:30:20ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242023-04-01171775178610.5194/tc-17-1775-2023Subglacial lake activity beneath the ablation zone of the Greenland Ice SheetY. Fan0Y. Fan1Y. Fan2C.-Q. Ke3C.-Q. Ke4C.-Q. Ke5X. Shen6X. Shen7X. Shen8Y. Xiao9Y. Xiao10Y. Xiao11S. J. Livingstone12A. J. Sole13Jiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, ChinaCollaborative Innovation Center of Novel Software Technology and Industrialization, Nanjing, 210023, ChinaCollaborative Innovation Center of South China Sea Studies, Nanjing, 210023, ChinaJiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, ChinaCollaborative Innovation Center of Novel Software Technology and Industrialization, Nanjing, 210023, ChinaCollaborative Innovation Center of South China Sea Studies, Nanjing, 210023, ChinaJiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, ChinaCollaborative Innovation Center of Novel Software Technology and Industrialization, Nanjing, 210023, ChinaCollaborative Innovation Center of South China Sea Studies, Nanjing, 210023, ChinaJiangsu Provincial Key Laboratory of Geographic Information Science and Technology, Key Laboratory for Land Satellite Remote Sensing Applications of Ministry of Natural Resources, School of Geography and Ocean Science, Nanjing University, Nanjing, 210023, ChinaCollaborative Innovation Center of Novel Software Technology and Industrialization, Nanjing, 210023, ChinaCollaborative Innovation Center of South China Sea Studies, Nanjing, 210023, ChinaDepartment of Geography, University of Sheffield, Sheffield, S10 2TN, UKDepartment of Geography, University of Sheffield, Sheffield, S10 2TN, UK<p>Hydrologically active subglacial lakes can drain large volumes of water and sediment along subglacial pathways, affecting the motion and mass balance of ice masses and impacting downstream sediment dynamics. To date, only eight active lakes have been reported beneath the Greenland Ice Sheet (GrIS), and thus the understanding of their spatial distribution and dynamic processes is still lacking. Here, using ICESat-2 (Ice, Cloud, and land Elevation Satellite-2) ATL11 data, we identify 18 active subglacial lakes, 16 of which have not been previously reported. Multi-temporal ArcticDEM (digital elevation model of the Arctic) strip maps were used to extend the time series to verify lakes and determine their drainage history. The identification of active subglacial lakes beneath the GrIS is complicated by the occurrence of supraglacial lakes, which also fill and drain and are hypothesized to be almost co-located. We therefore used the temporal pattern of ice-surface elevation change to discriminate subglacial lakes and utilized the ability of ICESat-2 to penetrate through surface water to correct the elevation provided by the ATL11 data. A significant localized elevation anomaly (<span class="inline-formula">−16.03</span>–10.30 m yr<span class="inline-formula"><sup>−1</sup></span>) was measured in all detected subglacial lakes after correction, revealing that six subglacial lakes are twinned with supraglacial lakes. The active subglacial lakes have large upstream hydrological catchments and are located near or below the equilibrium line. Lakes have a median area of 1.20 km<span class="inline-formula"><sup>2</sup></span>, and 12 lakes exhibited positive elevation-change rates during the ICESat-2 period. These observations illustrate the potential for combining ICESat-2 and the ArcticDEM to differentiate small subglacial lakes in the ablation zone and beneath supraglacial lakes.</p>https://tc.copernicus.org/articles/17/1775/2023/tc-17-1775-2023.pdf
spellingShingle Y. Fan
Y. Fan
Y. Fan
C.-Q. Ke
C.-Q. Ke
C.-Q. Ke
X. Shen
X. Shen
X. Shen
Y. Xiao
Y. Xiao
Y. Xiao
S. J. Livingstone
A. J. Sole
Subglacial lake activity beneath the ablation zone of the Greenland Ice Sheet
The Cryosphere
title Subglacial lake activity beneath the ablation zone of the Greenland Ice Sheet
title_full Subglacial lake activity beneath the ablation zone of the Greenland Ice Sheet
title_fullStr Subglacial lake activity beneath the ablation zone of the Greenland Ice Sheet
title_full_unstemmed Subglacial lake activity beneath the ablation zone of the Greenland Ice Sheet
title_short Subglacial lake activity beneath the ablation zone of the Greenland Ice Sheet
title_sort subglacial lake activity beneath the ablation zone of the greenland ice sheet
url https://tc.copernicus.org/articles/17/1775/2023/tc-17-1775-2023.pdf
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