Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica

P(論文) Streamlined bedforms and small erosional marks observed on the Soya Coast, East Antarctica, are interpreted to have been formed by subglacial meltwater The source of water is attributed to subglacial lakes that may have existed beneath the upper part of the Mizuho Plateau In order to evaluate...

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Main Authors: Sawagaki ,Takanobu, Hirakawa ,Kazuomi
Language:English
Published: National Institute of Polar Research 2002
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/3114/files/KJ00000044232.pdf
https://doi.org/10.15094/00003114
https://nipr.repo.nii.ac.jp/records/3114
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author Sawagaki ,Takanobu
Hirakawa ,Kazuomi
author_facet Sawagaki ,Takanobu
Hirakawa ,Kazuomi
author_sort Sawagaki ,Takanobu
collection National Institute of Polar Research Repository, Japan
description P(論文) Streamlined bedforms and small erosional marks observed on the Soya Coast, East Antarctica, are interpreted to have been formed by subglacial meltwater The source of water is attributed to subglacial lakes that may have existed beneath the upper part of the Mizuho Plateau In order to evaluate the subglacial meltwater hypothesis, two theoretical investigations were carried out, one to model the formation of subglacial lakes in the Shirase drainage basin, and the second to estimate the conformity of water flow beneath the ice sheet to underlying topography In the first investigation we found that several subglacial lakes would have formed in the bed depressions with the water surfaces determined by englacial equipotential surfaces In the second investigation, several ice thicknesses and their surface gradients were determined in which agreement between potential gradients and the observed bedform distribution was found These experimental results add to the existing observations and inductive reasoning supporting a subglacial hydraulic origin for bedforms along the Soya Coast According to the results, possible causes of sudden subglacial outburst floods and their influence are discussed If subglacial water storage and sudden discharge occurred, a combination of water accumulation beneath the ice sheet and discharge of this water could make the ice sheet unstable leading to the rapid melting of the ice sheet supplying huge amount of meltwater to the ocean and formation of local ice streams Such subglacial meltwater events in Antarctica possibly contributed some global meltwater pulse events during MIS-3 or post-LGM periods departmental bulletin paper
genre Antarc*
Antarctica
East Antarctica
Ice Sheet
Polar geoscience
genre_facet Antarc*
Antarctica
East Antarctica
Ice Sheet
Polar geoscience
geographic East Antarctica
Mizuho
Mizuho Plateau
geographic_facet East Antarctica
Mizuho
Mizuho Plateau
id ftnipr:oai:nipr.repo.nii.ac.jp:00003114
institution Open Polar
language English
long_lat ENVELOPE(44.317,44.317,-70.683,-70.683)
ENVELOPE(40.000,40.000,-73.000,-73.000)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00003114
op_relation Polar geoscience
15
123
147
AA1130866X
https://nipr.repo.nii.ac.jp/record/3114/files/KJ00000044232.pdf
https://doi.org/10.15094/00003114
https://nipr.repo.nii.ac.jp/records/3114
publishDate 2002
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00003114 2025-04-13T14:08:38+00:00 Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica Sawagaki ,Takanobu Hirakawa ,Kazuomi 2002-10 application/pdf https://nipr.repo.nii.ac.jp/record/3114/files/KJ00000044232.pdf https://doi.org/10.15094/00003114 https://nipr.repo.nii.ac.jp/records/3114 eng eng National Institute of Polar Research Polar geoscience 15 123 147 AA1130866X https://nipr.repo.nii.ac.jp/record/3114/files/KJ00000044232.pdf https://doi.org/10.15094/00003114 https://nipr.repo.nii.ac.jp/records/3114 streamlined bedform subglacial lake meltwater East Antarctica 2002 ftnipr https://doi.org/10.15094/00003114 2025-03-19T10:19:57Z P(論文) Streamlined bedforms and small erosional marks observed on the Soya Coast, East Antarctica, are interpreted to have been formed by subglacial meltwater The source of water is attributed to subglacial lakes that may have existed beneath the upper part of the Mizuho Plateau In order to evaluate the subglacial meltwater hypothesis, two theoretical investigations were carried out, one to model the formation of subglacial lakes in the Shirase drainage basin, and the second to estimate the conformity of water flow beneath the ice sheet to underlying topography In the first investigation we found that several subglacial lakes would have formed in the bed depressions with the water surfaces determined by englacial equipotential surfaces In the second investigation, several ice thicknesses and their surface gradients were determined in which agreement between potential gradients and the observed bedform distribution was found These experimental results add to the existing observations and inductive reasoning supporting a subglacial hydraulic origin for bedforms along the Soya Coast According to the results, possible causes of sudden subglacial outburst floods and their influence are discussed If subglacial water storage and sudden discharge occurred, a combination of water accumulation beneath the ice sheet and discharge of this water could make the ice sheet unstable leading to the rapid melting of the ice sheet supplying huge amount of meltwater to the ocean and formation of local ice streams Such subglacial meltwater events in Antarctica possibly contributed some global meltwater pulse events during MIS-3 or post-LGM periods departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Ice Sheet Polar geoscience National Institute of Polar Research Repository, Japan East Antarctica Mizuho ENVELOPE(44.317,44.317,-70.683,-70.683) Mizuho Plateau ENVELOPE(40.000,40.000,-73.000,-73.000)
spellingShingle streamlined bedform
subglacial lake
meltwater
East Antarctica
Sawagaki ,Takanobu
Hirakawa ,Kazuomi
Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica
title Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica
title_full Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica
title_fullStr Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica
title_full_unstemmed Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica
title_short Hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, East Antarctica
title_sort hydrostatic investigations on subglacial meltwater: implications for the formation of streamlined bedforms and subglacial lakes, east antarctica
topic streamlined bedform
subglacial lake
meltwater
East Antarctica
topic_facet streamlined bedform
subglacial lake
meltwater
East Antarctica
url https://nipr.repo.nii.ac.jp/record/3114/files/KJ00000044232.pdf
https://doi.org/10.15094/00003114
https://nipr.repo.nii.ac.jp/records/3114