High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica
Dalk Glacier, which has been monitored by CHINARE since 2007, is a calving outlet glacier near the Chinese Zhongshan Station in East Antarctica. Using in situ observational azimuthal data from 2007 to 2012, 67 high-precision spatial intersection points were calculated. Consequently, the ice-flow fea...
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Format: | Article in Journal/Newspaper |
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ftnipr:oai:nipr.repo.nii.ac.jp:00015597 2023-05-15T13:49:00+02:00 High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica 2019-03 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15597 http://id.nii.ac.jp/1291/00015492/ en eng https://doi.org/10.1016/j.polar.2018.09.003 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15597 http://id.nii.ac.jp/1291/00015492/ Polar Science, 19, 13-23(2019-03) 18739652 Bedrock rise Dalk glacier East Antarctica Ice-flow velocity Surface fluctuation Journal Article 2019 ftnipr https://doi.org/10.1016/j.polar.2018.09.003 2022-12-03T19:43:10Z Dalk Glacier, which has been monitored by CHINARE since 2007, is a calving outlet glacier near the Chinese Zhongshan Station in East Antarctica. Using in situ observational azimuthal data from 2007 to 2012, 67 high-precision spatial intersection points were calculated. Consequently, the ice-flow features of the tongue of Dalk Glacier were explored via ground measurements. The maximum observed ice-flow velocity (IV) was 192.72 m/a, at stake P9. The velocities then decreased with the distance from the central flow line on both sides of the glacier in a cross section. Further analysis showed the following: the velocities of each stake increased annually; the closer to the terminus, the faster the ice flowed; and the ascent ratio of the IVs was approximately 10.67 m/a2 in the main flow area. We also observed seasonal variations in the ice-flow velocities, including a speed-up in January 2009 preceding an ice-calving event. The elevation change measurements at the stakes showed fluctuations along the central flow line, which indicates ice-shelf grounding over a seamount that had not been previously identified. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ice Shelf Polar Science Polar Science National Institute of Polar Research Repository, Japan East Antarctica Zhongshan ENVELOPE(76.371,76.371,-69.373,-69.373) Zhongshan Station ENVELOPE(76.371,76.371,-69.373,-69.373) Polar Science 19 13 23 |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
Bedrock rise Dalk glacier East Antarctica Ice-flow velocity Surface fluctuation |
spellingShingle |
Bedrock rise Dalk glacier East Antarctica Ice-flow velocity Surface fluctuation High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica |
topic_facet |
Bedrock rise Dalk glacier East Antarctica Ice-flow velocity Surface fluctuation |
description |
Dalk Glacier, which has been monitored by CHINARE since 2007, is a calving outlet glacier near the Chinese Zhongshan Station in East Antarctica. Using in situ observational azimuthal data from 2007 to 2012, 67 high-precision spatial intersection points were calculated. Consequently, the ice-flow features of the tongue of Dalk Glacier were explored via ground measurements. The maximum observed ice-flow velocity (IV) was 192.72 m/a, at stake P9. The velocities then decreased with the distance from the central flow line on both sides of the glacier in a cross section. Further analysis showed the following: the velocities of each stake increased annually; the closer to the terminus, the faster the ice flowed; and the ascent ratio of the IVs was approximately 10.67 m/a2 in the main flow area. We also observed seasonal variations in the ice-flow velocities, including a speed-up in January 2009 preceding an ice-calving event. The elevation change measurements at the stakes showed fluctuations along the central flow line, which indicates ice-shelf grounding over a seamount that had not been previously identified. |
format |
Article in Journal/Newspaper |
title |
High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica |
title_short |
High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica |
title_full |
High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica |
title_fullStr |
High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica |
title_full_unstemmed |
High-precision ice-flow velocities from ground observations on Dalk Glacier, Antarctica |
title_sort |
high-precision ice-flow velocities from ground observations on dalk glacier, antarctica |
publishDate |
2019 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15597 http://id.nii.ac.jp/1291/00015492/ |
long_lat |
ENVELOPE(76.371,76.371,-69.373,-69.373) ENVELOPE(76.371,76.371,-69.373,-69.373) |
geographic |
East Antarctica Zhongshan Zhongshan Station |
geographic_facet |
East Antarctica Zhongshan Zhongshan Station |
genre |
Antarc* Antarctica East Antarctica Ice Shelf Polar Science Polar Science |
genre_facet |
Antarc* Antarctica East Antarctica Ice Shelf Polar Science Polar Science |
op_relation |
https://doi.org/10.1016/j.polar.2018.09.003 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=15597 http://id.nii.ac.jp/1291/00015492/ Polar Science, 19, 13-23(2019-03) 18739652 |
op_doi |
https://doi.org/10.1016/j.polar.2018.09.003 |
container_title |
Polar Science |
container_volume |
19 |
container_start_page |
13 |
op_container_end_page |
23 |
_version_ |
1766250383992160256 |