Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain
Ice discharge from the Greenland ice sheet is controlled by tidewater glacier flow speed, which shows significant variations in different timescales. Short-term speed variations are key to understanding the physical processes controlling glacial motion, but studies are sparse for Greenlandic tidewat...
Main Authors: | , , , , , , , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2024
|
Subjects: | |
Online Access: | https://doi.org/10.5194/egusphere-2024-1476 https://noa.gwlb.de/receive/cop_mods_00073897 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00072032/egusphere-2024-1476.pdf https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1476/egusphere-2024-1476.pdf |
id |
ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00073897 |
---|---|
record_format |
openpolar |
spelling |
ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00073897 2024-06-23T07:53:00+00:00 Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain Sugiyama, Shin Tsutaki, Shun Sakakibara, Daiki Asaji, Izumi Kondo, Ken Wang, Yefan Podolskiy, Evgeny Jouvet, Guillaume Funk, Martin 2024-05 electronic https://doi.org/10.5194/egusphere-2024-1476 https://noa.gwlb.de/receive/cop_mods_00073897 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00072032/egusphere-2024-1476.pdf https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1476/egusphere-2024-1476.pdf eng eng Copernicus Publications https://doi.org/10.5194/egusphere-2024-1476 https://noa.gwlb.de/receive/cop_mods_00073897 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00072032/egusphere-2024-1476.pdf https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1476/egusphere-2024-1476.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2024 ftnonlinearchiv https://doi.org/10.5194/egusphere-2024-1476 2024-06-03T23:38:30Z Ice discharge from the Greenland ice sheet is controlled by tidewater glacier flow speed, which shows significant variations in different timescales. Short-term speed variations are key to understanding the physical processes controlling glacial motion, but studies are sparse for Greenlandic tidewater glaciers, particularly near the calving front. Here, we present high-frequency ice speed measurements performed at 0.5–4 km from the front of Bowdoin Glacier, a tidewater glacier in northwestern Greenland. Three GPS (global positioning system) receivers were operated for several weeks in July of 2013–2017 and 2019. Horizontal ice speed varied over timescales of hours to days, including short-term speed-up events as well as diurnal and semidiurnal variations. Frequency analysis revealed that semidiurnal signals decay upglacier, whereas diurnal signals are consistently observed over the area of study. Speed-up events were associated with heavy rain, and longer-term variations were correlated with air temperature. Uplift of the glacier surface was observed during fast-flowing periods, suggesting basal separation due to elevated water pressure. These observations confirm the strong and immediate impact of melt/rainwater on subglacial water pressure and sliding speed. Tidally modulated ice speed peaks coincided with or slightly before low tide, which demonstrates the key role viscoelastic ice dynamics play in response to changing hydrostatic pressure acting on the glacier front. Our study results reveal details of short-term flow variations near the front of a Greenlandic tidewater glacier and provide insights into calving glacier dynamics. During melt season, ice speed is controlled by atmospheric conditions through meltwater production and rain events as commonly observed in alpine glaciers, but additional complexity arises from tidal influence near the calving front. Article in Journal/Newspaper glacier Greenland greenlandic Ice Sheet Tidewater Niedersächsisches Online-Archiv NOA Bowdoin ENVELOPE(-69.317,-69.317,77.683,77.683) Greenland |
institution |
Open Polar |
collection |
Niedersächsisches Online-Archiv NOA |
op_collection_id |
ftnonlinearchiv |
language |
English |
topic |
article Verlagsveröffentlichung |
spellingShingle |
article Verlagsveröffentlichung Sugiyama, Shin Tsutaki, Shun Sakakibara, Daiki Asaji, Izumi Kondo, Ken Wang, Yefan Podolskiy, Evgeny Jouvet, Guillaume Funk, Martin Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain |
topic_facet |
article Verlagsveröffentlichung |
description |
Ice discharge from the Greenland ice sheet is controlled by tidewater glacier flow speed, which shows significant variations in different timescales. Short-term speed variations are key to understanding the physical processes controlling glacial motion, but studies are sparse for Greenlandic tidewater glaciers, particularly near the calving front. Here, we present high-frequency ice speed measurements performed at 0.5–4 km from the front of Bowdoin Glacier, a tidewater glacier in northwestern Greenland. Three GPS (global positioning system) receivers were operated for several weeks in July of 2013–2017 and 2019. Horizontal ice speed varied over timescales of hours to days, including short-term speed-up events as well as diurnal and semidiurnal variations. Frequency analysis revealed that semidiurnal signals decay upglacier, whereas diurnal signals are consistently observed over the area of study. Speed-up events were associated with heavy rain, and longer-term variations were correlated with air temperature. Uplift of the glacier surface was observed during fast-flowing periods, suggesting basal separation due to elevated water pressure. These observations confirm the strong and immediate impact of melt/rainwater on subglacial water pressure and sliding speed. Tidally modulated ice speed peaks coincided with or slightly before low tide, which demonstrates the key role viscoelastic ice dynamics play in response to changing hydrostatic pressure acting on the glacier front. Our study results reveal details of short-term flow variations near the front of a Greenlandic tidewater glacier and provide insights into calving glacier dynamics. During melt season, ice speed is controlled by atmospheric conditions through meltwater production and rain events as commonly observed in alpine glaciers, but additional complexity arises from tidal influence near the calving front. |
format |
Article in Journal/Newspaper |
author |
Sugiyama, Shin Tsutaki, Shun Sakakibara, Daiki Asaji, Izumi Kondo, Ken Wang, Yefan Podolskiy, Evgeny Jouvet, Guillaume Funk, Martin |
author_facet |
Sugiyama, Shin Tsutaki, Shun Sakakibara, Daiki Asaji, Izumi Kondo, Ken Wang, Yefan Podolskiy, Evgeny Jouvet, Guillaume Funk, Martin |
author_sort |
Sugiyama, Shin |
title |
Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain |
title_short |
Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain |
title_full |
Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain |
title_fullStr |
Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain |
title_full_unstemmed |
Ice speed of a Greenlandic tidewater glacier modulated by tide, melt, and rain |
title_sort |
ice speed of a greenlandic tidewater glacier modulated by tide, melt, and rain |
publisher |
Copernicus Publications |
publishDate |
2024 |
url |
https://doi.org/10.5194/egusphere-2024-1476 https://noa.gwlb.de/receive/cop_mods_00073897 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00072032/egusphere-2024-1476.pdf https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1476/egusphere-2024-1476.pdf |
long_lat |
ENVELOPE(-69.317,-69.317,77.683,77.683) |
geographic |
Bowdoin Greenland |
geographic_facet |
Bowdoin Greenland |
genre |
glacier Greenland greenlandic Ice Sheet Tidewater |
genre_facet |
glacier Greenland greenlandic Ice Sheet Tidewater |
op_relation |
https://doi.org/10.5194/egusphere-2024-1476 https://noa.gwlb.de/receive/cop_mods_00073897 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00072032/egusphere-2024-1476.pdf https://egusphere.copernicus.org/preprints/2024/egusphere-2024-1476/egusphere-2024-1476.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/egusphere-2024-1476 |
_version_ |
1802644477535322112 |