Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland
Russell Glacier is a land terminating glacier in South West Greenland. Survey site SHR lies at several kilometers from the terminus and is closely monitored. In recent Summer months research site SHR has seen unusual high ice velocity of 400m/a which has been linked to increased Summer melt. To capt...
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ftawi:oai:epic.awi.de:39384 2024-09-15T18:07:38+00:00 Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland Hofstede, Coen Bohleber, P. Fritzsche, Diedrich Kleiner, Thomas Bondzio, Johannes Hubbard, Alun 2015-04-14 https://epic.awi.de/id/eprint/39384/ http://meetingorganizer.copernicus.org/EGU2015/pico/17131 https://hdl.handle.net/10013/epic.46583 unknown Hofstede, C. orcid:0000-0002-6015-6918 , Bohleber, P. , Fritzsche, D. orcid:0000-0002-0018-8993 , Kleiner, T. orcid:0000-0001-7825-5765 , Bondzio, J. and Hubbard, A. (2015) Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland , EGU General Assembly, Vienna, 12 April 2015 - 17 April 2015 . hdl:10013/epic.46583 info:eu-repo/semantics/openAccess EPIC3EGU General Assembly, Vienna, 2015-04-12-2015-04-17 Conference notRev info:eu-repo/semantics/conferenceObject 2015 ftawi 2024-06-24T04:13:16Z Russell Glacier is a land terminating glacier in South West Greenland. Survey site SHR lies at several kilometers from the terminus and is closely monitored. In recent Summer months research site SHR has seen unusual high ice velocity of 400m/a which has been linked to increased Summer melt. To capture the probably changing basal conditions of SHR we carried out two seismic surveys at site SHR, one in September 2013 at the end of the melt seaasn and one in May 2014 at the start of the melt season. Data were recorded using a 300m snow streamer and explosives. The seismic data reveal an ice thickness of about 550m and 30 to 40m thick accreted subglacial sediments with varying degrees of water saturation. We speculate the increased ice velocity is caused by sediments that become temporarily liquefied in the Summer months. Conference Object glacier Greenland Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
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unknown |
description |
Russell Glacier is a land terminating glacier in South West Greenland. Survey site SHR lies at several kilometers from the terminus and is closely monitored. In recent Summer months research site SHR has seen unusual high ice velocity of 400m/a which has been linked to increased Summer melt. To capture the probably changing basal conditions of SHR we carried out two seismic surveys at site SHR, one in September 2013 at the end of the melt seaasn and one in May 2014 at the start of the melt season. Data were recorded using a 300m snow streamer and explosives. The seismic data reveal an ice thickness of about 550m and 30 to 40m thick accreted subglacial sediments with varying degrees of water saturation. We speculate the increased ice velocity is caused by sediments that become temporarily liquefied in the Summer months. |
format |
Conference Object |
author |
Hofstede, Coen Bohleber, P. Fritzsche, Diedrich Kleiner, Thomas Bondzio, Johannes Hubbard, Alun |
spellingShingle |
Hofstede, Coen Bohleber, P. Fritzsche, Diedrich Kleiner, Thomas Bondzio, Johannes Hubbard, Alun Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland |
author_facet |
Hofstede, Coen Bohleber, P. Fritzsche, Diedrich Kleiner, Thomas Bondzio, Johannes Hubbard, Alun |
author_sort |
Hofstede, Coen |
title |
Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland |
title_short |
Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland |
title_full |
Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland |
title_fullStr |
Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland |
title_full_unstemmed |
Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland |
title_sort |
using reflection seismics to identify and monitor the basal conditions of russell glacier south west greenland |
publishDate |
2015 |
url |
https://epic.awi.de/id/eprint/39384/ http://meetingorganizer.copernicus.org/EGU2015/pico/17131 https://hdl.handle.net/10013/epic.46583 |
genre |
glacier Greenland |
genre_facet |
glacier Greenland |
op_source |
EPIC3EGU General Assembly, Vienna, 2015-04-12-2015-04-17 |
op_relation |
Hofstede, C. orcid:0000-0002-6015-6918 , Bohleber, P. , Fritzsche, D. orcid:0000-0002-0018-8993 , Kleiner, T. orcid:0000-0001-7825-5765 , Bondzio, J. and Hubbard, A. (2015) Using reflection seismics to identify and monitor the basal conditions of Russell Glacier South West Greenland , EGU General Assembly, Vienna, 12 April 2015 - 17 April 2015 . hdl:10013/epic.46583 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1810445024540753920 |