Kamb Ice Stream flow history and surge potential

A basal zone, tens of meters thick, of debris-laden ice was observed in Kamb Ice Stream, West Antarctica, using a video camera lowered into boreholes made by hot-water drilling. The debris content varies, sometimes abruptly, forming a sequence of layers that reflect the complex history of fast ice f...

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Published in:Annals of Glaciology
Main Authors: Engelhardt, Hermann, Kamb, Barclay
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 2013
Subjects:
Online Access:https://doi.org/10.3189/2013AoG63A535
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spelling ftcaltechauth:oai:authors.library.caltech.edu:hnzkp-dws78 2024-10-20T14:02:59+00:00 Kamb Ice Stream flow history and surge potential Engelhardt, Hermann Kamb, Barclay 2013-07-01 https://doi.org/10.3189/2013AoG63A535 unknown International Glaciological Society https://doi.org/10.3189/2013AoG63A535 eprintid:40909 info:eu-repo/semantics/openAccess Other Annals of Glaciology, 54(63), 287-298, (2013-07-01) info:eu-repo/semantics/article 2013 ftcaltechauth https://doi.org/10.3189/2013AoG63A535 2024-09-25T18:46:41Z A basal zone, tens of meters thick, of debris-laden ice was observed in Kamb Ice Stream, West Antarctica, using a video camera lowered into boreholes made by hot-water drilling. The debris content varies, sometimes abruptly, forming a sequence of layers that reflect the complex history of fast ice flow and bed interaction. In most parts, the concentration of debris is low, a few percent by weight, with particles, often mud clots, dispersed in a matrix of clear ice. The nature of the debris distribution can be interpreted in terms of specific time intervals in the history of fast motion of Kamb Ice Stream including processes leading up to the termination of its streaming behavior and possible reactivation. © 2013 International Glaciological Society. Publication date: 2013-07-01. The results presented here are based on a research program initiated by the visionary Barclay Kamb, who persisted in studying the basal conditions of fast-moving glaciers and ice streams in situ. I am extremely grateful for his keen interest and constant support. I am very grateful to our field assistants, who showed great enthusiasm and unrelenting dedication even under demanding circumstances. The 2000/ 01 drilling team included Shulamit Gordon, Matt Bachmann, Daniel Abrams, Stefan Vogel, Regina Sterr, Kate Batten, Michele Koppes and Robin Bolsey. The JPL/Caltech camera design team also included Frank Carsey, Lonne Lane, Robert Ivlev, Ken Manatt, Kobie Boykins, Jason Feldman, Fabien Nicaise, Kai Zhu and Alberto Behar. Alberto Behar was also crucial for the video image acquisition. Bjorn Johns of the University Navstar Consortium (UNAVCO) helped with the precision GPS measurements. The comments of my reviewers and editors greatly improved the paper. I also appreciate the help of a great number of support people, especially my late wife Luise Engelhardt. The US National Science Foundation Office of Polar Programs funded this work under grant OPP-9615420. Published - Engelhardt_2013p287.pdf Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctica Kamb Ice Stream National Science Foundation Office of Polar Programs West Antarctica Caltech Authors (California Institute of Technology) Abrams ENVELOPE(-72.425,-72.425,-75.365,-75.365) Barclay ENVELOPE(-61.000,-61.000,-62.600,-62.600) Ivlev ENVELOPE(156.303,156.303,52.975,52.975) Kamb Ice Stream ENVELOPE(-145.000,-145.000,-82.250,-82.250) Regina ENVELOPE(165.750,165.750,-71.450,-71.450) West Antarctica Annals of Glaciology 54 63 287 298
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language unknown
description A basal zone, tens of meters thick, of debris-laden ice was observed in Kamb Ice Stream, West Antarctica, using a video camera lowered into boreholes made by hot-water drilling. The debris content varies, sometimes abruptly, forming a sequence of layers that reflect the complex history of fast ice flow and bed interaction. In most parts, the concentration of debris is low, a few percent by weight, with particles, often mud clots, dispersed in a matrix of clear ice. The nature of the debris distribution can be interpreted in terms of specific time intervals in the history of fast motion of Kamb Ice Stream including processes leading up to the termination of its streaming behavior and possible reactivation. © 2013 International Glaciological Society. Publication date: 2013-07-01. The results presented here are based on a research program initiated by the visionary Barclay Kamb, who persisted in studying the basal conditions of fast-moving glaciers and ice streams in situ. I am extremely grateful for his keen interest and constant support. I am very grateful to our field assistants, who showed great enthusiasm and unrelenting dedication even under demanding circumstances. The 2000/ 01 drilling team included Shulamit Gordon, Matt Bachmann, Daniel Abrams, Stefan Vogel, Regina Sterr, Kate Batten, Michele Koppes and Robin Bolsey. The JPL/Caltech camera design team also included Frank Carsey, Lonne Lane, Robert Ivlev, Ken Manatt, Kobie Boykins, Jason Feldman, Fabien Nicaise, Kai Zhu and Alberto Behar. Alberto Behar was also crucial for the video image acquisition. Bjorn Johns of the University Navstar Consortium (UNAVCO) helped with the precision GPS measurements. The comments of my reviewers and editors greatly improved the paper. I also appreciate the help of a great number of support people, especially my late wife Luise Engelhardt. The US National Science Foundation Office of Polar Programs funded this work under grant OPP-9615420. Published - Engelhardt_2013p287.pdf
format Article in Journal/Newspaper
author Engelhardt, Hermann
Kamb, Barclay
spellingShingle Engelhardt, Hermann
Kamb, Barclay
Kamb Ice Stream flow history and surge potential
author_facet Engelhardt, Hermann
Kamb, Barclay
author_sort Engelhardt, Hermann
title Kamb Ice Stream flow history and surge potential
title_short Kamb Ice Stream flow history and surge potential
title_full Kamb Ice Stream flow history and surge potential
title_fullStr Kamb Ice Stream flow history and surge potential
title_full_unstemmed Kamb Ice Stream flow history and surge potential
title_sort kamb ice stream flow history and surge potential
publisher International Glaciological Society
publishDate 2013
url https://doi.org/10.3189/2013AoG63A535
long_lat ENVELOPE(-72.425,-72.425,-75.365,-75.365)
ENVELOPE(-61.000,-61.000,-62.600,-62.600)
ENVELOPE(156.303,156.303,52.975,52.975)
ENVELOPE(-145.000,-145.000,-82.250,-82.250)
ENVELOPE(165.750,165.750,-71.450,-71.450)
geographic Abrams
Barclay
Ivlev
Kamb Ice Stream
Regina
West Antarctica
geographic_facet Abrams
Barclay
Ivlev
Kamb Ice Stream
Regina
West Antarctica
genre Annals of Glaciology
Antarc*
Antarctica
Kamb Ice Stream
National Science Foundation Office of Polar Programs
West Antarctica
genre_facet Annals of Glaciology
Antarc*
Antarctica
Kamb Ice Stream
National Science Foundation Office of Polar Programs
West Antarctica
op_source Annals of Glaciology, 54(63), 287-298, (2013-07-01)
op_relation https://doi.org/10.3189/2013AoG63A535
eprintid:40909
op_rights info:eu-repo/semantics/openAccess
Other
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container_title Annals of Glaciology
container_volume 54
container_issue 63
container_start_page 287
op_container_end_page 298
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