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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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Engelhardt, Hermann, Kamb, Barclay
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2013
Subjects:
Online Access:https://authors.library.caltech.edu/40909/
https://authors.library.caltech.edu/40909/1/Engelhardt_2013p287.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20130822-134141566
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spelling ftcaltechauth:oai:authors.library.caltech.edu:40909 2023-05-15T13:29:40+02:00 Kamb Ice Stream flow history and surge potential Engelhardt, Hermann Kamb, Barclay 2013-07-01 application/pdf https://authors.library.caltech.edu/40909/ https://authors.library.caltech.edu/40909/1/Engelhardt_2013p287.pdf https://resolver.caltech.edu/CaltechAUTHORS:20130822-134141566 en eng International Glaciological Society https://authors.library.caltech.edu/40909/1/Engelhardt_2013p287.pdf Engelhardt, Hermann and Kamb, Barclay (2013) Kamb Ice Stream flow history and surge potential. Annals of Glaciology, 54 (63). pp. 287-298. ISSN 0260-3055. doi:10.3189/2013AoG63A535. https://resolver.caltech.edu/CaltechAUTHORS:20130822-134141566 <https://resolver.caltech.edu/CaltechAUTHORS:20130822-134141566> other Article PeerReviewed 2013 ftcaltechauth https://doi.org/10.3189/2013AoG63A535 2021-11-11T18:54:58Z 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. Article in Journal/Newspaper Annals of Glaciology Antarc* Antarctica Kamb Ice Stream West Antarctica Caltech Authors (California Institute of Technology) Kamb Ice Stream ENVELOPE(-145.000,-145.000,-82.250,-82.250) West Antarctica Annals of Glaciology 54 63 287 298
institution Open Polar
collection Caltech Authors (California Institute of Technology)
op_collection_id ftcaltechauth
language English
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.
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://authors.library.caltech.edu/40909/
https://authors.library.caltech.edu/40909/1/Engelhardt_2013p287.pdf
https://resolver.caltech.edu/CaltechAUTHORS:20130822-134141566
long_lat ENVELOPE(-145.000,-145.000,-82.250,-82.250)
geographic Kamb Ice Stream
West Antarctica
geographic_facet Kamb Ice Stream
West Antarctica
genre Annals of Glaciology
Antarc*
Antarctica
Kamb Ice Stream
West Antarctica
genre_facet Annals of Glaciology
Antarc*
Antarctica
Kamb Ice Stream
West Antarctica
op_relation https://authors.library.caltech.edu/40909/1/Engelhardt_2013p287.pdf
Engelhardt, Hermann and Kamb, Barclay (2013) Kamb Ice Stream flow history and surge potential. Annals of Glaciology, 54 (63). pp. 287-298. ISSN 0260-3055. doi:10.3189/2013AoG63A535. https://resolver.caltech.edu/CaltechAUTHORS:20130822-134141566 <https://resolver.caltech.edu/CaltechAUTHORS:20130822-134141566>
op_rights other
op_doi https://doi.org/10.3189/2013AoG63A535
container_title Annals of Glaciology
container_volume 54
container_issue 63
container_start_page 287
op_container_end_page 298
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