Ice streams in the Laurentide Ice Sheet: a new mapping inventory

Rapidly flowing ice streams dominate the drainage of continental ice sheets and are a key component of their mass balance. Due to their potential impact on sea level, their activity in the Antarctic and Greenland Ice Sheets has undergone detailed scrutiny in recent decades. However, these observatio...

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Main Authors: Martin Margold, Chris R. Stokes, Chris D. Clark, Johan Kleman
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://hdl.handle.net/10.1080/17445647.2014.912036
id ftrepec:oai:RePEc:taf:tjomxx:v:11:y:2015:i:3:p:380-395
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spelling ftrepec:oai:RePEc:taf:tjomxx:v:11:y:2015:i:3:p:380-395 2023-05-15T13:31:11+02:00 Ice streams in the Laurentide Ice Sheet: a new mapping inventory Martin Margold Chris R. Stokes Chris D. Clark Johan Kleman http://hdl.handle.net/10.1080/17445647.2014.912036 unknown http://hdl.handle.net/10.1080/17445647.2014.912036 article ftrepec 2020-12-04T13:32:26Z Rapidly flowing ice streams dominate the drainage of continental ice sheets and are a key component of their mass balance. Due to their potential impact on sea level, their activity in the Antarctic and Greenland Ice Sheets has undergone detailed scrutiny in recent decades. However, these observations only cover a fraction of their 'life-span' and the subglacial processes that facilitate their rapid flow are very difficult to observe. To circumvent these problems, numerous workers have highlighted the potential of investigating palaeo-ice streams tracks, preserved in the landform and sedimentary record of former ice sheets. As such, it is becoming increasingly important to know where and when palaeo-ice streams operated. In this paper, we present a new map of ice streams in the North American Laurentide Ice Sheet (LIS; including the Innuitian Ice Sheet), which was the largest of the ephemeral Pleistocene ice sheets and where numerous ice streams have been identified. We compile previously published evidence of ice stream activity and complement it with new mapping to generate the most complete and consistent mapping inventory to date. The map depicts close to three times as many ice streams (117 in total) compared to previous inventories, and categorises them according to the evidence they left behind, with some locations more speculative than others. The map considerably refines our understanding of LIS dynamics, but there is a clear requirement for improved dating of ice stream activity. Article in Journal/Newspaper Antarc* Antarctic Greenland Ice Sheet RePEc (Research Papers in Economics) Antarctic Greenland The Antarctic
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Rapidly flowing ice streams dominate the drainage of continental ice sheets and are a key component of their mass balance. Due to their potential impact on sea level, their activity in the Antarctic and Greenland Ice Sheets has undergone detailed scrutiny in recent decades. However, these observations only cover a fraction of their 'life-span' and the subglacial processes that facilitate their rapid flow are very difficult to observe. To circumvent these problems, numerous workers have highlighted the potential of investigating palaeo-ice streams tracks, preserved in the landform and sedimentary record of former ice sheets. As such, it is becoming increasingly important to know where and when palaeo-ice streams operated. In this paper, we present a new map of ice streams in the North American Laurentide Ice Sheet (LIS; including the Innuitian Ice Sheet), which was the largest of the ephemeral Pleistocene ice sheets and where numerous ice streams have been identified. We compile previously published evidence of ice stream activity and complement it with new mapping to generate the most complete and consistent mapping inventory to date. The map depicts close to three times as many ice streams (117 in total) compared to previous inventories, and categorises them according to the evidence they left behind, with some locations more speculative than others. The map considerably refines our understanding of LIS dynamics, but there is a clear requirement for improved dating of ice stream activity.
format Article in Journal/Newspaper
author Martin Margold
Chris R. Stokes
Chris D. Clark
Johan Kleman
spellingShingle Martin Margold
Chris R. Stokes
Chris D. Clark
Johan Kleman
Ice streams in the Laurentide Ice Sheet: a new mapping inventory
author_facet Martin Margold
Chris R. Stokes
Chris D. Clark
Johan Kleman
author_sort Martin Margold
title Ice streams in the Laurentide Ice Sheet: a new mapping inventory
title_short Ice streams in the Laurentide Ice Sheet: a new mapping inventory
title_full Ice streams in the Laurentide Ice Sheet: a new mapping inventory
title_fullStr Ice streams in the Laurentide Ice Sheet: a new mapping inventory
title_full_unstemmed Ice streams in the Laurentide Ice Sheet: a new mapping inventory
title_sort ice streams in the laurentide ice sheet: a new mapping inventory
url http://hdl.handle.net/10.1080/17445647.2014.912036
geographic Antarctic
Greenland
The Antarctic
geographic_facet Antarctic
Greenland
The Antarctic
genre Antarc*
Antarctic
Greenland
Ice Sheet
genre_facet Antarc*
Antarctic
Greenland
Ice Sheet
op_relation http://hdl.handle.net/10.1080/17445647.2014.912036
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