Longitudinal surface structures (flowstripes) on Antarctic glaciers
Longitudinal surface structures (“flowstripes”) are common on many glaciers but their origin and significance are poorly understood. In this paper we present observations of the development of these longitudinal structures from four different Antarctic glacier systems; the Lambert Glacier/Amery Ice...
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2012
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ftnerc:oai:nora.nerc.ac.uk:18617 2023-05-15T13:22:09+02:00 Longitudinal surface structures (flowstripes) on Antarctic glaciers Glasser, N. F. Gudmundsson, G. H. 2012 text http://nora.nerc.ac.uk/id/eprint/18617/ https://nora.nerc.ac.uk/id/eprint/18617/1/tc-6-383-2012.pdf en eng Copernicus Publications https://nora.nerc.ac.uk/id/eprint/18617/1/tc-6-383-2012.pdf Glasser, N. F.; Gudmundsson, G. H. orcid:0000-0003-4236-5369 . 2012 Longitudinal surface structures (flowstripes) on Antarctic glaciers. The Cryosphere, 6 (2). 383-391. https://doi.org/10.5194/tc-6-383-2012 <https://doi.org/10.5194/tc-6-383-2012> Publication - Article PeerReviewed 2012 ftnerc https://doi.org/10.5194/tc-6-383-2012 2023-02-04T19:31:51Z Longitudinal surface structures (“flowstripes”) are common on many glaciers but their origin and significance are poorly understood. In this paper we present observations of the development of these longitudinal structures from four different Antarctic glacier systems; the Lambert Glacier/Amery Ice Shelf area, the Taylor and Ferrar Glaciers in the Ross Sea sector, Crane and Jorum Glaciers (ice-shelf tributary glaciers) on the Antarctic Peninsula, and the onset zone of a tributary to the Recovery Glacier Ice Stream in the Filchner Ice Shelf area. Mapping from optical satellite images demonstrates that longitudinal surface structures develop in two main situations: (1) as relatively wide flow stripes within glacier flow units and (2) as relatively narrow flow stripes where there is convergent flow around nunataks or at glacier confluence zones. Our observations indicate that the confluence features are narrower, sharper, and more clearly defined features. They are characterised by linear troughs or depressions on the ice surface and are much more common than the former type. Longitudinal surface structures within glacier flow units have previously been explained as the surface expression of localised bed perturbations but a universal explanation for those forming at glacier confluences is lacking. Here we propose that these features are formed at zones of ice acceleration and extensional flow at glacier confluences. We provide a schematic model for the development of longitudinal surface structures based on extensional flow that can explain their ridge and trough morphology as well as their down-ice persistence. Article in Journal/Newspaper Amery Ice Shelf Antarc* Antarctic Antarctic Peninsula Ice Shelf Lambert Glacier Recovery Glacier Ross Sea The Cryosphere Natural Environment Research Council: NERC Open Research Archive Antarctic The Antarctic Antarctic Peninsula Ross Sea Amery ENVELOPE(-94.063,-94.063,56.565,56.565) Amery Ice Shelf ENVELOPE(71.000,71.000,-69.750,-69.750) Lambert Glacier ENVELOPE(67.490,67.490,-73.065,-73.065) Filchner Ice Shelf ENVELOPE(-40.000,-40.000,-79.000,-79.000) Recovery Glacier ENVELOPE(-25.500,-25.500,-81.166,-81.166) The Cryosphere 6 2 383 391 |
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Open Polar |
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Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
English |
description |
Longitudinal surface structures (“flowstripes”) are common on many glaciers but their origin and significance are poorly understood. In this paper we present observations of the development of these longitudinal structures from four different Antarctic glacier systems; the Lambert Glacier/Amery Ice Shelf area, the Taylor and Ferrar Glaciers in the Ross Sea sector, Crane and Jorum Glaciers (ice-shelf tributary glaciers) on the Antarctic Peninsula, and the onset zone of a tributary to the Recovery Glacier Ice Stream in the Filchner Ice Shelf area. Mapping from optical satellite images demonstrates that longitudinal surface structures develop in two main situations: (1) as relatively wide flow stripes within glacier flow units and (2) as relatively narrow flow stripes where there is convergent flow around nunataks or at glacier confluence zones. Our observations indicate that the confluence features are narrower, sharper, and more clearly defined features. They are characterised by linear troughs or depressions on the ice surface and are much more common than the former type. Longitudinal surface structures within glacier flow units have previously been explained as the surface expression of localised bed perturbations but a universal explanation for those forming at glacier confluences is lacking. Here we propose that these features are formed at zones of ice acceleration and extensional flow at glacier confluences. We provide a schematic model for the development of longitudinal surface structures based on extensional flow that can explain their ridge and trough morphology as well as their down-ice persistence. |
format |
Article in Journal/Newspaper |
author |
Glasser, N. F. Gudmundsson, G. H. |
spellingShingle |
Glasser, N. F. Gudmundsson, G. H. Longitudinal surface structures (flowstripes) on Antarctic glaciers |
author_facet |
Glasser, N. F. Gudmundsson, G. H. |
author_sort |
Glasser, N. F. |
title |
Longitudinal surface structures (flowstripes) on Antarctic glaciers |
title_short |
Longitudinal surface structures (flowstripes) on Antarctic glaciers |
title_full |
Longitudinal surface structures (flowstripes) on Antarctic glaciers |
title_fullStr |
Longitudinal surface structures (flowstripes) on Antarctic glaciers |
title_full_unstemmed |
Longitudinal surface structures (flowstripes) on Antarctic glaciers |
title_sort |
longitudinal surface structures (flowstripes) on antarctic glaciers |
publisher |
Copernicus Publications |
publishDate |
2012 |
url |
http://nora.nerc.ac.uk/id/eprint/18617/ https://nora.nerc.ac.uk/id/eprint/18617/1/tc-6-383-2012.pdf |
long_lat |
ENVELOPE(-94.063,-94.063,56.565,56.565) ENVELOPE(71.000,71.000,-69.750,-69.750) ENVELOPE(67.490,67.490,-73.065,-73.065) ENVELOPE(-40.000,-40.000,-79.000,-79.000) ENVELOPE(-25.500,-25.500,-81.166,-81.166) |
geographic |
Antarctic The Antarctic Antarctic Peninsula Ross Sea Amery Amery Ice Shelf Lambert Glacier Filchner Ice Shelf Recovery Glacier |
geographic_facet |
Antarctic The Antarctic Antarctic Peninsula Ross Sea Amery Amery Ice Shelf Lambert Glacier Filchner Ice Shelf Recovery Glacier |
genre |
Amery Ice Shelf Antarc* Antarctic Antarctic Peninsula Ice Shelf Lambert Glacier Recovery Glacier Ross Sea The Cryosphere |
genre_facet |
Amery Ice Shelf Antarc* Antarctic Antarctic Peninsula Ice Shelf Lambert Glacier Recovery Glacier Ross Sea The Cryosphere |
op_relation |
https://nora.nerc.ac.uk/id/eprint/18617/1/tc-6-383-2012.pdf Glasser, N. F.; Gudmundsson, G. H. orcid:0000-0003-4236-5369 . 2012 Longitudinal surface structures (flowstripes) on Antarctic glaciers. The Cryosphere, 6 (2). 383-391. https://doi.org/10.5194/tc-6-383-2012 <https://doi.org/10.5194/tc-6-383-2012> |
op_doi |
https://doi.org/10.5194/tc-6-383-2012 |
container_title |
The Cryosphere |
container_volume |
6 |
container_issue |
2 |
container_start_page |
383 |
op_container_end_page |
391 |
_version_ |
1766363504423469056 |