The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica
We examine the change in terminus positions of glaciers flowing into the western Ross Sea, Antarctica, between 71°S and 78°S as a proxy for changes in snowfall and/or summer air temperature. This coastline's major glaciers terminate in ice tongues, which are particularly sensitive to changes in...
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ftportlandstate:oai:pdxscholar.library.pdx.edu:geology_fac-1127 2023-11-12T04:08:13+01:00 The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica Fountain, Andrew G. Glenn, Bryce Scambos, Ted A. 2017-01-01T08:00:00Z https://pdxscholar.library.pdx.edu/geology_fac/126 https://doi.org/10.1130/G39240.1 unknown PDXScholar https://pdxscholar.library.pdx.edu/geology_fac/126 doi:10.1130/G39240.1 Geology Faculty Publications and Presentations Geology text 2017 ftportlandstate https://doi.org/10.1130/G39240.1 2023-10-26T18:11:13Z We examine the change in terminus positions of glaciers flowing into the western Ross Sea, Antarctica, between 71°S and 78°S as a proxy for changes in snowfall and/or summer air temperature. This coastline's major glaciers terminate in ice tongues, which are particularly sensitive to changes in flow rate and calving. Using historic maps and satellite imagery spanning 60 yr (A.D. 1955-2015), the terminus positions, ice speed, calving rates, and ice front advance and retreat rates for 34 glaciers are documented. Additionally, changes in regional ice flow speed from 2008 to 2014 are examined. No significant spatial or temporal patterns of terminus position, flow speed, or calving emerged, implying that the conditions associated with ice tongue stability are unchanged. A weak trend of advance may be present in the northernmost part of the coast, consistent with estimates of increased snow accumulation and glacier mass balance in that region. The stability of these glaciers over the past half century contrasts sharply with the rapidly shrinking glaciers of the Antarctic Peninsula and suggests that no significant climate change, as manifest in glacier change, has reached this region of Antarctica. The changing extent of the glaciers along the western Ross Sea, Antarctica. Text Antarc* Antarctic Antarctic Peninsula Antarctica Ross Sea Portland State University: PDXScholar Antarctic Antarctic Peninsula Ross Sea The Antarctic Geology 45 10 927 930 |
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Portland State University: PDXScholar |
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Geology |
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Geology Fountain, Andrew G. Glenn, Bryce Scambos, Ted A. The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica |
topic_facet |
Geology |
description |
We examine the change in terminus positions of glaciers flowing into the western Ross Sea, Antarctica, between 71°S and 78°S as a proxy for changes in snowfall and/or summer air temperature. This coastline's major glaciers terminate in ice tongues, which are particularly sensitive to changes in flow rate and calving. Using historic maps and satellite imagery spanning 60 yr (A.D. 1955-2015), the terminus positions, ice speed, calving rates, and ice front advance and retreat rates for 34 glaciers are documented. Additionally, changes in regional ice flow speed from 2008 to 2014 are examined. No significant spatial or temporal patterns of terminus position, flow speed, or calving emerged, implying that the conditions associated with ice tongue stability are unchanged. A weak trend of advance may be present in the northernmost part of the coast, consistent with estimates of increased snow accumulation and glacier mass balance in that region. The stability of these glaciers over the past half century contrasts sharply with the rapidly shrinking glaciers of the Antarctic Peninsula and suggests that no significant climate change, as manifest in glacier change, has reached this region of Antarctica. The changing extent of the glaciers along the western Ross Sea, Antarctica. |
format |
Text |
author |
Fountain, Andrew G. Glenn, Bryce Scambos, Ted A. |
author_facet |
Fountain, Andrew G. Glenn, Bryce Scambos, Ted A. |
author_sort |
Fountain, Andrew G. |
title |
The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica |
title_short |
The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica |
title_full |
The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica |
title_fullStr |
The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica |
title_full_unstemmed |
The Changing Extent of the Glaciers Along the Western Ross Sea, Antarctica |
title_sort |
changing extent of the glaciers along the western ross sea, antarctica |
publisher |
PDXScholar |
publishDate |
2017 |
url |
https://pdxscholar.library.pdx.edu/geology_fac/126 https://doi.org/10.1130/G39240.1 |
geographic |
Antarctic Antarctic Peninsula Ross Sea The Antarctic |
geographic_facet |
Antarctic Antarctic Peninsula Ross Sea The Antarctic |
genre |
Antarc* Antarctic Antarctic Peninsula Antarctica Ross Sea |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Antarctica Ross Sea |
op_source |
Geology Faculty Publications and Presentations |
op_relation |
https://pdxscholar.library.pdx.edu/geology_fac/126 doi:10.1130/G39240.1 |
op_doi |
https://doi.org/10.1130/G39240.1 |
container_title |
Geology |
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45 |
container_issue |
10 |
container_start_page |
927 |
op_container_end_page |
930 |
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1782328570634305536 |