Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica
The ice-shelf-fringed coast of Dronning Maud Land in East Antarctica contains numerous ice rises that influence the dynamics and mass balance of the region. However, only a few of these ice rises have been investigated in detail. Here, we present field measurements of Blåskimen Island, an isle-type...
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00007797 2023-05-15T13:34:49+02:00 Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica Goel, Vikram Brown, Joel Matsuoka, Kenichi 2017-12 electronic https://doi.org/10.5194/tc-11-2883-2017 https://noa.gwlb.de/receive/cop_mods_00007797 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007754/tc-11-2883-2017.pdf https://tc.copernicus.org/articles/11/2883/2017/tc-11-2883-2017.pdf eng eng Copernicus Publications The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-11-2883-2017 https://noa.gwlb.de/receive/cop_mods_00007797 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007754/tc-11-2883-2017.pdf https://tc.copernicus.org/articles/11/2883/2017/tc-11-2883-2017.pdf uneingeschränkt info:eu-repo/semantics/openAccess article Verlagsveröffentlichung article Text doc-type:article 2017 ftnonlinearchiv https://doi.org/10.5194/tc-11-2883-2017 2022-02-08T22:58:19Z The ice-shelf-fringed coast of Dronning Maud Land in East Antarctica contains numerous ice rises that influence the dynamics and mass balance of the region. However, only a few of these ice rises have been investigated in detail. Here, we present field measurements of Blåskimen Island, an isle-type ice rise adjacent to Fimbul Ice Shelf. This ice rise is largely dome shaped, with a pronounced ridge extending to the south-west from its summit (410 m a.s.l.). Its bed is mostly flat and about 100 m below the current sea level. Shallow radar-detected isochrones dated with a firn core reveal that the surface mass balance is higher on the south-eastern (upwind) slope than on the north-western (downwind) slope by ∼ 37 %, and this pattern has persisted for at least the past decade. Moreover, arches in radar stratigraphy suggest that the summit of the ice rise has been stable for ∼ 600 years. Ensemble estimates of the mass balance using the input–output method show that this ice rise has thickened by 0.12–0.37 m ice equivalent per year over the past decade. Article in Journal/Newspaper Antarc* Antarctica Blåskimen Island Dronning Maud Land East Antarctica Fimbul Ice Shelf Ice Shelf The Cryosphere Niedersächsisches Online-Archiv NOA Blåskimen ENVELOPE(-3.000,-3.000,-70.500,-70.500) Dronning Maud Land East Antarctica Fimbul Ice Shelf ENVELOPE(-0.500,-0.500,-70.750,-70.750) The Cryosphere 11 6 2883 2896 |
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Open Polar |
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Niedersächsisches Online-Archiv NOA |
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ftnonlinearchiv |
language |
English |
topic |
article Verlagsveröffentlichung |
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article Verlagsveröffentlichung Goel, Vikram Brown, Joel Matsuoka, Kenichi Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica |
topic_facet |
article Verlagsveröffentlichung |
description |
The ice-shelf-fringed coast of Dronning Maud Land in East Antarctica contains numerous ice rises that influence the dynamics and mass balance of the region. However, only a few of these ice rises have been investigated in detail. Here, we present field measurements of Blåskimen Island, an isle-type ice rise adjacent to Fimbul Ice Shelf. This ice rise is largely dome shaped, with a pronounced ridge extending to the south-west from its summit (410 m a.s.l.). Its bed is mostly flat and about 100 m below the current sea level. Shallow radar-detected isochrones dated with a firn core reveal that the surface mass balance is higher on the south-eastern (upwind) slope than on the north-western (downwind) slope by ∼ 37 %, and this pattern has persisted for at least the past decade. Moreover, arches in radar stratigraphy suggest that the summit of the ice rise has been stable for ∼ 600 years. Ensemble estimates of the mass balance using the input–output method show that this ice rise has thickened by 0.12–0.37 m ice equivalent per year over the past decade. |
format |
Article in Journal/Newspaper |
author |
Goel, Vikram Brown, Joel Matsuoka, Kenichi |
author_facet |
Goel, Vikram Brown, Joel Matsuoka, Kenichi |
author_sort |
Goel, Vikram |
title |
Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica |
title_short |
Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica |
title_full |
Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica |
title_fullStr |
Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica |
title_full_unstemmed |
Glaciological settings and recent mass balance of Blåskimen Island in Dronning Maud Land, Antarctica |
title_sort |
glaciological settings and recent mass balance of blåskimen island in dronning maud land, antarctica |
publisher |
Copernicus Publications |
publishDate |
2017 |
url |
https://doi.org/10.5194/tc-11-2883-2017 https://noa.gwlb.de/receive/cop_mods_00007797 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007754/tc-11-2883-2017.pdf https://tc.copernicus.org/articles/11/2883/2017/tc-11-2883-2017.pdf |
long_lat |
ENVELOPE(-3.000,-3.000,-70.500,-70.500) ENVELOPE(-0.500,-0.500,-70.750,-70.750) |
geographic |
Blåskimen Dronning Maud Land East Antarctica Fimbul Ice Shelf |
geographic_facet |
Blåskimen Dronning Maud Land East Antarctica Fimbul Ice Shelf |
genre |
Antarc* Antarctica Blåskimen Island Dronning Maud Land East Antarctica Fimbul Ice Shelf Ice Shelf The Cryosphere |
genre_facet |
Antarc* Antarctica Blåskimen Island Dronning Maud Land East Antarctica Fimbul Ice Shelf Ice Shelf The Cryosphere |
op_relation |
The Cryosphere -- ˜Theœ Cryosphere -- http://www.bibliothek.uni-regensburg.de/ezeit/?2393169 -- http://www.the-cryosphere.net/ -- 1994-0424 https://doi.org/10.5194/tc-11-2883-2017 https://noa.gwlb.de/receive/cop_mods_00007797 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00007754/tc-11-2883-2017.pdf https://tc.copernicus.org/articles/11/2883/2017/tc-11-2883-2017.pdf |
op_rights |
uneingeschränkt info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/tc-11-2883-2017 |
container_title |
The Cryosphere |
container_volume |
11 |
container_issue |
6 |
container_start_page |
2883 |
op_container_end_page |
2896 |
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1766058066751520768 |