The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet
New high-resolution geophysical data acquired from eastern Storbanken in the central Barents Sea allow reconstruction of the flow of marine-based ice dome during the final stages of ice-sheet decay. Ice-marginal and subglacial landforms show diverging and quasi-radial grounding-line retreat patterns...
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Online Access: | http://hdl.handle.net/10852/100626 https://doi.org/10.1016/j.quascirev.2023.107973 |
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ftoslouniv:oai:www.duo.uio.no:10852/100626 2023-05-15T15:38:26+02:00 The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet ENEngelskEnglishThe Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet Montelli, Aleksandr Solovyeva, M Akhmanov, G Mazzini, Adriano Piatilova, Anna Bakay, E. Dowdeswell, Julian 2023-02-11T12:33:45Z http://hdl.handle.net/10852/100626 https://doi.org/10.1016/j.quascirev.2023.107973 EN eng NFR/288299 NFR/223272 Montelli, Aleksandr Solovyeva, M Akhmanov, G Mazzini, Adriano Piatilova, Anna Bakay, E. Dowdeswell, Julian . The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet. Quaternary Science Reviews. 2023, 303(107973) http://hdl.handle.net/10852/100626 2125223 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Quaternary Science Reviews&rft.volume=303&rft.spage=&rft.date=2023 Quaternary Science Reviews 303 107973 https://doi.org/10.1016/j.quascirev.2023.107973 Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ CC-BY 0277-3791 Journal article Tidsskriftartikkel Peer reviewed PublishedVersion 2023 ftoslouniv https://doi.org/10.1016/j.quascirev.2023.107973 2023-03-08T23:36:44Z New high-resolution geophysical data acquired from eastern Storbanken in the central Barents Sea allow reconstruction of the flow of marine-based ice dome during the final stages of ice-sheet decay. Ice-marginal and subglacial landforms show diverging and quasi-radial grounding-line retreat patterns, implying that an isolated, dynamic, shrinking ice dome was centred at ∼77° N 40° E on eastern Storbanken prior to final marine-based ice-sheet collapse. This geomorphological reconstruction contrasts with previous numerical and observational models that infer a northward-migrating ice dome or crest that extended longitudinally from Svalbard to Franz-Josef Land prior to its eventual demise. Our results provide an important past analogue for late-stage decay of marine ice domes, as well as robust empirical constraints that can be used to calibrate numerical models simulating the behaviour of marine-based ice sheets in a warming environment. Article in Journal/Newspaper Barents Sea Franz Josef Land Ice Sheet Sea ice Storbanken Svalbard Universitet i Oslo: Digitale utgivelser ved UiO (DUO) Barents Sea Franz Josef Land ENVELOPE(55.000,55.000,81.000,81.000) Storbanken ENVELOPE(33.000,33.000,78.000,78.000) Svalbard Quaternary Science Reviews 303 107973 |
institution |
Open Polar |
collection |
Universitet i Oslo: Digitale utgivelser ved UiO (DUO) |
op_collection_id |
ftoslouniv |
language |
English |
description |
New high-resolution geophysical data acquired from eastern Storbanken in the central Barents Sea allow reconstruction of the flow of marine-based ice dome during the final stages of ice-sheet decay. Ice-marginal and subglacial landforms show diverging and quasi-radial grounding-line retreat patterns, implying that an isolated, dynamic, shrinking ice dome was centred at ∼77° N 40° E on eastern Storbanken prior to final marine-based ice-sheet collapse. This geomorphological reconstruction contrasts with previous numerical and observational models that infer a northward-migrating ice dome or crest that extended longitudinally from Svalbard to Franz-Josef Land prior to its eventual demise. Our results provide an important past analogue for late-stage decay of marine ice domes, as well as robust empirical constraints that can be used to calibrate numerical models simulating the behaviour of marine-based ice sheets in a warming environment. |
format |
Article in Journal/Newspaper |
author |
Montelli, Aleksandr Solovyeva, M Akhmanov, G Mazzini, Adriano Piatilova, Anna Bakay, E. Dowdeswell, Julian |
spellingShingle |
Montelli, Aleksandr Solovyeva, M Akhmanov, G Mazzini, Adriano Piatilova, Anna Bakay, E. Dowdeswell, Julian The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet |
author_facet |
Montelli, Aleksandr Solovyeva, M Akhmanov, G Mazzini, Adriano Piatilova, Anna Bakay, E. Dowdeswell, Julian |
author_sort |
Montelli, Aleksandr |
title |
The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet |
title_short |
The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet |
title_full |
The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet |
title_fullStr |
The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet |
title_full_unstemmed |
The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet |
title_sort |
geomorphic record of marine-based ice dome decay: final collapse of the barents sea ice sheet |
publishDate |
2023 |
url |
http://hdl.handle.net/10852/100626 https://doi.org/10.1016/j.quascirev.2023.107973 |
long_lat |
ENVELOPE(55.000,55.000,81.000,81.000) ENVELOPE(33.000,33.000,78.000,78.000) |
geographic |
Barents Sea Franz Josef Land Storbanken Svalbard |
geographic_facet |
Barents Sea Franz Josef Land Storbanken Svalbard |
genre |
Barents Sea Franz Josef Land Ice Sheet Sea ice Storbanken Svalbard |
genre_facet |
Barents Sea Franz Josef Land Ice Sheet Sea ice Storbanken Svalbard |
op_source |
0277-3791 |
op_relation |
NFR/288299 NFR/223272 Montelli, Aleksandr Solovyeva, M Akhmanov, G Mazzini, Adriano Piatilova, Anna Bakay, E. Dowdeswell, Julian . The Geomorphic Record of Marine-Based Ice Dome Decay: Final Collapse of the Barents Sea Ice Sheet. Quaternary Science Reviews. 2023, 303(107973) http://hdl.handle.net/10852/100626 2125223 info:ofi/fmt:kev:mtx:ctx&ctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Quaternary Science Reviews&rft.volume=303&rft.spage=&rft.date=2023 Quaternary Science Reviews 303 107973 https://doi.org/10.1016/j.quascirev.2023.107973 |
op_rights |
Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/ |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1016/j.quascirev.2023.107973 |
container_title |
Quaternary Science Reviews |
container_volume |
303 |
container_start_page |
107973 |
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1766369357469843456 |