Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat
Rates of ice stream retreat over decades can be determined from repeated satellite surveys and over millennia by palaeoenvironmental reconstructions. Centennial time scales are an important temporal gap in geological observations of value in process understanding and evaluating numerical models. We...
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Geological Society of America
2017
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ftkeeleuniv:oai:eprints.keele.ac.uk:3430 2023-07-30T04:04:13+02:00 Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat Smedley, R Chiverrell, RC Ballantyne, CK Burke, MJ Clark, CD Duller, GAT Fabel, D McCarroll, D Scourse, JD Small, D Thomas, GSP 2017-05-06 text https://eprints.keele.ac.uk/id/eprint/3430/ https://eprints.keele.ac.uk/id/eprint/3430/7/Smedley%20et%20al._Geology_DATA%20REPOSITORY.pdf http://geology.gsapubs.org/ en eng Geological Society of America https://eprints.keele.ac.uk/id/eprint/3430/7/Smedley%20et%20al._Geology_DATA%20REPOSITORY.pdf Smedley, R, Chiverrell, RC, Ballantyne, CK, Burke, MJ, Clark, CD, Duller, GAT, Fabel, D, McCarroll, D, Scourse, JD, Small, D and Thomas, GSP (2017) Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat. Geology. (In Press) cc_by_nc_4 Article PeerReviewed 2017 ftkeeleuniv 2023-07-10T21:15:50Z Rates of ice stream retreat over decades can be determined from repeated satellite surveys and over millennia by palaeoenvironmental reconstructions. Centennial time scales are an important temporal gap in geological observations of value in process understanding and evaluating numerical models. We address this temporal gap by developing a 3 ka and 123 km retreat time series for the Irish Sea Ice Stream (ISIS), a major outlet draining the last British Irish Ice Sheet. The Llŷn Peninsula (NW Wales, UK) contains numerous ice-marginal indicators from which we reconstruct a robust chronological framework of margin oscillations. The landscape documents the retreat of a former marine-terminating ice stream through a topographic constriction, across a reverse bed-slope and across variations in calving margin width. New dating constraints for this sequence are integrated in a Bayesian sequence model to develop a high-resolution ice retreat chronology. Our results show that retreat of the ISIS during the period 24–20 ka displayed centennial-scale oscillatory behavior of the margin despite relatively stable climatic, oceanic and relative sea level forcings. Faster retreat rates coincided with greater axial trough depths as the ice passed over a reverse bed-slope and the calving margin widened (from 65 to 139 km). The geological observations presented here over a 123 km long ice retreat sequence are consistent with theory that marine-based ice can be inherently unstable when passing over a reverse bed-slope, but also that wider calving margins lead to much faster ice retreat. Article in Journal/Newspaper Ice Sheet Sea ice Keele University: Keele Research Repository |
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Open Polar |
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Keele University: Keele Research Repository |
op_collection_id |
ftkeeleuniv |
language |
English |
description |
Rates of ice stream retreat over decades can be determined from repeated satellite surveys and over millennia by palaeoenvironmental reconstructions. Centennial time scales are an important temporal gap in geological observations of value in process understanding and evaluating numerical models. We address this temporal gap by developing a 3 ka and 123 km retreat time series for the Irish Sea Ice Stream (ISIS), a major outlet draining the last British Irish Ice Sheet. The Llŷn Peninsula (NW Wales, UK) contains numerous ice-marginal indicators from which we reconstruct a robust chronological framework of margin oscillations. The landscape documents the retreat of a former marine-terminating ice stream through a topographic constriction, across a reverse bed-slope and across variations in calving margin width. New dating constraints for this sequence are integrated in a Bayesian sequence model to develop a high-resolution ice retreat chronology. Our results show that retreat of the ISIS during the period 24–20 ka displayed centennial-scale oscillatory behavior of the margin despite relatively stable climatic, oceanic and relative sea level forcings. Faster retreat rates coincided with greater axial trough depths as the ice passed over a reverse bed-slope and the calving margin widened (from 65 to 139 km). The geological observations presented here over a 123 km long ice retreat sequence are consistent with theory that marine-based ice can be inherently unstable when passing over a reverse bed-slope, but also that wider calving margins lead to much faster ice retreat. |
format |
Article in Journal/Newspaper |
author |
Smedley, R Chiverrell, RC Ballantyne, CK Burke, MJ Clark, CD Duller, GAT Fabel, D McCarroll, D Scourse, JD Small, D Thomas, GSP |
spellingShingle |
Smedley, R Chiverrell, RC Ballantyne, CK Burke, MJ Clark, CD Duller, GAT Fabel, D McCarroll, D Scourse, JD Small, D Thomas, GSP Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat |
author_facet |
Smedley, R Chiverrell, RC Ballantyne, CK Burke, MJ Clark, CD Duller, GAT Fabel, D McCarroll, D Scourse, JD Small, D Thomas, GSP |
author_sort |
Smedley, R |
title |
Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat |
title_short |
Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat |
title_full |
Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat |
title_fullStr |
Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat |
title_full_unstemmed |
Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat |
title_sort |
internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat |
publisher |
Geological Society of America |
publishDate |
2017 |
url |
https://eprints.keele.ac.uk/id/eprint/3430/ https://eprints.keele.ac.uk/id/eprint/3430/7/Smedley%20et%20al._Geology_DATA%20REPOSITORY.pdf http://geology.gsapubs.org/ |
genre |
Ice Sheet Sea ice |
genre_facet |
Ice Sheet Sea ice |
op_relation |
https://eprints.keele.ac.uk/id/eprint/3430/7/Smedley%20et%20al._Geology_DATA%20REPOSITORY.pdf Smedley, R, Chiverrell, RC, Ballantyne, CK, Burke, MJ, Clark, CD, Duller, GAT, Fabel, D, McCarroll, D, Scourse, JD, Small, D and Thomas, GSP (2017) Internal dynamics condition centennial-scale oscillations in marine-based ice stream retreat. Geology. (In Press) |
op_rights |
cc_by_nc_4 |
_version_ |
1772815492348641280 |