Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet
Palaeo‐ice sheets are important analogues for understanding contemporary ice sheets, offering a record of ice sheet behaviour that spans millennia. There are two main approaches to reconstructing palaeo‐ice sheets. Empirical reconstructions use the available glacial geological and chronological evid...
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ftleedsuniv:oai:eprints.whiterose.ac.uk:144776 2023-05-15T16:39:38+02:00 Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet Ely, JC Clark, CD Hindmarsh, RCA Hughes, ALC Greenwood, SL Bradley, SL Gasson, E Gregoire, L Gandy, N Stokes, CR Small, D 2021-07 text https://eprints.whiterose.ac.uk/144776/ https://eprints.whiterose.ac.uk/144776/1/Ely-etal-JQS-specialissue-BC-authors_accepted.pdf en eng Wiley https://eprints.whiterose.ac.uk/144776/1/Ely-etal-JQS-specialissue-BC-authors_accepted.pdf Ely, JC, Clark, CD, Hindmarsh, RCA et al. (8 more authors) (2021) Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet. Journal of Quaternary Science, 36 (5). pp. 946-960. ISSN 0267-8179 Article NonPeerReviewed 2021 ftleedsuniv 2023-01-30T22:17:48Z Palaeo‐ice sheets are important analogues for understanding contemporary ice sheets, offering a record of ice sheet behaviour that spans millennia. There are two main approaches to reconstructing palaeo‐ice sheets. Empirical reconstructions use the available glacial geological and chronological evidence to estimate ice sheet extent and dynamics but lack direct consideration of ice physics. In contrast, numerically modelled simulations implement ice physics, but often lack direct quantitative comparison with empirical evidence. Despite being long identified as a fruitful scientific endeavour, few ice sheet reconstructions attempt to reconcile the empirical and model‐based approaches. To achieve this goal, model‐data comparison procedures are required. Here, we compare three numerically modelled simulations of the former British–Irish Ice Sheet with the following lines of evidence: (a) position and shape of former margin positions, recorded by moraines; (b) former ice‐flow direction and flow‐switching, recorded by flowsets of subglacial bedforms; and (c) the timing of ice‐free conditions, recorded by geochronological data. These model–data comparisons provide a useful framework for quantifying the degree of fit between numerical model simulations and empirical constraints. Such tools are vital for reconciling numerical modelling and empirical evidence, the combination of which will lead to more robust palaeo‐ice sheet reconstructions with greater explicative and ultimately predictive power. Article in Journal/Newspaper Ice Sheet White Rose Research Online (Universities of Leeds, Sheffield & York) Endeavour ENVELOPE(162.000,162.000,-76.550,-76.550) |
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White Rose Research Online (Universities of Leeds, Sheffield & York) |
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ftleedsuniv |
language |
English |
description |
Palaeo‐ice sheets are important analogues for understanding contemporary ice sheets, offering a record of ice sheet behaviour that spans millennia. There are two main approaches to reconstructing palaeo‐ice sheets. Empirical reconstructions use the available glacial geological and chronological evidence to estimate ice sheet extent and dynamics but lack direct consideration of ice physics. In contrast, numerically modelled simulations implement ice physics, but often lack direct quantitative comparison with empirical evidence. Despite being long identified as a fruitful scientific endeavour, few ice sheet reconstructions attempt to reconcile the empirical and model‐based approaches. To achieve this goal, model‐data comparison procedures are required. Here, we compare three numerically modelled simulations of the former British–Irish Ice Sheet with the following lines of evidence: (a) position and shape of former margin positions, recorded by moraines; (b) former ice‐flow direction and flow‐switching, recorded by flowsets of subglacial bedforms; and (c) the timing of ice‐free conditions, recorded by geochronological data. These model–data comparisons provide a useful framework for quantifying the degree of fit between numerical model simulations and empirical constraints. Such tools are vital for reconciling numerical modelling and empirical evidence, the combination of which will lead to more robust palaeo‐ice sheet reconstructions with greater explicative and ultimately predictive power. |
format |
Article in Journal/Newspaper |
author |
Ely, JC Clark, CD Hindmarsh, RCA Hughes, ALC Greenwood, SL Bradley, SL Gasson, E Gregoire, L Gandy, N Stokes, CR Small, D |
spellingShingle |
Ely, JC Clark, CD Hindmarsh, RCA Hughes, ALC Greenwood, SL Bradley, SL Gasson, E Gregoire, L Gandy, N Stokes, CR Small, D Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet |
author_facet |
Ely, JC Clark, CD Hindmarsh, RCA Hughes, ALC Greenwood, SL Bradley, SL Gasson, E Gregoire, L Gandy, N Stokes, CR Small, D |
author_sort |
Ely, JC |
title |
Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet |
title_short |
Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet |
title_full |
Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet |
title_fullStr |
Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet |
title_full_unstemmed |
Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet |
title_sort |
recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last british–irish ice sheet |
publisher |
Wiley |
publishDate |
2021 |
url |
https://eprints.whiterose.ac.uk/144776/ https://eprints.whiterose.ac.uk/144776/1/Ely-etal-JQS-specialissue-BC-authors_accepted.pdf |
long_lat |
ENVELOPE(162.000,162.000,-76.550,-76.550) |
geographic |
Endeavour |
geographic_facet |
Endeavour |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
https://eprints.whiterose.ac.uk/144776/1/Ely-etal-JQS-specialissue-BC-authors_accepted.pdf Ely, JC, Clark, CD, Hindmarsh, RCA et al. (8 more authors) (2021) Recent progress on combining geomorphological and geochronological data with ice sheet modelling, demonstrated using the last British–Irish Ice Sheet. Journal of Quaternary Science, 36 (5). pp. 946-960. ISSN 0267-8179 |
_version_ |
1766029963294670848 |