The configuration of Northern Hemisphere ice sheets through the Quaternary

Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-level change is currently limited by a lack of knowledge of the configuration of ice sheets prior to the Last Glacial Maximum (LGM). Here, we compile a synthesis of empirical data and numerical modell...

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Published in:Nature Communications
Main Authors: Batchelor, Christine L, Margold, Martin, Krapp, Mario, Murton, Della K, Dalton, April S, Gibbard, Philip L, Stokes, Chris R, Murton, Julian B, Manica, Andrea
Format: Article in Journal/Newspaper
Language:English
Published: Nature Publishing Group 2019
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Online Access:http://sro.sussex.ac.uk/id/eprint/85241/
http://sro.sussex.ac.uk/id/eprint/85241/11/s41467-019-11601-2.pdf
https://doi.org/10.1038/s41467-019-11601-2
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spelling ftunivsussex:oai:sro.sussex.ac.uk:85241 2023-07-30T04:04:11+02:00 The configuration of Northern Hemisphere ice sheets through the Quaternary Batchelor, Christine L Margold, Martin Krapp, Mario Murton, Della K Dalton, April S Gibbard, Philip L Stokes, Chris R Murton, Julian B Manica, Andrea 2019-08-16 application/pdf http://sro.sussex.ac.uk/id/eprint/85241/ http://sro.sussex.ac.uk/id/eprint/85241/11/s41467-019-11601-2.pdf https://doi.org/10.1038/s41467-019-11601-2 en eng Nature Publishing Group http://sro.sussex.ac.uk/id/eprint/85241/11/s41467-019-11601-2.pdf Batchelor, Christine L, Margold, Martin, Krapp, Mario, Murton, Della K, Dalton, April S, Gibbard, Philip L, Stokes, Chris R, Murton, Julian B and Manica, Andrea (2019) The configuration of Northern Hemisphere ice sheets through the Quaternary. Nature Communications, 10 (1). a3713. ISSN 2041-1723 cc_by_4 Article PeerReviewed 2019 ftunivsussex https://doi.org/10.1038/s41467-019-11601-2 2023-07-11T20:41:16Z Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-level change is currently limited by a lack of knowledge of the configuration of ice sheets prior to the Last Glacial Maximum (LGM). Here, we compile a synthesis of empirical data and numerical modelling results related to pre-LGM ice sheets to produce new hypotheses regarding their extent in the Northern Hemisphere (NH) at 17 time-slices that span the Quaternary. Our reconstructions illustrate pronounced ice-sheet asymmetry within the last glacial cycle and significant variations in ice-marginal positions between older 26 glacial cycles. We find support for a significant reduction in the extent of the Laurentide Ice Sheet (LIS) during MIS 3, implying that global sea levels may have been 30–40 m higher than most previous estimates. Our ice-sheet reconstructions illustrate the current state-of-the-art knowledge of pre-LGM ice sheets and provide a conceptual framework to interpret NH 30 landscape evolution. Article in Journal/Newspaper Ice Sheet University of Sussex: Sussex Research Online Nature Communications 10 1
institution Open Polar
collection University of Sussex: Sussex Research Online
op_collection_id ftunivsussex
language English
description Our understanding of how global climatic changes are translated into ice-sheet fluctuations and sea-level change is currently limited by a lack of knowledge of the configuration of ice sheets prior to the Last Glacial Maximum (LGM). Here, we compile a synthesis of empirical data and numerical modelling results related to pre-LGM ice sheets to produce new hypotheses regarding their extent in the Northern Hemisphere (NH) at 17 time-slices that span the Quaternary. Our reconstructions illustrate pronounced ice-sheet asymmetry within the last glacial cycle and significant variations in ice-marginal positions between older 26 glacial cycles. We find support for a significant reduction in the extent of the Laurentide Ice Sheet (LIS) during MIS 3, implying that global sea levels may have been 30–40 m higher than most previous estimates. Our ice-sheet reconstructions illustrate the current state-of-the-art knowledge of pre-LGM ice sheets and provide a conceptual framework to interpret NH 30 landscape evolution.
format Article in Journal/Newspaper
author Batchelor, Christine L
Margold, Martin
Krapp, Mario
Murton, Della K
Dalton, April S
Gibbard, Philip L
Stokes, Chris R
Murton, Julian B
Manica, Andrea
spellingShingle Batchelor, Christine L
Margold, Martin
Krapp, Mario
Murton, Della K
Dalton, April S
Gibbard, Philip L
Stokes, Chris R
Murton, Julian B
Manica, Andrea
The configuration of Northern Hemisphere ice sheets through the Quaternary
author_facet Batchelor, Christine L
Margold, Martin
Krapp, Mario
Murton, Della K
Dalton, April S
Gibbard, Philip L
Stokes, Chris R
Murton, Julian B
Manica, Andrea
author_sort Batchelor, Christine L
title The configuration of Northern Hemisphere ice sheets through the Quaternary
title_short The configuration of Northern Hemisphere ice sheets through the Quaternary
title_full The configuration of Northern Hemisphere ice sheets through the Quaternary
title_fullStr The configuration of Northern Hemisphere ice sheets through the Quaternary
title_full_unstemmed The configuration of Northern Hemisphere ice sheets through the Quaternary
title_sort configuration of northern hemisphere ice sheets through the quaternary
publisher Nature Publishing Group
publishDate 2019
url http://sro.sussex.ac.uk/id/eprint/85241/
http://sro.sussex.ac.uk/id/eprint/85241/11/s41467-019-11601-2.pdf
https://doi.org/10.1038/s41467-019-11601-2
genre Ice Sheet
genre_facet Ice Sheet
op_relation http://sro.sussex.ac.uk/id/eprint/85241/11/s41467-019-11601-2.pdf
Batchelor, Christine L, Margold, Martin, Krapp, Mario, Murton, Della K, Dalton, April S, Gibbard, Philip L, Stokes, Chris R, Murton, Julian B and Manica, Andrea (2019) The configuration of Northern Hemisphere ice sheets through the Quaternary. Nature Communications, 10 (1). a3713. ISSN 2041-1723
op_rights cc_by_4
op_doi https://doi.org/10.1038/s41467-019-11601-2
container_title Nature Communications
container_volume 10
container_issue 1
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