Obliquity-paced climate change recorded in Antarctic debris-covered glaciers

The degree to which debris-covered glaciers record past environmental conditions is debated. Here, the authors show that obliquity-paced variations in solar radiation over the past ∼220 ka are expressed in Mullins glacier as repetitive changes in englacial debris and corresponding surface topography...

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Published in:Nature Communications
Main Authors: Sean L. Mackay, David R. Marchant
Format: Article in Journal/Newspaper
Language:English
Published: Nature Portfolio 2017
Subjects:
Q
Online Access:https://doi.org/10.1038/ncomms14194
https://doaj.org/article/03006305c14c4e698913a0bca292e313
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spelling ftdoajarticles:oai:doaj.org/article:03006305c14c4e698913a0bca292e313 2023-05-15T13:52:24+02:00 Obliquity-paced climate change recorded in Antarctic debris-covered glaciers Sean L. Mackay David R. Marchant 2017-02-01T00:00:00Z https://doi.org/10.1038/ncomms14194 https://doaj.org/article/03006305c14c4e698913a0bca292e313 EN eng Nature Portfolio https://doi.org/10.1038/ncomms14194 https://doaj.org/toc/2041-1723 doi:10.1038/ncomms14194 2041-1723 https://doaj.org/article/03006305c14c4e698913a0bca292e313 Nature Communications, Vol 8, Iss 1, Pp 1-12 (2017) Science Q article 2017 ftdoajarticles https://doi.org/10.1038/ncomms14194 2022-12-31T07:08:10Z The degree to which debris-covered glaciers record past environmental conditions is debated. Here, the authors show that obliquity-paced variations in solar radiation over the past ∼220 ka are expressed in Mullins glacier as repetitive changes in englacial debris and corresponding surface topography. Article in Journal/Newspaper Antarc* Antarctic Directory of Open Access Journals: DOAJ Articles Antarctic Nature Communications 8 1
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Science
Q
spellingShingle Science
Q
Sean L. Mackay
David R. Marchant
Obliquity-paced climate change recorded in Antarctic debris-covered glaciers
topic_facet Science
Q
description The degree to which debris-covered glaciers record past environmental conditions is debated. Here, the authors show that obliquity-paced variations in solar radiation over the past ∼220 ka are expressed in Mullins glacier as repetitive changes in englacial debris and corresponding surface topography.
format Article in Journal/Newspaper
author Sean L. Mackay
David R. Marchant
author_facet Sean L. Mackay
David R. Marchant
author_sort Sean L. Mackay
title Obliquity-paced climate change recorded in Antarctic debris-covered glaciers
title_short Obliquity-paced climate change recorded in Antarctic debris-covered glaciers
title_full Obliquity-paced climate change recorded in Antarctic debris-covered glaciers
title_fullStr Obliquity-paced climate change recorded in Antarctic debris-covered glaciers
title_full_unstemmed Obliquity-paced climate change recorded in Antarctic debris-covered glaciers
title_sort obliquity-paced climate change recorded in antarctic debris-covered glaciers
publisher Nature Portfolio
publishDate 2017
url https://doi.org/10.1038/ncomms14194
https://doaj.org/article/03006305c14c4e698913a0bca292e313
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_source Nature Communications, Vol 8, Iss 1, Pp 1-12 (2017)
op_relation https://doi.org/10.1038/ncomms14194
https://doaj.org/toc/2041-1723
doi:10.1038/ncomms14194
2041-1723
https://doaj.org/article/03006305c14c4e698913a0bca292e313
op_doi https://doi.org/10.1038/ncomms14194
container_title Nature Communications
container_volume 8
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