North African humid periods over the past 800,000 years

The Sahara region has experienced periodic wet periods over the Quaternary and beyond. These North African Humid Periods (NAHPs) are astronomically paced by precession which controls the intensity of the African monsoon system. However, most climate models cannot reconcile the magnitude of these eve...

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Published in:Nature Communications
Main Authors: Armstrong, Edward, Tallavaara, Miikka, Hopcroft, Peter O., Valdes, Paul J.
Format: Text
Language:English
Published: Nature Publishing Group UK 2023
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10491769/
http://www.ncbi.nlm.nih.gov/pubmed/37684244
https://doi.org/10.1038/s41467-023-41219-4
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spelling ftpubmed:oai:pubmedcentral.nih.gov:10491769 2023-10-09T21:52:24+02:00 North African humid periods over the past 800,000 years Armstrong, Edward Tallavaara, Miikka Hopcroft, Peter O. Valdes, Paul J. 2023-09-08 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10491769/ http://www.ncbi.nlm.nih.gov/pubmed/37684244 https://doi.org/10.1038/s41467-023-41219-4 en eng Nature Publishing Group UK http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10491769/ http://www.ncbi.nlm.nih.gov/pubmed/37684244 http://dx.doi.org/10.1038/s41467-023-41219-4 © Springer Nature Limited 2023 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) . Nat Commun Article Text 2023 ftpubmed https://doi.org/10.1038/s41467-023-41219-4 2023-09-17T00:43:17Z The Sahara region has experienced periodic wet periods over the Quaternary and beyond. These North African Humid Periods (NAHPs) are astronomically paced by precession which controls the intensity of the African monsoon system. However, most climate models cannot reconcile the magnitude of these events and so the driving mechanisms remain poorly constrained. Here, we utilise a recently developed version of the HadCM3B coupled climate model that simulates 20 NAHPs over the past 800 kyr which have good agreement with NAHPs identified in proxy data. Our results show that precession determines NAHP pacing, but we identify that their amplitude is strongly linked to eccentricity via its control over ice sheet extent. During glacial periods, enhanced ice-albedo driven cooling suppresses NAHP amplitude at precession minima, when humid conditions would otherwise be expected. This highlights the importance of both precession and eccentricity, and the role of high latitude processes in determining the timing and amplitude of the NAHPs. This may have implications for the out of Africa dispersal of plants and animals throughout the Quaternary. Text Ice Sheet PubMed Central (PMC) Nature Communications 14 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Article
spellingShingle Article
Armstrong, Edward
Tallavaara, Miikka
Hopcroft, Peter O.
Valdes, Paul J.
North African humid periods over the past 800,000 years
topic_facet Article
description The Sahara region has experienced periodic wet periods over the Quaternary and beyond. These North African Humid Periods (NAHPs) are astronomically paced by precession which controls the intensity of the African monsoon system. However, most climate models cannot reconcile the magnitude of these events and so the driving mechanisms remain poorly constrained. Here, we utilise a recently developed version of the HadCM3B coupled climate model that simulates 20 NAHPs over the past 800 kyr which have good agreement with NAHPs identified in proxy data. Our results show that precession determines NAHP pacing, but we identify that their amplitude is strongly linked to eccentricity via its control over ice sheet extent. During glacial periods, enhanced ice-albedo driven cooling suppresses NAHP amplitude at precession minima, when humid conditions would otherwise be expected. This highlights the importance of both precession and eccentricity, and the role of high latitude processes in determining the timing and amplitude of the NAHPs. This may have implications for the out of Africa dispersal of plants and animals throughout the Quaternary.
format Text
author Armstrong, Edward
Tallavaara, Miikka
Hopcroft, Peter O.
Valdes, Paul J.
author_facet Armstrong, Edward
Tallavaara, Miikka
Hopcroft, Peter O.
Valdes, Paul J.
author_sort Armstrong, Edward
title North African humid periods over the past 800,000 years
title_short North African humid periods over the past 800,000 years
title_full North African humid periods over the past 800,000 years
title_fullStr North African humid periods over the past 800,000 years
title_full_unstemmed North African humid periods over the past 800,000 years
title_sort north african humid periods over the past 800,000 years
publisher Nature Publishing Group UK
publishDate 2023
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10491769/
http://www.ncbi.nlm.nih.gov/pubmed/37684244
https://doi.org/10.1038/s41467-023-41219-4
genre Ice Sheet
genre_facet Ice Sheet
op_source Nat Commun
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC10491769/
http://www.ncbi.nlm.nih.gov/pubmed/37684244
http://dx.doi.org/10.1038/s41467-023-41219-4
op_rights © Springer Nature Limited 2023
https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
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