A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene

Abstract Understanding the dynamics between the East Asian summer (EASM) and winter monsoon (EAWM) is needed to predict their variability under future global warming scenarios. Here, we investigate the relationship between EASM and EAWM as well as the mechanisms driving their variability during the...

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Main Authors: Stefanie Kaboth-Bahr, André Bahr, Christian Zeeden, Kweku A. Yamoah, Mahjoor Ahmad Lone, Chih-Kai Chuang, Ludvig Löwemark, Kuo-Yen Wei
Format: Article
Language:English
Published: Nature Publishing Group 2021-03-01
Series:Scientific Reports
Online Access:https://doi.org/10.1038/s41598-021-85444-7
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spelling doaj-f27591eb46344ef3b844e6c7419085982021-03-28T11:30:58ZengNature Publishing GroupScientific Reports2045-23222021-03-0111111010.1038/s41598-021-85444-7A tale of shifting relations: East Asian summer and winter monsoon variability during the HoloceneStefanie Kaboth-Bahr0André Bahr1Christian Zeeden2Kweku A. Yamoah3Mahjoor Ahmad Lone4Chih-Kai Chuang5Ludvig Löwemark6Kuo-Yen Wei7Institute of Geosciences, University of PotsdamInstitute of Earth Sciences, Heidelberg UniversityLIAG, Leibniz Institute for Applied GeophysicsSchool of Geography, Earth and Environmental Sciences, University of BirminghamHigh-Precision Mass Spectrometry and Environment Change Laboratory, Department of Geosciences, National Taiwan UniversityDepartment of Geosciences, National Taiwan UniversityDepartment of Geosciences, National Taiwan UniversityDepartment of Geosciences, National Taiwan UniversityAbstract Understanding the dynamics between the East Asian summer (EASM) and winter monsoon (EAWM) is needed to predict their variability under future global warming scenarios. Here, we investigate the relationship between EASM and EAWM as well as the mechanisms driving their variability during the last 10,000 years by stacking marine and terrestrial (non-speleothem) proxy records from the East Asian realm. This provides a regional and proxy independent signal for both monsoonal systems. The respective signal was subsequently analysed using a linear regression model. We find that the phase relationship between EASM and EAWM is not time-constant and significantly depends on orbital configuration changes. In addition, changes in the Atlantic Meridional Overturning circulation, Arctic sea-ice coverage, El Niño-Southern Oscillation and Sun Spot numbers contributed to millennial scale changes in the EASM and EAWM during the Holocene. We also argue that the bulk signal of monsoonal activity captured by the stacked non-speleothem proxy records supports the previously argued bias of speleothem climatic archives to moisture source changes and/or seasonality.https://doi.org/10.1038/s41598-021-85444-7
collection DOAJ
language English
format Article
sources DOAJ
author Stefanie Kaboth-Bahr
André Bahr
Christian Zeeden
Kweku A. Yamoah
Mahjoor Ahmad Lone
Chih-Kai Chuang
Ludvig Löwemark
Kuo-Yen Wei
spellingShingle Stefanie Kaboth-Bahr
André Bahr
Christian Zeeden
Kweku A. Yamoah
Mahjoor Ahmad Lone
Chih-Kai Chuang
Ludvig Löwemark
Kuo-Yen Wei
A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene
Scientific Reports
author_facet Stefanie Kaboth-Bahr
André Bahr
Christian Zeeden
Kweku A. Yamoah
Mahjoor Ahmad Lone
Chih-Kai Chuang
Ludvig Löwemark
Kuo-Yen Wei
author_sort Stefanie Kaboth-Bahr
title A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene
title_short A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene
title_full A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene
title_fullStr A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene
title_full_unstemmed A tale of shifting relations: East Asian summer and winter monsoon variability during the Holocene
title_sort tale of shifting relations: east asian summer and winter monsoon variability during the holocene
publisher Nature Publishing Group
series Scientific Reports
issn 2045-2322
publishDate 2021-03-01
description Abstract Understanding the dynamics between the East Asian summer (EASM) and winter monsoon (EAWM) is needed to predict their variability under future global warming scenarios. Here, we investigate the relationship between EASM and EAWM as well as the mechanisms driving their variability during the last 10,000 years by stacking marine and terrestrial (non-speleothem) proxy records from the East Asian realm. This provides a regional and proxy independent signal for both monsoonal systems. The respective signal was subsequently analysed using a linear regression model. We find that the phase relationship between EASM and EAWM is not time-constant and significantly depends on orbital configuration changes. In addition, changes in the Atlantic Meridional Overturning circulation, Arctic sea-ice coverage, El Niño-Southern Oscillation and Sun Spot numbers contributed to millennial scale changes in the EASM and EAWM during the Holocene. We also argue that the bulk signal of monsoonal activity captured by the stacked non-speleothem proxy records supports the previously argued bias of speleothem climatic archives to moisture source changes and/or seasonality.
url https://doi.org/10.1038/s41598-021-85444-7
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