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

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 10,0...

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Main Authors: Kaboth-Bahr, Stefanie, Bahr, André, Zeeden, Christian, Yamoah, Kweku A., Lone, Mahjoor Ahmad, Chuang, Chih-Kai, Löwemark, Ludvig, Wei, Kuo-Yen
Format: Text
Language:English
Published: Universität Potsdam 2021
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Online Access:https://dx.doi.org/10.25932/publishup-51573
https://publishup.uni-potsdam.de/51573
id ftdatacite:10.25932/publishup-51573
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spelling ftdatacite:10.25932/publishup-51573 2023-05-15T15:06:05+02:00 A tale of shifting relations : East Asian summer and winter monsoon variability during the Holocene Kaboth-Bahr, Stefanie Bahr, André Zeeden, Christian Yamoah, Kweku A. Lone, Mahjoor Ahmad Chuang, Chih-Kai Löwemark, Ludvig Wei, Kuo-Yen 2021 application/pdf https://dx.doi.org/10.25932/publishup-51573 https://publishup.uni-potsdam.de/51573 en eng Universität Potsdam Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY 500 Naturwissenschaften und Mathematik 600 Technik, Technologie article-journal Text ScholarlyArticle 2021 ftdatacite https://doi.org/10.25932/publishup-51573 2021-11-05T12:55:41Z 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. : Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe; 1145 Text Arctic Global warming Sea ice DataCite Metadata Store (German National Library of Science and Technology) Arctic
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic 500 Naturwissenschaften und Mathematik
600 Technik, Technologie
spellingShingle 500 Naturwissenschaften und Mathematik
600 Technik, Technologie
Kaboth-Bahr, Stefanie
Bahr, André
Zeeden, Christian
Yamoah, Kweku A.
Lone, Mahjoor Ahmad
Chuang, Chih-Kai
Löwemark, Ludvig
Wei, Kuo-Yen
A tale of shifting relations : East Asian summer and winter monsoon variability during the Holocene
topic_facet 500 Naturwissenschaften und Mathematik
600 Technik, Technologie
description 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. : Postprints der Universität Potsdam : Mathematisch-Naturwissenschaftliche Reihe; 1145
format Text
author Kaboth-Bahr, Stefanie
Bahr, André
Zeeden, Christian
Yamoah, Kweku A.
Lone, Mahjoor Ahmad
Chuang, Chih-Kai
Löwemark, Ludvig
Wei, Kuo-Yen
author_facet Kaboth-Bahr, Stefanie
Bahr, André
Zeeden, Christian
Yamoah, Kweku A.
Lone, Mahjoor Ahmad
Chuang, Chih-Kai
Löwemark, Ludvig
Wei, Kuo-Yen
author_sort Kaboth-Bahr, Stefanie
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 Universität Potsdam
publishDate 2021
url https://dx.doi.org/10.25932/publishup-51573
https://publishup.uni-potsdam.de/51573
geographic Arctic
geographic_facet Arctic
genre Arctic
Global warming
Sea ice
genre_facet Arctic
Global warming
Sea ice
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.25932/publishup-51573
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