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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ftleibnizopen:oai:oai.leibnizopen.de:IiePVYsBBwLIz6xGigZZ 2023-11-12T04:12:21+01:00 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://oa.tib.eu/renate/handle/123456789/11791 https://doi.org/10.34657/10824 eng eng [London] : Macmillan Publishers Limited, part of Springer Nature CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0 Scientific reports 11 (2021) Arctic El Nino Holocene information center linear regression analysis 500 600 550 article Text 2021 ftleibnizopen https://doi.org/10.34657/10824 2023-10-22T23:18:39Z 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. publishedVersion Article in Journal/Newspaper Arctic Global warming Sea ice Unknown Arctic |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
ftleibnizopen |
language |
English |
topic |
Arctic El Nino Holocene information center linear regression analysis 500 600 550 |
spellingShingle |
Arctic El Nino Holocene information center linear regression analysis 500 600 550 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 |
Arctic El Nino Holocene information center linear regression analysis 500 600 550 |
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. publishedVersion |
format |
Article in Journal/Newspaper |
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 |
[London] : Macmillan Publishers Limited, part of Springer Nature |
publishDate |
2021 |
url |
https://oa.tib.eu/renate/handle/123456789/11791 https://doi.org/10.34657/10824 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Global warming Sea ice |
genre_facet |
Arctic Global warming Sea ice |
op_source |
Scientific reports 11 (2021) |
op_rights |
CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0 |
op_doi |
https://doi.org/10.34657/10824 |
_version_ |
1782330938756169728 |