Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China
Three cores (ZY-1, ZY-2 and ZY-3) retrieved from the Central Yellow Sea mud (CYSM) were analyzed in sensitive grain size and AMS 14C dating to reconstruct the history of the East Asian Winter Monsoon (EAWM) since the Middle Holocene in the study area. The results show that these data provide a conti...
Published in: | Science China Earth Sciences |
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2012
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Online Access: | http://ir.ieecas.cn/handle/361006/10142 https://doi.org/10.1007/s11430-012-4447-7 |
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ftchinacascieeca:oai:ir.ieecas.cn:361006/10142 2023-06-11T04:14:43+02:00 Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China Hu, BQ (Hu ,Bangqi) 1,2,3 Yang, ZS (Yang, Zuosheng) 3 Zhao, MX (Zhao ,Meixun) 4 Saito, Y (Saito, Yoshiki) 5 Fan, DJ (Fan ,Dejiang) 3 Wang, LB (Wang ,Libo) 1 2012-10-30 http://ir.ieecas.cn/handle/361006/10142 https://doi.org/10.1007/s11430-012-4447-7 英语 eng Science China-Earth Sciences http://ir.ieecas.cn/handle/361006/10142 doi:10.1007/s11430-012-4447-7 null 期刊论文 2012 ftchinacascieeca https://doi.org/10.1007/s11430-012-4447-7 2023-05-08T13:23:31Z Three cores (ZY-1, ZY-2 and ZY-3) retrieved from the Central Yellow Sea mud (CYSM) were analyzed in sensitive grain size and AMS 14C dating to reconstruct the history of the East Asian Winter Monsoon (EAWM) since the Middle Holocene in the study area. The results show that these data provide a continuous history of the EAWM over the past 7. 2 ka and that the EAWM can be divided into three periods: strong and highly fluctuating during 7. 2-4. 2 ka BP; moderate and relatively stable during 4. 2-1. 8 ka BP; and weakened during 1. 8-0 ka BP. Compared with the East Asian Summer Monsoon (EASM) recorded in the previous studies, the evolutionary history of the EAWM broadly follows the orbital-derived winter insolation with a similar long-term step-decreased trend as the EASM. At the centennial scale, however, the EAWM intensified events correlate well with the EASM weakened events and the North Atlantic climatic variations (Bond events 0 to 5) within the dating error, most likely forced by the reduction of solar irradiance through changes in the oceanic-atmospheric circulation patterns. Report North Atlantic Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) Science China Earth Sciences 55 10 1656 1668 |
institution |
Open Polar |
collection |
Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchinacascieeca |
language |
English |
description |
Three cores (ZY-1, ZY-2 and ZY-3) retrieved from the Central Yellow Sea mud (CYSM) were analyzed in sensitive grain size and AMS 14C dating to reconstruct the history of the East Asian Winter Monsoon (EAWM) since the Middle Holocene in the study area. The results show that these data provide a continuous history of the EAWM over the past 7. 2 ka and that the EAWM can be divided into three periods: strong and highly fluctuating during 7. 2-4. 2 ka BP; moderate and relatively stable during 4. 2-1. 8 ka BP; and weakened during 1. 8-0 ka BP. Compared with the East Asian Summer Monsoon (EASM) recorded in the previous studies, the evolutionary history of the EAWM broadly follows the orbital-derived winter insolation with a similar long-term step-decreased trend as the EASM. At the centennial scale, however, the EAWM intensified events correlate well with the EASM weakened events and the North Atlantic climatic variations (Bond events 0 to 5) within the dating error, most likely forced by the reduction of solar irradiance through changes in the oceanic-atmospheric circulation patterns. |
format |
Report |
author |
Hu, BQ (Hu ,Bangqi) 1,2,3 Yang, ZS (Yang, Zuosheng) 3 Zhao, MX (Zhao ,Meixun) 4 Saito, Y (Saito, Yoshiki) 5 Fan, DJ (Fan ,Dejiang) 3 Wang, LB (Wang ,Libo) 1 |
spellingShingle |
Hu, BQ (Hu ,Bangqi) 1,2,3 Yang, ZS (Yang, Zuosheng) 3 Zhao, MX (Zhao ,Meixun) 4 Saito, Y (Saito, Yoshiki) 5 Fan, DJ (Fan ,Dejiang) 3 Wang, LB (Wang ,Libo) 1 Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China |
author_facet |
Hu, BQ (Hu ,Bangqi) 1,2,3 Yang, ZS (Yang, Zuosheng) 3 Zhao, MX (Zhao ,Meixun) 4 Saito, Y (Saito, Yoshiki) 5 Fan, DJ (Fan ,Dejiang) 3 Wang, LB (Wang ,Libo) 1 |
author_sort |
Hu, BQ (Hu ,Bangqi) 1,2,3 |
title |
Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China |
title_short |
Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China |
title_full |
Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China |
title_fullStr |
Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China |
title_full_unstemmed |
Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China |
title_sort |
grain size records reveal variability of the east asian winter monsoon since the middle holocene in the central yellow sea mud area, china |
publishDate |
2012 |
url |
http://ir.ieecas.cn/handle/361006/10142 https://doi.org/10.1007/s11430-012-4447-7 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Science China-Earth Sciences http://ir.ieecas.cn/handle/361006/10142 doi:10.1007/s11430-012-4447-7 |
op_rights |
null |
op_doi |
https://doi.org/10.1007/s11430-012-4447-7 |
container_title |
Science China Earth Sciences |
container_volume |
55 |
container_issue |
10 |
container_start_page |
1656 |
op_container_end_page |
1668 |
_version_ |
1768370969340018688 |