1000-Year Quasi-Periodicity of Weak Monsoon Events in TemperateNortheast Asia since the Mid-Holocene
- Collection with item attached
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2017
- Item details URL
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http://open-repository.kisti.re.kr/cube/handle/open_repository/473398.do
- DOI
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10.1038/s41598-017-15566-4
- Title
- 1000-Year Quasi-Periodicity of Weak Monsoon Events in TemperateNortheast Asia since the Mid-Holocene
- Description
- This research was supported by the Basic Science Research Programthrough the National Research Foundation of Korea (NRF) funded by theMinistry of Science, ICT & Future Planning (No. NRF-2015RIA4A1041105)and (No. NRF-2016R1C1B2016525). In addition, this work was partiallysupported by the Basic Research Project (GP2017-013) of Korea Instituteof Geoscience and Mineral Resources (KIGAM) and by 2015 Research Grantfrom Kangwon National University (KNU).
- abstract
- The Holocene variability in the East Asian summer monsoon (EASM) based on speleothem delta O-18 records has inconsistencies in timing, duration, and expression of millennial-scale events among nearby regions, and even within the same cave. Here, we present another stalagmite delta O-18 record with multi-decadal time resolution from the temperate Korean Peninsula (KP) for the last 5500 years in order to compare with Holocene millennial-scale EASM events from Southeast Asia. Based on our new stalagmite delta O-18 record, millennial-scale events since the mid-Holocene were successfully identified in the KP, representing a noticeable cyclic pattern with a periodicity of around 1000 years. We propose that the Holocene millennial-scale events are common hydroclimatic phenomena at least in the East Asian monsoon system. Meanwhile, the shorter periodicity of millennial-scale events than that of the North Atlantic region is likely to decouple the EASM system from the North Atlantic climate system. This observation suggests that weak EASM and North Atlantic Bond events may have been induced independently by direct solar activity (and then possible feedback) and ocean-ice sheet dynamics, respectively, rather than simple propagation from the North Atlantic to the EASM regions.
- provenance
- Made available in Cube on 2018-09-28T10:18:25Z (GMT). No. of bitstreams: 0
- language
- English
- author
- Jo, Kyoung-nam
- Yi, Sangheon
- Lee, Jin-Yong
- Woo, Kyung Sik
- Cheng, Hai
- Edwards, Lawrence R.
- Kim, Sang-Tae
- orcid
- CHENG, HAI/0000-0002-5305-9458
- accessioned
- 2018-09-28T10:18:25Z
- available
- 2018-09-28T10:18:25Z
- issued
- 2017
- citation
- SCIENTIFIC REPORTS(7)
- issn
- 2045-2322
- uri
- http://open-repository.kisti.re.kr/cube/handle/open_repository/473398.do
- Funder
- 과학기술정보통신부
- Funding Program
- 한국지질자원연구원연구운영비지원
- Project ID
- 1711051646
- Jurisdiction
- Rep.of Korea
- Project Name
- 지질 기록체를 활용한 한반도 아열대화 규명 연구 : 중기 홀로세 기후-지표환경 특성 평가
- rights
- openAccess
- type
- article
- Files in This Item
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