Articles | Volume 12, issue 7
https://doi.org/10.5194/cp-12-1583-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-1583-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Quantification of southwest China rainfall during the 8.2 ka BP event with response to North Atlantic cooling
Yuhui Liu
CORRESPONDING AUTHOR
State Key Laboratory of Biogeology and Environmental Geology, China
University of Geosciences, Wuhan, 430074, PR China
Faculty of Materials Science and Chemistry, China University of
Geosciences, Wuhan, 430074, PR China
Chaoyong Hu
State Key Laboratory of Biogeology and Environmental Geology, China
University of Geosciences, Wuhan, 430074, PR China
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Cited
14 citations as recorded by crossref.
- Reconstruction of the East Asian Summer monsoon rainfall distribution at centennial scale during the Last Glacial Maximum Y. Liu et al. https://doi.org/10.1016/j.palaeo.2020.109879
- Vegetation succession, climate change and cold events during 9.2–8.0 cal kyr BP in eastern China: High-resolution pollen evidence from the Yangtze delta plain area B. Song et al. https://doi.org/10.1016/j.palaeo.2022.111335
- The Climate Fluctuation of the 8.2 ka BP Cooling Event and the Transition into Neolithic Lifeways in North China C. Zhao https://doi.org/10.3390/quat3030023
- Spatiotemporal pattern of the East Asian monsoon hydroclimate during the 8.2 ka event inferred from a new speleothem multi-proxy record from SE China X. Zhang et al. https://doi.org/10.1016/j.quascirev.2024.109141
- Large-scale vegetation response to the 8.2 ka BP cooling event in East Asia W. Zhao et al. https://doi.org/10.1016/j.palaeo.2022.111303
- Variability of the East Asian summer monsoon rainfall over Korea during the Early to Mid-Holocene and its links to global climate changes S. Park & J. Lim https://doi.org/10.1017/qua.2025.10046
- İklim Değişikliğinin Davranışsal İktisadı B. ÖZÜŞEN https://doi.org/10.21076/vizyoner.1259570
- The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records H. Zhang et al. https://doi.org/10.3390/quat2030026
- Debris flow events of 4000 a BP and its resulting archaeological site destruction in Qian River gorge, the upper reach of Wei River, central China S. Fan et al. https://doi.org/10.1002/gj.3879
- The 5400 a BP extreme weakening event of the Asian summer monsoon and cultural evolution Y. Bai et al. https://doi.org/10.1007/s11430-016-9017-3
- Freshwater input variability in a west coastal area of Korea and its links to the global monsoon and ITCZ shifts during the period 8500–7800 cal yr BP S. Park et al. https://doi.org/10.1016/j.palaeo.2023.111737
- The timing, duration and magnitude of the 8.2 ka event in global speleothem records S. Parker & S. Harrison https://doi.org/10.1038/s41598-022-14684-y
- Interdecadal to Centennial Climate Variability Surrounding the 8.2 ka Event in North China Revealed Through an Annually Resolved Speleothem Record From Beijing P. Duan et al. https://doi.org/10.1029/2022GL101182
- Climatic implication of stalagmite δ13C in the middle reaches of the Yangtze River since the Last Glacial Maximum and coupling with δ18O Z. Wang et al. https://doi.org/10.1016/j.palaeo.2022.111290
14 citations as recorded by crossref.
- Reconstruction of the East Asian Summer monsoon rainfall distribution at centennial scale during the Last Glacial Maximum Y. Liu et al. https://doi.org/10.1016/j.palaeo.2020.109879
- Vegetation succession, climate change and cold events during 9.2–8.0 cal kyr BP in eastern China: High-resolution pollen evidence from the Yangtze delta plain area B. Song et al. https://doi.org/10.1016/j.palaeo.2022.111335
- The Climate Fluctuation of the 8.2 ka BP Cooling Event and the Transition into Neolithic Lifeways in North China C. Zhao https://doi.org/10.3390/quat3030023
- Spatiotemporal pattern of the East Asian monsoon hydroclimate during the 8.2 ka event inferred from a new speleothem multi-proxy record from SE China X. Zhang et al. https://doi.org/10.1016/j.quascirev.2024.109141
- Large-scale vegetation response to the 8.2 ka BP cooling event in East Asia W. Zhao et al. https://doi.org/10.1016/j.palaeo.2022.111303
- Variability of the East Asian summer monsoon rainfall over Korea during the Early to Mid-Holocene and its links to global climate changes S. Park & J. Lim https://doi.org/10.1017/qua.2025.10046
- İklim Değişikliğinin Davranışsal İktisadı B. ÖZÜŞEN https://doi.org/10.21076/vizyoner.1259570
- The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records H. Zhang et al. https://doi.org/10.3390/quat2030026
- Debris flow events of 4000 a BP and its resulting archaeological site destruction in Qian River gorge, the upper reach of Wei River, central China S. Fan et al. https://doi.org/10.1002/gj.3879
- The 5400 a BP extreme weakening event of the Asian summer monsoon and cultural evolution Y. Bai et al. https://doi.org/10.1007/s11430-016-9017-3
- Freshwater input variability in a west coastal area of Korea and its links to the global monsoon and ITCZ shifts during the period 8500–7800 cal yr BP S. Park et al. https://doi.org/10.1016/j.palaeo.2023.111737
- The timing, duration and magnitude of the 8.2 ka event in global speleothem records S. Parker & S. Harrison https://doi.org/10.1038/s41598-022-14684-y
- Interdecadal to Centennial Climate Variability Surrounding the 8.2 ka Event in North China Revealed Through an Annually Resolved Speleothem Record From Beijing P. Duan et al. https://doi.org/10.1029/2022GL101182
- Climatic implication of stalagmite δ13C in the middle reaches of the Yangtze River since the Last Glacial Maximum and coupling with δ18O Z. Wang et al. https://doi.org/10.1016/j.palaeo.2022.111290
Saved (final revised paper)
Latest update: 23 Jun 2026
Short summary
The 8.2 ka BP event, a global climate anomaly that occurred 8200 years ago, could provide climate teleconnection information for the simulation of abrupt climate changes, but there are few quantitative reconstructions of this event. This paper provides a 10-year resolution rainfall record from the East Asian monsoon area during the event, showing the reduced rainfall in southwest China during the 8.2 ka BP period was coupled with Greenland cooling with a possible response rate of 110 ± 30 mm/℃.
The 8.2 ka BP event, a global climate anomaly that occurred 8200 years ago, could provide...