13 citations as recorded by crossref.

1. Reconstruction of the East Asian Summer monsoon rainfall distribution at centennial scale during the Last Glacial Maximum Y. Liu et al. 10.1016/j.palaeo.2020.109879
2. 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. 10.1016/j.palaeo.2022.111335
3. The Climate Fluctuation of the 8.2 ka BP Cooling Event and the Transition into Neolithic Lifeways in North China C. Zhao 10.3390/quat3030023
4. 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. 10.1016/j.quascirev.2024.109141
5. Large-scale vegetation response to the 8.2 ka BP cooling event in East Asia W. Zhao et al. 10.1016/j.palaeo.2022.111303
6. İklim Değişikliğinin Davranışsal İktisadı B. ÖZÜŞEN 10.21076/vizyoner.1259570
7. The Asian Summer Monsoon: Teleconnections and Forcing Mechanisms—A Review from Chinese Speleothem δ18O Records H. Zhang et al. 10.3390/quat2030026
8. 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. 10.1002/gj.3879
9. The 5400 a BP extreme weakening event of the Asian summer monsoon and cultural evolution Y. Bai et al. 10.1007/s11430-016-9017-3
10. 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. 10.1016/j.palaeo.2023.111737
11. The timing, duration and magnitude of the 8.2 ka event in global speleothem records S. Parker & S. Harrison 10.1038/s41598-022-14684-y
12. 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. 10.1029/2022GL101182
13. 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. 10.1016/j.palaeo.2022.111290