66 citations as recorded by crossref.

1. The prolonged weak monsoon event in East Asia and the interhemispheric seesaw: implications for persistent AMOC forcing at the mid-late Holocene transition M. Li et al. https://doi.org/10.1016/j.gloplacha.2025.105091
2. High-resolution reconstructions of Holocene sea-surface conditions from dinoflagellate cyst assemblages in the northern South China Sea Z. Li et al. https://doi.org/10.1016/j.margeo.2021.106528
3. Response of a low elevation carbonate lake in the Yucatan Peninsula (Mexico) to climatic and human forcings S. Metcalfe et al. https://doi.org/10.1016/j.quascirev.2022.107445
4. A speleothem record of hydroclimate variability in northwestern Madagascar during the mid-late Holocene B. Williams et al. https://doi.org/10.1177/09596836231225725
5. Climate change and early urbanism in Southwest Asia: A review D. Lawrence et al. https://doi.org/10.1002/wcc.741
6. The Culture of the Motillas in La Mancha - witness to the 4.2 ka cal BP Climate Event M. Mejías Moreno et al. https://doi.org/10.21701/bolgeomin.131.1.006
7. Hydroclimate variability in the Madagascar and Southeast African summer monsoons at the Mid- to Late-Holocene transition N. Scroxton et al. https://doi.org/10.1016/j.quascirev.2022.107874
8. The Influence of Increased CO2 Concentrations on AMOC Interdecadal Variability Under the LGM Background Y. Gao et al. https://doi.org/10.1029/2023JD039976
9. Holocene vegetation patterns in southern Lithuania indicate astronomical forcing on the millennial and centennial time scales A. Spiridonov et al. https://doi.org/10.1038/s41598-019-51321-7
10. 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
11. A review of paleofloods in the middle-lower reaches of the Yangtze River during the Holocene: Processes, causes and effects Z. Zhang et al. https://doi.org/10.1016/j.quascirev.2024.109019
12. Subsistence economic changes and their influencing factors in the lower Yangtze river region during 11,000–2,300 BP: archaeobotanical and zooarchaeological evidence H. Li et al. https://doi.org/10.1016/j.quaint.2025.109891
13. Low-latitude forcing on 4.2 ka event indicated by records in the Asian monsoon region X. Zhou et al. https://doi.org/10.1016/j.gloplacha.2024.104401
14. Seasonal climatic patterns of the Pleistocene–Holocene transition in northwestern Mexico reconstructed from pollen data C. Galaz-Samaniego et al. https://doi.org/10.1007/s00382-026-08156-6
15. Tipping points in ocean and atmosphere circulations S. Loriani et al. https://doi.org/10.5194/esd-16-1611-2025
16. Holocene insolation and sea surface temperature influences on the polar front jet stream and precipitation in the midcontinental United States D. Gibson et al. https://doi.org/10.1016/j.quascirev.2024.108865
17. Coral Paleoclimate Perspectives Support the Role of Low‐Latitude Forcing on the 4.2 ka BP Event X. Chen et al. https://doi.org/10.1029/2023GL104010
18. The 4.2 ka event in the Northern Hemisphere: Spatial heterogeneity and driving mechanisms of hydroclimatic change Q. Nan et al. https://doi.org/10.1016/j.earscirev.2025.105128
19. Expression of the “4.2 ka event” in the southern Rocky Mountains, USA D. Liefert & B. Shuman https://doi.org/10.5194/cp-18-1109-2022
20. Possible Underlying Mechanisms of Severe Decadal Droughts in Arid Central Asia During the Last 530 Years: Results From the Last Millennium Climate Reanalysis Project Version 2.0 Y. Peng https://doi.org/10.1029/2020JD033409
21. Ecosystem collapses in Southwest China revealed by stalagmite records during the Mid-to-Late Holocene S. Yang et al. https://doi.org/10.1016/j.palaeo.2026.113862
22. Holocene changes in moisture source and temperature revealed by the oxygen isotopic composition of fossil Daphnia ephippia in Sierra Nevada, southern Spain C. López-Blanco et al. https://doi.org/10.1016/j.catena.2025.108984
23. Late Holocene vegetation succession and climate change in the Central Plains of China: Evidence from a high-resolution pollen record P. Chen et al. https://doi.org/10.1016/j.catena.2024.108589
24. Episodic deposition of stalagmites in the northeastern Democratic Republic of the Congo suggests Equatorial Humid Periods during insolation maxima L. Dupont et al. https://doi.org/10.1016/j.quascirev.2022.107552
25. Centennial Variation and Mechanism of the Extreme High Temperatures in Summer over China during the Holocene Forced by Total Solar Irradiance L. Liu et al. https://doi.org/10.3390/atmos14081207
26. Impact of Multiscale Variability on Last 6,000 Years Indian and West African Monsoon Rain P. Braconnot et al. https://doi.org/10.1029/2019GL084797
27. Late Holocene temperature variability in northern Xinjiang (NW China) and its potential connection to the Atlantic Meridional Overturning Circulation R. Chen et al. https://doi.org/10.1016/j.quascirev.2025.109571
28. Collapse of prehistoric cultures in central-eastern China linked to the El Niño-like states during the 4.2 ka event S. Jiang et al. https://doi.org/10.1016/j.gloplacha.2025.104772
29. North Atlantic linkage to hydroclimatic weakening in the NW Himalaya during the 4.2 ka event D. Singh et al. https://doi.org/10.1016/j.palaeo.2026.114101
30. The tripartite 4.2 ka event in East Asia: Stalagmite evidence and its interregional implications Z. Zhang et al. https://doi.org/10.1016/j.gloplacha.2025.105200
31. The connection of east Asia and southwestern north America in climate change mode since the last glacial maximum at various timescales Y. Li et al. https://doi.org/10.1016/j.quascirev.2021.106935
32. Influence of the North Atlantic subpolar gyre circulation on the 4.2 ka BP event B. Jalali et al. https://doi.org/10.5194/cp-15-701-2019
33. Double-plunging structure of the Bond 4 event evidenced in new mid-Holocene stalagmite records from northern China Q. Wang et al. https://doi.org/10.1016/j.gloplacha.2025.105082
34. The Impacts of Regime Shift in Summer Arctic Oscillation on Precipitation in East Asia X. Zou et al. https://doi.org/10.3390/atmos15030283
35. 末次盛冰期以来中国区域气候降尺度模拟研究 乃. 曹 et al. https://doi.org/10.1360/SSTe-2025-0391
36. Asynchronous 500-year summer monsoon rainfall cycles between Northeast and Central China during the Holocene D. Xu et al. https://doi.org/10.1016/j.gloplacha.2020.103324
37. Regional but not global temperature variability underestimated by climate models at supradecadal timescales T. Laepple et al. https://doi.org/10.1038/s41561-023-01299-9
38. Climate and sea-level fluctuations on the western coast of Bohai Bay during the 4.2 ka event: Multi-proxy evidence from the Nandagang area of Cangzhou, China H. You et al. https://doi.org/10.1016/j.quascirev.2023.108467
39. A continuous simulation of Holocene effective moisture change represented by variability of virtual lake level in East and Central Asia Y. Li et al. https://doi.org/10.1007/s11430-019-9576-x
40. The 4.2 ka event: A review of palaeoclimate literature and directions for future research S. Helama https://doi.org/10.1177/09596836241254486
41. The spatial rainfall pattern in China during the 4.2 ka event and its forcing mechanism B. Zhao et al. https://doi.org/10.1007/s00382-026-08273-2
42. Quantitative paleoclimate reconstruction in the Yangtze River Delta since the Last Glacial Maximum based on pollen records F. Chen et al. https://doi.org/10.1038/s41598-025-33476-8
43. Late-Holocene: Cooler or warmer? H. Wanner https://doi.org/10.1177/09596836211019106
44. The most complete Holocene peat record from Central Europe: multi-proxy reconstruction of postglacial wetness changes and climate events from Linje peatland, Poland E. Poolma et al. https://doi.org/10.5194/cp-21-1933-2025
45. Spatially diverse hydroclimatic response to the 4.2 ka event in the Asian monsoon region J. Lin et al. https://doi.org/10.1016/j.quascirev.2022.107809
46. Assessing the temporal stability of snail-climate relationships since the Last Glacial Maximum: Insights from boosted regression trees and LOESS models F. Wei et al. https://doi.org/10.1016/j.palaeo.2025.112771
47. Regional climate downscaling simulations for China since the Last Glacial Maximum N. Cao et al. https://doi.org/10.1007/s11430-025-1962-7
48. Quantitative climate reconstruction of the Mid- to late Holocene based on pollen records from Northern Shandong, China Y. Li et al. https://doi.org/10.1016/j.palaeo.2025.112815
49. An absolutely dated mid-Holocene English yew chronology offers new opportunities for archaeological and palaeoenvironmental research T. Bebchuk et al. https://doi.org/10.1177/09596836251407634
50. The Gutian Invasion in the Middle East as a Possible Anthropogenic Trigger Factor in the Development of the 4.2 ky Event T. Szczęsny https://doi.org/10.4236/oje.2019.99024
51. 全新世不同时期夏季西风急流与东亚夏季风的协同演变及其对中国降水格局的影响 雅. 刘 et al. https://doi.org/10.1360/SSTe-2024-0147
52. Collapse and continuity: A multi-proxy reconstruction of settlement organization and population trajectories in the Northern Fertile Crescent during the 4.2kya Rapid Climate Change event D. Lawrence et al. https://doi.org/10.1371/journal.pone.0244871
53. Mid-late Holocene environmental change and social resilience in Central Plains of China: Evidence from Sha-Ying Rivers floodplain W. Li et al. https://doi.org/10.1016/j.quascirev.2025.109692
54. Mid-Holocene to present-day evolution of the Indian monsoon in transient global simulations J. Crétat et al. https://doi.org/10.1007/s00382-020-05418-9
55. El Niño/Southern Oscillation during the 4.2 ka event recorded by growth rates of corals from the North South China Sea S. Dang et al. https://doi.org/10.1007/s13131-019-1520-5
56. Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate Y. Kang & H. Yang https://doi.org/10.5194/cp-19-2013-2023
57. Fossil leaf wax hydrogen isotopes reveal variability of Atlantic and Mediterranean climate forcing on the southeast Iberian Peninsula between 6000 to 3000 cal. BP J. Schirrmacher et al. https://doi.org/10.1371/journal.pone.0243662
58. Tropical Indian Ocean basin hydroclimate at the Mid- to Late-Holocene transition and the double drying hypothesis N. Scroxton et al. https://doi.org/10.1016/j.quascirev.2022.107837
59. Spatial and temporal characteristics of the precipitation response to the 4.2 ka event in the Asian summer monsoon region D. Wang et al. https://doi.org/10.1016/j.gloplacha.2022.103854
60. External Forcings Caused the Tripole Trend of Asian Precipitation During the Holocene H. Xu et al. https://doi.org/10.1029/2023JD039460
61. Climatic change around the 4.2 ka event in coastal areas of the East China Sea and its potential influence on prehistoric Japanese people H. Kajita et al. https://doi.org/10.1016/j.palaeo.2022.111310
62. The co-evolution of East Asian subtropical westerly jet and East Asian summer monsoon during different time periods in the Holocene and its influence on precipitation patterns in China Y. Liu et al. https://doi.org/10.1007/s11430-024-1505-3
63. Additional multi-proxy stalagmite evidence from northeast Namibia supports recent models of wetter conditions during the 4.2 ka Event in the Southern Hemisphere L. Railsback et al. https://doi.org/10.1016/j.palaeo.2021.110756
64. The ‘4.2 ka drought event’ and the fall of the Harappan Civilization: A critical review T. Jahan & M. Quamar https://doi.org/10.1016/j.revpalbo.2024.105187
65. Climate model experiments on the 4.2 ka event: The impact of tropical sea-surface temperature anomalies and desertification H. Renssen https://doi.org/10.1177/09596836221074031
66. A loess-paleosol record of climate and vegetation change during the past 27,000 years from South-East of the Caspian Sea, Iran S. Maleki et al. https://doi.org/10.1016/j.quaint.2022.12.011