43 citations as recorded by crossref.

1. High-resolution reconstructions of Holocene sea-surface conditions from dinoflagellate cyst assemblages in the northern South China Sea Z. Li et al. 10.1016/j.margeo.2021.106528
2. Response of a low elevation carbonate lake in the Yucatan Peninsula (Mexico) to climatic and human forcings S. Metcalfe et al. 10.1016/j.quascirev.2022.107445
3. 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. 10.1016/j.quascirev.2021.106935
4. A speleothem record of hydroclimate variability in northwestern Madagascar during the mid-late Holocene B. Williams et al. 10.1177/09596836231225725
5. Influence of the North Atlantic subpolar gyre circulation on the 4.2 ka BP event B. Jalali et al. 10.5194/cp-15-701-2019
6. Climate change and early urbanism in Southwest Asia: A review D. Lawrence et al. 10.1002/wcc.741
7. The Impacts of Regime Shift in Summer Arctic Oscillation on Precipitation in East Asia X. Zou et al. 10.3390/atmos15030283
8. Asynchronous 500-year summer monsoon rainfall cycles between Northeast and Central China during the Holocene D. Xu et al. 10.1016/j.gloplacha.2020.103324
9. Regional but not global temperature variability underestimated by climate models at supradecadal timescales T. Laepple et al. 10.1038/s41561-023-01299-9
10. 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. 10.1016/j.quascirev.2023.108467
11. The Culture of the Motillas in La Mancha - witness to the 4.2 ka cal BP Climate Event M. Mejías Moreno et al. 10.21701/bolgeomin.131.1.006
12. A continuous simulation of Holocene effective moisture change represented by variability of virtual lake level in East and Central Asia Y. Li et al. 10.1007/s11430-019-9576-x
13. The 4.2 ka event: A review of palaeoclimate literature and directions for future research S. Helama 10.1177/09596836241254486
14. Hydroclimate variability in the Madagascar and Southeast African summer monsoons at the Mid- to Late-Holocene transition N. Scroxton et al. 10.1016/j.quascirev.2022.107874
15. The Influence of Increased CO2 Concentrations on AMOC Interdecadal Variability Under the LGM Background Y. Gao et al. 10.1029/2023JD039976
16. Late-Holocene: Cooler or warmer? H. Wanner 10.1177/09596836211019106
17. Holocene vegetation patterns in southern Lithuania indicate astronomical forcing on the millennial and centennial time scales A. Spiridonov et al. 10.1038/s41598-019-51321-7
18. Spatially diverse hydroclimatic response to the 4.2 ka event in the Asian monsoon region J. Lin et al. 10.1016/j.quascirev.2022.107809
19. 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
20. A review of paleofloods in the middle-lower reaches of the Yangtze River during the Holocene: Processes, causes and effects Z. Zhang et al. 10.1016/j.quascirev.2024.109019
21. Low-latitude forcing on 4.2 ka event indicated by records in the Asian monsoon region X. Zhou et al. 10.1016/j.gloplacha.2024.104401
22. 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. 10.1371/journal.pone.0244871
23. Mid-Holocene to present-day evolution of the Indian monsoon in transient global simulations J. Crétat et al. 10.1007/s00382-020-05418-9
24. Holocene insolation and sea surface temperature influences on the polar front jet stream and precipitation in the midcontinental United States D. Gibson et al. 10.1016/j.quascirev.2024.108865
25. Coral Paleoclimate Perspectives Support the Role of Low‐Latitude Forcing on the 4.2 ka BP Event X. Chen et al. 10.1029/2023GL104010
26. 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. 10.1007/s13131-019-1520-5
27. Quantifying effects of Earth orbital parameters and greenhouse gases on mid-Holocene climate Y. Kang & H. Yang 10.5194/cp-19-2013-2023
28. 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. 10.1371/journal.pone.0243662
29. Tropical Indian Ocean basin hydroclimate at the Mid- to Late-Holocene transition and the double drying hypothesis N. Scroxton et al. 10.1016/j.quascirev.2022.107837
30. Expression of the “4.2 ka event” in the southern Rocky Mountains, USA D. Liefert & B. Shuman 10.5194/cp-18-1109-2022
31. 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 10.1029/2020JD033409
32. Spatial and temporal characteristics of the precipitation response to the 4.2 ka event in the Asian summer monsoon region D. Wang et al. 10.1016/j.gloplacha.2022.103854
33. External Forcings Caused the Tripole Trend of Asian Precipitation During the Holocene H. Xu et al. 10.1029/2023JD039460
34. 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. 10.1016/j.palaeo.2022.111310
35. 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. 10.1016/j.palaeo.2021.110756
36. The ‘4.2 ka drought event’ and the fall of the Harappan Civilization: A critical review T. Jahan & M. Quamar 10.1016/j.revpalbo.2024.105187
37. Late holocene vegetation succession and climate change in the Central Plains of China: Evidence from a high-resolution pollen record P. Chen et al. 10.1016/j.catena.2024.108589
38. Climate model experiments on the 4.2 ka event: The impact of tropical sea-surface temperature anomalies and desertification H. Renssen 10.1177/09596836221074031
39. Episodic deposition of stalagmites in the northeastern Democratic Republic of the Congo suggests Equatorial Humid Periods during insolation maxima L. Dupont et al. 10.1016/j.quascirev.2022.107552
40. 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. 10.1016/j.quaint.2022.12.011
41. 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. 10.3390/atmos14081207
42. Impact of Multiscale Variability on Last 6,000 Years Indian and West African Monsoon Rain P. Braconnot et al. 10.1029/2019GL084797
43. Hydroclimatic variations in southeastern China during the 4.2 ka event reflected by stalagmite records H. Zhang et al. 10.5194/cp-14-1805-2018