» Articles » PMID: 34282014

Long-term Decrease in Asian Monsoon Rainfall and Abrupt Climate Change Events over the Past 6,700 Years

Abstract

Asian summer monsoon (ASM) variability and its long-term ecological and societal impacts extending back to Neolithic times are poorly understood due to a lack of high-resolution climate proxy data. Here, we present a precisely dated and well-calibrated tree-ring stable isotope chronology from the Tibetan Plateau with 1- to 5-y resolution that reflects high- to low-frequency ASM variability from 4680 BCE to 2011 CE. Superimposed on a persistent drying trend since the mid-Holocene, a rapid decrease in moisture availability between ∼2000 and ∼1500 BCE caused a dry hydroclimatic regime from ∼1675 to ∼1185 BCE, with mean precipitation estimated at 42 ± 4% and 5 ± 2% lower than during the mid-Holocene and the instrumental period, respectively. This second-millennium-BCE megadrought marks the mid-to late Holocene transition, during which regional forests declined and enhanced aeolian activity affected northern Chinese ecosystems. We argue that this abrupt aridification starting ∼2000 BCE contributed to the shift of Neolithic cultures in northern China and likely triggered human migration and societal transformation.

Citing Articles

Recent centennial drought on the Tibetan Plateau is outstanding within the past 3500 years.

Liu Y, Song H, An Z, Li Q, Leavitt S, Buntgen U Nat Commun. 2025; 16(1):1311.

PMID: 39900890 PMC: 11790959. DOI: 10.1038/s41467-025-56687-z.


Persistent humid climate favored the Qin and Western Han Dynasties in China around 2,200 y ago.

Qin C, Yang B, Brauning A, Ljungqvist F, Osborn T, Shishov V Proc Natl Acad Sci U S A. 2024; 122(1):e2415294121.

PMID: 39715434 PMC: 11725930. DOI: 10.1073/pnas.2415294121.


Radiocarbon chronology and settlement patterns in the Bronze Age of the Qaidam Basin, Northwestern China.

Li B, Ma J, Chen H, Guo M, Li J, Ren M Sci Rep. 2024; 14(1):28117.

PMID: 39548267 PMC: 11568209. DOI: 10.1038/s41598-024-79638-y.


Sahara's surface transformation forced an abrupt hydroclimate decline and Neolithic culture transition in northern China.

Hou Y, Long H, Tsukamoto S, Lu Z, Chen J, Ibarra D Innovation (Camb). 2024; 5(1):100550.

PMID: 38204586 PMC: 10777076. DOI: 10.1016/j.xinn.2023.100550.


Mid-to-late Holocene climate variability in coastal East Asia and its impact on ancient Korean societies.

Park J, Bahk J, Park J, Kim H, Choi J Sci Rep. 2023; 13(1):15379.

PMID: 37717094 PMC: 10505234. DOI: 10.1038/s41598-023-42551-x.


References
1.
Cook E, Anchukaitis K, Buckley B, DArrigo R, Jacoby G, Wright W . Asian monsoon failure and megadrought during the last millennium. Science. 2010; 328(5977):486-9. DOI: 10.1126/science.1185188. View

2.
deMenocal P . Cultural responses to climate change during the late Holocene. Science. 2001; 292(5517):667-73. DOI: 10.1126/science.1059827. View

3.
Stenseth N, Mysterud A, Ottersen G, Hurrell J, Chan K, Lima M . Ecological effects of climate fluctuations. Science. 2002; 297(5585):1292-6. DOI: 10.1126/science.1071281. View

4.
Tian H, Yan C, Xu L, Buntgen U, Stenseth N, Zhang Z . Scale-dependent climatic drivers of human epidemics in ancient China. Proc Natl Acad Sci U S A. 2017; 114(49):12970-12975. PMC: 5724254. DOI: 10.1073/pnas.1706470114. View

5.
Evans N, Bauska T, Gazquez-Sanchez F, Brenner M, Curtis J, Hodell D . Quantification of drought during the collapse of the classic Maya civilization. Science. 2018; 361(6401):498-501. DOI: 10.1126/science.aas9871. View