Abstract
The Asian–Australian monsoon is an important component of the Earth’s climate system that influences the societal and economic activity of roughly half the world’s population. The past strength of the rain-bearing East Asian summer monsoon can be reconstructed with archives such as cave deposits1,2,3, but the winter monsoon has no such signature in the hydrological cycle and has thus proved difficult to reconstruct. Here we present high-resolution records of the magnetic properties and the titanium content of the sediments of Lake Huguang Maar in coastal southeast China over the past 16,000 years, which we use as proxies for the strength of the winter monsoon winds. We find evidence for stronger winter monsoon winds before the Bølling–Allerød warming, during the Younger Dryas episode and during the middle and late Holocene, when cave stalagmites suggest weaker summer monsoons1,2,3. We conclude that this anticorrelation is best explained by migrations in the intertropical convergence zone. Similar migrations of the intertropical convergence zone have been observed in Central America for the period ad 700 to 900 (refs 4–6), suggesting global climatic changes at that time. From the coincidence in timing, we suggest that these migrations in the tropical rain belt could have contributed to the declines of both the Tang dynasty in China and the Classic Maya in Central America.
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References
Wang, Y. J. et al. A high-resolution absolute-dated Late Pleistocene monsoon record from Hulu Cave, China. Science 294, 2345–2348 (2001)
Yuan, D. et al. Timing, duration, and transitions of the Last Interglacial Asian Monsoon. Science 304, 575–578 (2004)
Dykoski, C. A. et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth Planet. Sci. Lett. 233, 71–86 (2005)
Diamond, J. Collapse (Penguin, London, 2005)
Fagan, B. Floods, Famines and Emperors: El Nino and the Fate of Civilizations (Pimlico, London, 2000)
Haug, G. H. et al. Climate and the collapse of Maya civilization. Science 299, 1731–1735 (2003)
Kumar, K. K., Rajagopalan, B. & Cane, M. A. On the weakening of the relationship between the Indian monsoon and ENSO. Science 284, 2156–2159 (1999)
Wang, B. The Asian Monsoon (Springer, Berlin, 2006)
Thompson, L. G. et al. Tropical climate instability: the last glacial cycle from a Qinghai-Tibetan ice core. Science 276, 1821–1825 (1997)
Sirocko, F., Garbe-Schonberg, D., McIntyre, A. & Molfino, B. Teleconnections between the subtropical monsoons and high-latitude climates during the last deglaciation. Science 272, 526–529 (1996)
Heslop, D. et al. Sub-millennial scale variations in East Asian monsoon systems recorded by dust deposits from the North-Western Chinese loess plateau. Phys. Chem. Earth 24, 785–792 (1999)
Porter, S. C. & An, Z. Correlation between climate events in the North Atlantic and China during the last glaciation. Nature 375, 305–308 (1995)
Oppo, D. W. & Sun, Y. Amplitude and timing of sea-surface temperature change in the northern South China Sea: Dynamic link to the East Asian monsoon. Geology 33, 785–788 (2005)
Liu, T. & Ding, Z. Chinese loess and the paleomonsoon. Annu. Rev. Earth Planet. Sci. 26, 111–145 (1998)
Ding, Z., Rutter, N., Han, J. & Liu, T. A coupled environmental system formed at about 2.5 Ma in East Asia. Palaeogeogr. Palaeoclimatol. Palaeoecol. 94, 223–242 (1992)
Hughen, K. A., Overpeck, J. T., Peterson, L. C. & Trumbore, S. Rapid climate changes in the tropical Atlantic region during the last deglaciation. Nature 380, 51–54 (1996)
Haug, G. H., Hughen, K. A., Sigman, D. M., Peterson, L. C. & Röhl, U. Southward migration of the Intertropical Convergence Zone through the Holocene. Science 293, 1304–1308 (2001)
Wang, X. et al. Wet periods in northeastern Brazil over the past 210 kyr linked to distant climate anomalies. Nature 432, 740–743 (2004)
Cane, M. A. The evolution of El Nino, past and future. Earth Planet. Sci. Lett. 230, 227–240 (2005)
Koutavas, A. & Lynch-Stieglitz, J. Marchitto Jr, T. M. & Sachs, J. P. El Nino-like pattern in ice age tropical Pacific sea surface temperature. Science 297, 226–230 (2002)
Ivanochko, T. S. et al. Variations in tropical convection as an amplifier of global climate change at the millennial scale. Earth Planet. Sci. Lett. 235, 302–314 (2005)
Bloemendal, J., King, J. W., Hall, F. R. & Doh, S. J. Rock magnetism of Late Neogene and Pleistocene deep-sea sediments: Relationship to sediment source, diagenetic processes and sediment lithology. J. Geophys. Res. 97, 4361–4375 (1992)
Mingram, J. et al. The Huguang maar lake – a high-resolution record of palaeoenvironmental and palaeoclimatic changes over the last 78,000 years from South China. Quat. Int. 122, 85–107 (2004)
Wang, L. et al. East Asian monsoon climate during the Late Pleistocene: high-resolution sediment records from the South China Sea. Mar. Geol. 156, 245–284 (1999)
Hastenrath, S. & Greischar, L. Circulation mechanisms related to northeast Brazil rainfall anomalies. J. Geophys. Res. 98, 5093–5102 (1993)
Wang, L. et al. Holocene variations in Asian monsoon moisture: a bidecadal sediment record from South China Sea. Geophys. Res. Lett. 26, 2889–2892 (1999)
Fleitmann, D. et al. Holocene forcing of the Indian Monsoon recorded in a stalagmite from Southern Oman. Science 300, 1737–1739 (2003)
deMenocal, P. B. Cultural responses to climate change during the late Holocene. Science 292, 667–673 (2001)
Hodell, D. A., Brenner, M., Curtis, J. H. & Guilderson, T. Solar forcing of drought frequency in the Maya lowlands. Science 292, 1367–1370 (2001)
Blunden, C. & Elvin, M. Cultural Atlas of China (Checkmark Books, New York, 1998)
Acknowledgements
We thank M. Cane, R. Seager, P. deMenocal and S. Clemens for discussions, comments and reviews. This work was supported by the Deutsche Forschungsgemeinschaft (DFG). D.M.S. and G.H.H. thank the Humboldt Foundation for support. D.M.S. was also supported by BP and Ford Motor Company through the Princeton Carbon Mitigation Initiative.
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Yancheva, G., Nowaczyk, N., Mingram, J. et al. Influence of the intertropical convergence zone on the East Asian monsoon. Nature 445, 74–77 (2007). https://doi.org/10.1038/nature05431
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DOI: https://doi.org/10.1038/nature05431
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