Deposits in a Chinese cave tell the story of the region's climate stretching back more than 200,000 years, well past the last interglacial warm period — an invaluable resource for understanding the Asian monsoon.
References
Wang, Y. et al. Nature 451, 1090–1093 (2008).
Cheng, H. et al. Geology 34, 217–220 (2006).
Dykoski, C. A. et al. Earth Planet. Sci. Lett. 233, 71–86 (2005).
Kelly, M. J. et al. Palaeogeogr. Palaeoclim. Palaeoecol. 236, 20–38 (2006).
Wang, Y. J. et al. Science 294, 2345–2348 (2001).
Wang, Y. et al. Science 308, 854–857 (2005).
Yuan, D. et al. Science 304, 575–578 (2004).
Kutzbach, J. E. Science 214, 59–61 (1981).
McDermott, F. Quat. Sci. Rev. 23, 901–918 (2004).
Mickler, P. J., Stern, L. A. & Banner, J. L. Geol. Soc. Am. Bull. 118, 65–81 (2006).
Andersen, K. K. et al. Nature 431, 147–151 (2004).
Clemens, S. & Prell, W. Mar. Geol. 201, 35–51 (2003).
Ruddiman, W. F. Quat. Sci. Rev. 25, 657–658 (2006).
Goswami, B. N., Madhusoodanan, M. S., Neema, C. P. & Sengupta, D. Geophys. Res. Lett. 33, doi:10.1029/2005GL024803 (2006).
Barnett, T. P., Dümenil, L., Schlese, U. & Roeckner, E. Science 239, 504–507 (1988).
Berger, A. L. J. Atmos. Sci. 35, 2632–2637 (1978).
Author information
Authors and Affiliations
Rights and permissions
About this article
Cite this article
Overpeck, J., Cole, J. The rhythm of the rains. Nature 451, 1062–1063 (2008). https://doi.org/10.1038/4511061a
Published:
Issue Date:
DOI: https://doi.org/10.1038/4511061a
- Springer Nature Limited
This article is cited by
-
Chinese stalagmite paleoclimate researches: A review and perspective
Science China Earth Sciences (2019)
-
1000-Year Quasi-Periodicity of Weak Monsoon Events in Temperate Northeast Asia since the Mid-Holocene
Scientific Reports (2017)
-
Air mass origin signals in δ 18O of tree-ring cellulose revealed by back-trajectory modeling at the monsoonal Tibetan plateau
International Journal of Biometeorology (2017)
-
Global monsoon in a geological perspective
Science Bulletin (2009)