Articles | Volume 14, issue 4
https://doi.org/10.5194/cp-14-577-2018
https://doi.org/10.5194/cp-14-577-2018
Research article
 | 
26 Apr 2018
Research article |  | 26 Apr 2018

Timescale dependence of the relationship between the East Asian summer monsoon strength and precipitation over eastern China in the last millennium

Jian Shi, Qing Yan, and Huijun Wang

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Subject: Atmospheric Dynamics | Archive: Modelling only | Timescale: Centennial-Decadal
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Cited articles

Bothe, O., Jungclaus, J. H., and Zanchettin, D.: Consistency of the multi-model CMIP5/PMIP3-past1000 ensemble, Clim. Past, 9, 2471–2487, https://doi.org/10.5194/cp-9-2471-2013, 2013. 
Brown, J. R., Hope, P., Gergis, J., and Henley, B. J.: ENSO teleconnections with Australian rainfall in coupled model simulations of the last millennium, Clim. Dynam., 47, 79–93, 2015. 
Chen, J., Chen, F., Feng, S., Huang, W., Liu, J., and Zhou, A.: Hydroclimatic changes in China and surroundings during the Medieval Climate Anomaly and Little Ice Age: spatial patterns and possible mechanisms, Quaternary Sci. Rev., 107, 98–111, https://doi.org/10.1016/j.quascirev.2014.10.012, 2015. 
Coats, S., Cook, B. I., Smerdon, J. E., and Seager, R.: North American pancontinental droughts in model simulations of the last millennium, J. Clim., 28, 2025–2043, 2015. 
Cook, E. R., Krusic, P. J., Anchukaitis, K. J., Buckley, B. M., Nakatsuka, T., and Sano, M.: Tree-ring reconstructed summer temperature anomalies for temperate East Asia since 800 CE, Clim. Dynam., 41, 2957–2972, 2013. 
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The paleo-East Asian summer monsoon (EASM) is widely reconstructed by precipitation/humidity proxies over East Asia. However, based on numerical simulations over the last millennium, we find that the multi-decadal relationship between the EASM and precipitation over eastern China is non-stationary, which may be attributed to the internal variability of the climate system rather than the external forcings. In contrast, the centennial EASM–precipitation relationship is much more close and stable.