Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-2291-2021
https://doi.org/10.5194/cp-17-2291-2021
Research article
 | 
29 Oct 2021
Research article |  | 29 Oct 2021

Different facets of dry–wet patterns in south-western China over the past 27 000 years

Mengna Liao, Kai Li, Weiwei Sun, and Jian Ni

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Modern Pollen Dataset of the Tibetan Plateau
Mengna Liao, Kai Li, Yili Jin, Lina Liu, Xianyong Cao, and Jian Ni
Earth Syst. Sci. Data Discuss., https://doi.org/10.5194/essd-2025-71,https://doi.org/10.5194/essd-2025-71, 2025
Revised manuscript accepted for ESSD
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Cited articles

Ahn, J., Wahlen, M., Deck, B. L., Brook, E. J., Mayewski, P. A., Taylor, K. C., and White, J. W.: A record of atmospheric CO2 during the last 40 000 years from the Siple Dome, Antarctica ice core, J. Geophys. Res.-Atmos., 109, D13305, https://doi.org/10.1029/2003JD004415, 2004. 
Aichner, B., Makhmudov, Z., Rajabov, I., Zhang, Q., Pausata, F. S., Werner, M., Heinecke, L., Kuessner, M. L., Feakins, S. J., and Sachse, D.: Hydroclimate in the Pamirs was driven by changes in precipitation-evaporation seasonality since the Last Glacial Period, Geophys. Res. Lett., 46, 13972–13983, https://doi.org/10.1029/2019GL085202, 2019. 
Blaauw, M., Christen, J. A., and Lopez, M. A. A.: rbacon: Age-depth modelling using Bayesian statistics, R package version 2.5.0 [code], available at: https://CRAN.R-project.org/package=rbacon, last access date: 15 November 2020. 
Breshears, D. D., Cobb, N. S., Rich, P. M., Price, K. P., Allen, C. D., Balice, R. G., Romme, W. H., Kastens, J. H., Floyd, M. L., and Belnap, J.: Regional vegetation die-off in response to global-change-type drought, P. Natl. Acad. Sci. USA, 102, 15144–15148, https://doi.org/10.1073/pnas.0505734102, 2005. 
Cai, Y., Fung, I. Y., Edwards, R. L., An, Z., Cheng, H., Lee, J.-E., Tan, L., Shen, C.-C., Wang, X., and Day, J. A.: Variability of stalagmite-inferred Indian monsoon precipitation over the past 252 000 yrs, P. Natl. Acad. Sci. USA, 112, 2954–2959, https://doi.org/10.1073/pnas.1424035112, 2015. 
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Short summary
The long-term trajectories of precipitation, hydrological balance and soil moisture are not completely consistent in southwest China. Hydrological balance was more sensitive to temperature change on a millennial scale. For soil moisture, plant processes also played a big role in addition to precipitation and temperature. Under future climate warming, surface water shortage in southwest China can be even more serious and efforts at reforestation may bring some relief to the soil moisture deficit.
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