Articles | Volume 16, issue 5
https://doi.org/10.5194/cp-16-1987-2020
https://doi.org/10.5194/cp-16-1987-2020
Research article
 | 
30 Oct 2020
Research article |  | 30 Oct 2020

Wet–dry status change in global closed basins between the mid-Holocene and the Last Glacial Maximum and its implication for future projection

Xinzhong Zhang, Yu Li, Wangting Ye, Simin Peng, Yuxin Zhang, Hebin Liu, Yichan Li, Qin Han, and Lingmei Xu

Related authors

Simultaneous seasonal dry/wet signals in eastern and central Asia since the Last Glacial Maximum
Simin Peng, Yu Li, Zhansen Zhang, Mingjun Gao, Xiaowen Chen, Junjie Duan, and Yaxin Xue
Clim. Past, 20, 2415–2429, https://doi.org/10.5194/cp-20-2415-2024,https://doi.org/10.5194/cp-20-2415-2024, 2024
Short summary
Gridded pollen-based Holocene regional plant cover in temperate and northern subtropical China suitable for climate modelling
Furong Li, Marie-José Gaillard, Xianyong Cao, Ulrike Herzschuh, Shinya Sugita, Jian Ni, Yan Zhao, Chengbang An, Xiaozhong Huang, Yu Li, Hongyan Liu, Aizhi Sun, and Yifeng Yao
Earth Syst. Sci. Data, 15, 95–112, https://doi.org/10.5194/essd-15-95-2023,https://doi.org/10.5194/essd-15-95-2023, 2023
Short summary
Synergy of the westerly winds and monsoons in the lake evolution of global closed basins since the Last Glacial Maximum and implications for hydrological change in central Asia
Yu Li and Yuxin Zhang
Clim. Past, 16, 2239–2254, https://doi.org/10.5194/cp-16-2239-2020,https://doi.org/10.5194/cp-16-2239-2020, 2020
Short summary

Related subject area

Subject: Feedback and Forcing | Archive: Terrestrial Archives | Timescale: Holocene
Viticulture extension in response to global climate change drivers – lessons from the past and future projections
Joel Guiot, Nicolas Bernigaud, Alberte Bondeau, Laurent Bouby, and Wolfgang Cramer
Clim. Past, 19, 1219–1244, https://doi.org/10.5194/cp-19-1219-2023,https://doi.org/10.5194/cp-19-1219-2023, 2023
Short summary
Volcanism and climate change as drivers in Holocene depositional dynamic of Laguna del Maule (Andes of central Chile – 36° S)
Matías Frugone-Álvarez, Claudio Latorre, Fernando Barreiro-Lostres, Santiago Giralt, Ana Moreno, Josué Polanco-Martínez, Antonio Maldonado, María Laura Carrevedo, Patricia Bernárdez, Ricardo Prego, Antonio Delgado Huertas, Magdalena Fuentealba, and Blas Valero-Garcés
Clim. Past, 16, 1097–1125, https://doi.org/10.5194/cp-16-1097-2020,https://doi.org/10.5194/cp-16-1097-2020, 2020
Short summary
Solar modulation of flood frequency in central Europe during spring and summer on interannual to multi-centennial timescales
Markus Czymzik, Raimund Muscheler, and Achim Brauer
Clim. Past, 12, 799–805, https://doi.org/10.5194/cp-12-799-2016,https://doi.org/10.5194/cp-12-799-2016, 2016
Short summary

Cited articles

An, Z., Porter, S. C., Kutzbach, J. E., Wu, X., Wang, S., Liu, X., Li, X., and Zhou, W.: Asynchronous Holocene optimum of the East Asian monsoon, Quaternary Sci. Rev., 19, 743–762, https://doi.org/10.1016/s0277-3791(99)00031-1, 2000. 
Bacon, S., Jayko, A., Owen, L., Lindvall, S., Rhodes, E., Schumer, R., and Decker, D.: A 50,000-year record of lake-level variations and overflow from Owens Lake, eastern California, USA, Quaternary Sci. Rev., 238, 106312, https://doi.org/10.1016/j.quascirev.2020.106312, 2020. 
Batchelor, C. L., Margold, M., Krapp, M., Murton, D. K., Dalton, A. S., Gibbard, P. L., Stokes, C. R., Murton, J. B., and Manica, A.:. The configuration of Northern Hemisphere ice sheets through the Quaternary, Nat. Commun., 10, 1–10, https://doi.org/10.1038/s41467-019-11601-2, 2019. 
Bernal, J. P., Cruz, F. W., Stríkis, N. M., Wang, X., Deininger, M., Catunda, M. C. A., Ortega-Obregóna, C., Cheng, H., Edwards, R. L., and Auler, A. S.: High-resolution Holocene South American monsoon history recorded by a speleothem from Botuverá Cave, Brazil, Earth Planet. Sci. Lett., 450, 186–196, https://doi.org/10.1016/j.epsl.2016.06.008, 2016. 
Download
Short summary
Many closed-basin lakes are now drying, causing water crisis in hinterlands; however, many were much wetter in a similar warm world 6000 years ago. Why do they respond differently and will it be wetter or drier? We assess the wet–dry status and mechanism at different timescales and suggest that moisture change in the past and future warm periods are controlled by summer and winter precipitation, respectively. Diversified responses in different closed basins need a more resilient strategy.