Climate of the Past
Climate of the Past
CP
Articles | Volume 16, issue 5
Articles | Volume 16, issue 5
https://doi.org/10.5194/cp-16-1987-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/cp-16-1987-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 16, issue 5
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

Viewed

Total article views: 2,665 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,710 797 158 2,665 191 102 150
  • HTML: 1,710
  • PDF: 797
  • XML: 158
  • Total: 2,665
  • Supplement: 191
  • BibTeX: 102
  • EndNote: 150
Views and downloads (calculated since 02 Mar 2020)
Cumulative views and downloads (calculated since 02 Mar 2020)

Viewed (geographical distribution)

Total article views: 2,665 (including HTML, PDF, and XML) Thereof 2,254 with geography defined and 411 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 25 Oct 2025
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.
Read more
Share