Articles | Volume 12, issue 1
https://doi.org/10.5194/esurf-12-163-2024
https://doi.org/10.5194/esurf-12-163-2024
Research article
 | 
18 Jan 2024
Research article |  | 18 Jan 2024

Past anthropogenic land use change caused a regime shift of the fluvial response to Holocene climate change in the Chinese Loess Plateau

Hao Chen, Xianyan Wang, Yanyan Yu, Huayu Lu, and Ronald Van Balen

Viewed

Total article views: 1,538 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,199 279 60 1,538 122 44 34
  • HTML: 1,199
  • PDF: 279
  • XML: 60
  • Total: 1,538
  • Supplement: 122
  • BibTeX: 44
  • EndNote: 34
Views and downloads (calculated since 30 Mar 2023)
Cumulative views and downloads (calculated since 30 Mar 2023)

Viewed (geographical distribution)

Total article views: 1,538 (including HTML, PDF, and XML) Thereof 1,495 with geography defined and 43 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 13 Dec 2024
Download
Short summary
The Wei River catchment, one of the centers of the agricultural revolution in China, has experienced intense land use changes since 6000 BCE. This makes it an ideal place to study the response of river systems to anthropogenic land use change. Modeling  results show the sensitivity of discharge and sediment yield to climate change increased abruptly when the agricultural land area exceeded a threshold at around 1000 BCE. This regime shift in the fluvial catchment led to a large sediment pulse.