Articles | Volume 23, issue 4
https://doi.org/10.5194/hess-23-1931-2019
https://doi.org/10.5194/hess-23-1931-2019
Research article
 | 
10 Apr 2019
Research article |  | 10 Apr 2019

Evaluating the relative importance of precipitation, temperature and land-cover change in the hydrologic response to extreme meteorological drought conditions over the North American High Plains

Annette Hein, Laura Condon, and Reed Maxwell

Viewed

Total article views: 3,147 (including HTML, PDF, and XML)
HTML PDF XML Total BibTeX EndNote
2,059 1,027 61 3,147 67 64
  • HTML: 2,059
  • PDF: 1,027
  • XML: 61
  • Total: 3,147
  • BibTeX: 67
  • EndNote: 64
Views and downloads (calculated since 02 Oct 2018)
Cumulative views and downloads (calculated since 02 Oct 2018)

Viewed (geographical distribution)

Total article views: 3,147 (including HTML, PDF, and XML) Thereof 2,854 with geography defined and 293 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Discussed (final revised paper)

Discussed (preprint)

Latest update: 27 Mar 2024
Download
Short summary
Drought is a natural disaster that can result from changes to temperature, precipitation and/or vegetation. Here we apply a high-resolution computer model to explore the relative importance of each factor on the North American High Plains, one of the most important agricultural regions of the USA. Decreased precipitation caused larger changes in hydrologic variables (evapotranspiration, soil moisture, stream flow and water table levels) than increased temperature or disturbed vegetation did.