Articles | Volume 11, issue 6
https://doi.org/10.5194/tc-11-2847-2017
https://doi.org/10.5194/tc-11-2847-2017
Research article
 | 
11 Dec 2017
Research article |  | 11 Dec 2017

Snowmelt response to simulated warming across a large elevation gradient, southern Sierra Nevada, California

Keith N. Musselman, Noah P. Molotch, and Steven A. Margulis

Viewed

Total article views: 2,961 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,714 1,122 125 2,961 361 93 119
  • HTML: 1,714
  • PDF: 1,122
  • XML: 125
  • Total: 2,961
  • Supplement: 361
  • BibTeX: 93
  • EndNote: 119
Views and downloads (calculated since 18 Jul 2017)
Cumulative views and downloads (calculated since 18 Jul 2017)

Viewed (geographical distribution)

Total article views: 2,961 (including HTML, PDF, and XML) Thereof 2,751 with geography defined and 210 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Apr 2024
Download
Short summary
We present a study of how melt rates in the California Sierra Nevada respond to a range of warming projected for this century. Snowfall and melt were simulated for historical and modified (warmer) snow seasons. Winter melt occurs more frequently and more intensely, causing an increase in extreme winter melt. In a warmer climate, less snow persists into the spring, causing spring melt to be substantially lower. The results offer insight into how snow water resources may respond to climate change.