The Cryosphere
The Cryosphere
TC
Articles | Volume 15, issue 9
Articles | Volume 15, issue 9
https://doi.org/10.5194/tc-15-4589-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/tc-15-4589-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 15, issue 9
Research article
 | 
29 Sep 2021
Research article |  | 29 Sep 2021

The role of grain size evolution in the rheology of ice: implications for reconciling laboratory creep data and the Glen flow law

Mark D. Behn, David L. Goldsby, and Greg Hirth

Viewed

Total article views: 2,404 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
1,577 782 45 2,404 151 42 32
  • HTML: 1,577
  • PDF: 782
  • XML: 45
  • Total: 2,404
  • Supplement: 151
  • BibTeX: 42
  • EndNote: 32
Views and downloads (calculated since 14 Nov 2020)
Cumulative views and downloads (calculated since 14 Nov 2020)

Viewed (geographical distribution)

Total article views: 2,404 (including HTML, PDF, and XML) Thereof 2,334 with geography defined and 70 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 18 Apr 2024
Download
Short summary
Grain size is a key microphysical property of ice, controlling the rheological behavior of ice sheets and glaciers. In this study, we develop a new model for grain size evolution in ice and show that it accurately predicts grain size in laboratory experiments and in natural ice core data. The model provides a physical explanation for the power-law relationship between stress and strain rate known as the Glen law and can be used as a predictive tool for modeling ice flow in natural systems.
Read more