Rate-and-state friction explains glacier surge propagation
Predicting the friction at the ice/bedrock interface prevents a full understanding of glacier dynamics. Here, the authors present a framework for the transient evolution of basal shear stress and incorporate it in glacier simulations. This tool is capable of explaining surge onset and propagation.
| প্রধান লেখক: | , , , |
|---|---|
| বিন্যাস: | প্রবন্ধ |
| ভাষা: | English |
| প্রকাশিত: |
Nature Portfolio
2019-06-01
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| মালা: | Nature Communications |
| অনলাইন ব্যবহার করুন: | https://doi.org/10.1038/s41467-019-10506-4 |