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.
Enregistré dans:
| Auteurs principaux: | , , , |
|---|---|
| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2019
|
| Sujets: | |
| Accès en ligne: | https://doaj.org/article/78676b502e854aaf9b10a71db83e52c1 |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|