How rock glacier hydrology, deformation velocities and ground temperatures interact: Examples from the Swiss Alps-Reference-Cited by-同舟云学术

How rock glacier hydrology, deformation velocities and ground temperatures interact: Examples from the Swiss Alps

Published:2019-09-05 Issue:1 Volume:31 Page:3-14
ISSN:1045-6740
Container-title:Permafrost and Periglacial Processes
language:en
Short-container-title:Permafrost and Periglac Process

Author:

Kenner Robert¹^ORCID,Pruessner Luisa²^ORCID,Beutel Jan³^ORCID,Limpach Philippe⁴⁵,Phillips Marcia¹

Affiliation:

1. WSL Institute for Snow and Avalanche Research SLF Davos Switzerland

2. Laboratory of Hydraulics Hydrology and GlaciologyETH Zürich Switzerland

3. Computer Engineering and Networks LaboratoryETH Zürich Switzerland

4. Institute of Geodesy and PhotogrammetryETH Zürich Switzerland

5. BSF Swissphoto AG Regensdorf Switzerland

Funder

Federal Office of Topography swisstopo

Publisher

Wiley

Subject

Earth-Surface Processes

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2023

Reference60 articles.

1. Nature and importance of mass-wasting by rock glaciers in alpine permafrost environments

2. ROCK GLACIERS IN THE ALASKA RANGE

3. HaeberliW.Creep of mountain permafrost: Internal structure and flow of alpine rock glaciers.Mitteilung der VAW/ETH Zürich.1985;77.

4. ChaixA.Les coulées de blocs du Parc national suisse d'Engadine (Note préliminaire).Le Globe. Revue genevoise de géographie. 1923:1–35.

5. KaufmannV.Deformation analysis of the Doesen rock glacier (Austria). Paper presented at: Proceedings of the 7th International Permafrost Conference;1998.

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