Estimating Non‐Conductive Heat Flow Leading to Intra‐Permafrost Talik Formation at the Ritigraben Rock Glacier (Western Swiss Alps)
Although non‐conductive heat flow plays an important role in the evolution of rock glacier temperature and dynamics, few studies have quantified it. At the Ritigraben rock glacier (Switzerland), intra‐permafrost talik formation was observed at around 12 m depth and related to snowmelt and rainfall i...
Published in: | Permafrost and Periglacial Processes |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Subjects: | |
Online Access: | https://doi.org/10.1002/ppp.1911 |