Resolution capacity of geophysical monitoring regarding permafrost degradation induced by hydrological processes
Geophysical methods are often used to characterize and monitor the subsurface composition of permafrost. The resolution capacity of standard methods, i.e. electrical resistivity tomography and refraction seismic tomography, depends not only on static parameters such as measurement geometry, but a...
Main Authors: | B. Mewes, C. Hilbich, R. Delaloye, C. Hauck |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2017-12-01
|
Series: | The Cryosphere |
Online Access: | https://www.the-cryosphere.net/11/2957/2017/tc-11-2957-2017.pdf |
Similar Items
-
Rapid warming and degradation of mountain permafrost in Norway and Iceland
by: B. Etzelmüller, et al.
Published: (2023-12-01) -
Towards accurate quantification of ice content in permafrost of the Central Andes – Part 1: Geophysics-based estimates from three different regions
by: C. Hilbich, et al.
Published: (2022-05-01) -
Coupled thermo–geophysical inversion for permafrost monitoring
by: S. Tomaškovičová, et al.
Published: (2024-01-01) -
Identifying mountain permafrost degradation by repeating historical electrical resistivity tomography (ERT) measurements
by: J. Buckel, et al.
Published: (2023-07-01) -
Challenges of Hydrological Engineering Design in Degrading Permafrost Environment of Russia
by: Olga Makarieva, et al.
Published: (2022-04-01)