Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Marc Hugentobler"'
Publikováno v:
Journal of Geophysical Research: Earth Surface. 127
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40adf0a9042b1db6930f4f8ffac2b671
https://doi.org/10.1029/2021jf006484
https://doi.org/10.1029/2021jf006484
Publikováno v:
EGUsphere
In deglaciating environments, rock slopes are affected by stress perturbations driven by mechanical unloading due to ice downwasting and concurrent changes in thermal and hydraulic boundary conditions. Since in-situ data is rare, the different proces
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e37415b480475a0adc1c02e201fa9323
https://hdl.handle.net/20.500.11850/593652
https://hdl.handle.net/20.500.11850/593652
Publikováno v:
Journal of Geophysical Research: Earth Surface, 127 (4)
Rock slope failures often result from progressive rock mass damage which accumulates over long timescales. In deglaciating environments, rock slopes are affected by stress perturbations driven by mechanical unloading due to ice downwasting and concur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1e3fcde09c39acb504855af322bae4c5
Autor:
Nicolas Oestreicher, Simon Loew, Clément Roques, Jordan Balfour Aaron, Adriano Gualandi, Laurent Longuevergne, Philippe Limpach, Marc Hugentobler
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4378ff8c66e70b119649306b878b9455
https://doi.org/10.1002/essoar.10507494.1
https://doi.org/10.1002/essoar.10507494.1
Large rock slopes instabilities form over long timescales through progressive rock mass strength weakening of initially stable slopes. Progressive rock mass damage is driven by environmental loads and is thus strongly dependent on the local setting a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::647b835138844530b0895bf21a254ef7
https://doi.org/10.5194/egusphere-egu21-5192
https://doi.org/10.5194/egusphere-egu21-5192
Autor:
Philippe Limpach, L. Longuevergne, Marc Hugentobler, Clément Roques, Jordan Aaron, Simon Loew, Nicolas Oestreicher, Adriano Gualandi
Publikováno v:
Journal of Geophysical Research: Earth Surface
Journal of Geophysical Research: Earth Surface, American Geophysical Union/Wiley, In press, ⟨10.1029/2021jf006353⟩
Journal of Geophysical Research: Earth Surface, 2021, 126 (12), pp.e2021JF006353. ⟨10.1029/2021jf006353⟩
Journal of Geophysical Research: Earth Surface, 126 (12)
Journal of Geophysical Research: Earth Surface, American Geophysical Union/Wiley, In press, ⟨10.1029/2021jf006353⟩
Journal of Geophysical Research: Earth Surface, 2021, 126 (12), pp.e2021JF006353. ⟨10.1029/2021jf006353⟩
Journal of Geophysical Research: Earth Surface, 126 (12)
A comprehensive surface displacement monitoring system installed in the recently deglaciated bedrock slopes of the Aletsch Valley shows systematic reversible motions at the annual scale. We explore potential drivers for this deformation signal and de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d0a0510b9a5084af6951f13f3484a733
https://hal-insu.archives-ouvertes.fr/insu-03438936/file/2021JF006353.pdf
https://hal-insu.archives-ouvertes.fr/insu-03438936/file/2021JF006353.pdf
Publikováno v:
EGUsphere
Retreating glaciers around the world lead to rapid and profound changes in the surrounding landscapes. In the Alps, many glaciers are rapidly retreating and downwasting, substantially modifying stresses and hydro-thermal boundary conditions on the ad
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e81d5a961da4ffacc5c65ce50709ddda
https://hdl.handle.net/20.500.11850/510396
https://hdl.handle.net/20.500.11850/510396
Publikováno v:
Journal of Geophysical Research: Earth Surface, 126 (11)
In deglaciating environments, rock mass weakening and potential formation of rock slope instabilities is driven by long-term and seasonal changes in thermal- and hydraulic- boundary conditions, combined with unloading due to ice melting. However, in-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::520bc8d87ca8eaa1bcadd5da009bded7
Monitoring and Analysis of Landslide-Glacier Interactions at the Great Aletsch Glacier (Switzerland)
Valley glaciers have traditionally been expected to significantly influence the stability and movement rates of adjacent paraglacial landslides. However, detailed studies related to the mechanical and displacement interactions between glacier ice and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2dbad635833527ec1c34e8f23622ff69
https://doi.org/10.5194/egusphere-egu2020-13369
https://doi.org/10.5194/egusphere-egu2020-13369