Zobrazeno 1 - 10
of 124
pro vyhledávání: '"M. Krautblatter"'
Publikováno v:
Earth Surface Dynamics, Vol 12, Pp 1027-1048 (2024)
The anticipation of massive rock slope failures is a key mitigation strategy in a changing climate and environment requiring a precise understanding of pre-failure process dynamics. Here we exploit >4 years of multi-method high-resolution monitoring
Externí odkaz:
https://doaj.org/article/29a8922a7a944be7bef345acad0df5b2
Publikováno v:
Earth Surface Dynamics, Vol 12, Pp 249-269 (2024)
Massive sediment pulses in catchments are a key alpine multi-risk component. Substantial sediment redistribution in alpine catchments frequently causes flooding, river erosion, and landsliding and affects infrastructure such as dam reservoirs as well
Externí odkaz:
https://doaj.org/article/3206e9f245b94e469b92b4ba5cd0d6b0
Publikováno v:
Earth Surface Dynamics, Vol 10, Pp 1185-1193 (2022)
Rockslides and rock avalanches are amongst the most destructive natural hazards in the alpine environment. The Flims rockslide is the largest known rock-slope failure in the Alps, which provides excellent outcrops and has fascinated researchers since
Externí odkaz:
https://doaj.org/article/4b328aca9fe848428c0f1040c151ad69
Autor:
S. P. Pudasaini, M. Krautblatter
Publikováno v:
Earth Surface Dynamics, Vol 10, Pp 165-189 (2022)
Proper knowledge of velocity is required in accurately determining the enormous destructive energy carried by a landslide. We present the first, simple and physics-based general analytical landslide velocity model that simultaneously incorporates the
Externí odkaz:
https://doaj.org/article/0e29426116ed4bea82c842c35013da20
Autor:
B. Etzelmüller, J. Czekirda, F. Magnin, P.-A. Duvillard, L. Ravanel, E. Malet, A. Aspaas, L. Kristensen, I. Skrede, G. D. Majala, B. Jacobs, J. Leinauer, C. Hauck, C. Hilbich, M. Böhme, R. Hermanns, H. Ø. Eriksen, T. R. Lauknes, M. Krautblatter, S. Westermann
Publikováno v:
Earth Surface Dynamics, Vol 10, Pp 97-129 (2022)
The warming and subsequent degradation of mountain permafrost within alpine areas represent an important process influencing the stability of steep slopes and rock faces. The unstable and monitored slopes of Mannen (Møre and Romsdal county, southern
Externí odkaz:
https://doaj.org/article/a9e052c18d1a46b7878e9673c31b3c1f
Publikováno v:
Earth Surface Dynamics, Vol 9, Pp 1481-1503 (2021)
The frequency of debris flows is hypothesized to have increased in recent decades with enhanced rainstorm activity. Geological evidence to test the relationship between climate and debris flow activity for prehistoric times is scarce due to incomplet
Externí odkaz:
https://doaj.org/article/80cc8c7c6b8d49ce96a0346fd82a2f99
Publikováno v:
Natural Hazards and Earth System Sciences, Vol 21, Pp 2753-2772 (2021)
While optical remote sensing has demonstrated its capabilities for landslide detection and monitoring, spatial and temporal demands for landslide early warning systems (LEWSs) had not been met until recently. We introduce a novel conceptual approach
Externí odkaz:
https://doaj.org/article/57a561ddfb804211bb0049c725a76259
A temperature-dependent mechanical model to assess the stability of degrading permafrost rock slopes
Publikováno v:
Earth Surface Dynamics, Vol 9, Pp 1125-1151 (2021)
Over the last 2 decades, permafrost degradation has been observed to be a major driver of enhanced rock slope instability and associated hazards in high mountains. While the thermal regime of permafrost degradation in high mountains has been addresse
Externí odkaz:
https://doaj.org/article/8774097d3fc54b98a64af98dddaf909a
Publikováno v:
Earth Surface Dynamics, Vol 8, Pp 729-751 (2020)
In the European Alps, almost half the glacier volume has disappeared over the past 150 years. The loss is reflected in glacier retreat and ice surface lowering even at high altitude. In steep glacial cirques, surface lowering exposes rock to atmosphe
Externí odkaz:
https://doaj.org/article/ce026f2a6b494249ab47677f655fb58e
Autor:
I. Hartmeyer, M. Keuschnig, R. Delleske, M. Krautblatter, A. Lang, L. Schrott, G. Prasicek, J.-C. Otto
Publikováno v:
Earth Surface Dynamics, Vol 8, Pp 753-768 (2020)
Cirque erosion contributes significantly to mountain denudation and is a key element of glaciated mountain topography. Despite long-standing efforts, rates of rockwall retreat and the proportional contributions of low-, mid- and high-magnitude rockfa
Externí odkaz:
https://doaj.org/article/af9856f42a2740dabbe14d98d872c473