Short-term geomorphological evolution of proglacial systems

JL Carrivick, T Heckmann - Geomorphology, 2017 - Elsevier
Proglacial systems are amongst the most rapidly changing landscapes on Earth, as glacier
mass loss, permafrost degradation and more episodes of intense rainfall progress with …

Rock glaciers as a water resource in a changing climate in the semiarid Chilean Andes

N Schaffer, S MacDonell, M Réveillet, E Yáñez… - Regional Environmental …, 2019 - Springer
Rock glaciers likely play an important hydrological role in the semiarid Andes (SA; 27°–35°
S). They supplement streamflow when water is needed most, especially during dry years in …

Impact of mountain permafrost on flow path and runoff response in a high alpine catchment

M Rogger, GB Chirico, H Hausmann… - Water Resources …, 2017 - Wiley Online Library
Permafrost in high alpine catchments is expected to disappear in future warmer climates, but
the hydrological impact of such changes is poorly understood. This paper investigates the …

Pluri-decadal (1955–2014) evolution of glacier–rock glacier transitional landforms in the central Andes of Chile (30–33 S)

S Monnier, C Kinnard - Earth Surface Dynamics, 2017 - esurf.copernicus.org
Three glacier–rock glacier transitional landforms in the central Andes of Chile are
investigated over the last decades in order to highlight and question the significance of their …

Occurrence, evolution and ice content of ice‐debris complexes in the Ak‐Shiirak, Central Tien Shan revealed by geophysical and remotely‐sensed investigations

T Bolch, N Rohrbach, S Kutuzov… - Earth Surface …, 2019 - Wiley Online Library
Rock glaciers and large ice‐debris complexes are common in many mountain ranges and
are especially prominent in semi‐arid mountains such as the Andes or the Tien Shan. These …

Internal structure and composition of a rock glacier in the Andes (upper Choapa valley, Chile) using borehole information and ground-penetrating radar

S Monnier, C Kinnard - Annals of Glaciology, 2013 - cambridge.org
This study uses boreholes, ground temperature monitoring and ground-penetrating radar
(GPR) in order to understand the internal structure and composition of a rock glacier in the …

Current transition from glacial to periglacial processes in the Dolomites (South-Eastern Alps)

R Seppi, T Zanoner, A Carton, A Bondesan… - Geomorphology, 2015 - Elsevier
A close relationship between glacial and periglacial landforms is frequently observed in
alpine environments, where a transition from glacial to periglacial processes often took …

Post‐glacial dynamics of an alpine Little Ice Age glacitectonized frozen landform (Aget, western Swiss Alps)

J Wee, R Delaloye - Permafrost and Periglacial Processes, 2022 - Wiley Online Library
Glaciers and frozen‐debris landforms have coexisted and episodically or continuously
interacted throughout the Holocene at elevations where the climate conditions are cold …

[HTML][HTML] An inventory-driven rock glacier status model (intact vs. relict) for South Tyrol, Eastern Italian Alps

C Kofler, S Steger, V Mair, M Zebisch, F Comiti… - Geomorphology, 2020 - Elsevier
Ice presence in rock glaciers is a topic that is likely to gain importance in the future due to the
expected decrease in water supply from glaciers and the increase of mass movements …

[PDF][PDF] 1.5. 5. Ground Penetrating Radar

M Robinson, C Bristow, J McKinley… - Geomorphological …, 2013 - academia.edu
Ground-penetrating radar (GPR) is an effective tool to visualise the structure of the shallow
subsurface. The purpose of this article is to offer guidelines to non-specialist GPR users on …