Results 11 to 20 of about 103 (97)
A Consistent Framework for Coupling Basal Friction With Subglacial Hydrology on Hard‐Bedded Glaciers [PDF]
Abstract Below hard‐bedded glaciers, both basal friction and distributed subglacial drainage are thought to be controlled by a network of cavities. Previous coupled hydro‐mechanical models, however, describe cavity‐driven friction and hydraulic transmissivity independently, resulting in a physically inconsistent cavity evolution between the two ...
Adrien Gilbert +4 more
wiley +2 more sources
Structural and functional responses of invertebrate communities to climate change and flow regulation in alpine catchments [PDF]
We explored the structural and functional effects of climate change in interaction with flow regulation by comparing data collected in the 1970s and 2010s in regulated and unregulated alpine catchments of France. Divergent structural but convergent functional responses were found between free‐flowing and regulated catchments. Although cold‐adapted taxa
Daniel Bruno +5 more
wiley +2 more sources
Repeating Low Frequency Icequakes in the Mont‐Blanc Massif Triggered by Snowfalls
Abstract Deformation mechanisms of glaciers are highly sensitive to basal temperature; the motion of temperate glaciers is dominated by basal slip while cold‐based glaciers deform mainly by internal creep. While basal slip is usually aseismic, unstable slip sometimes occurs and can be detected by seismometers.
Agnès Helmstetter
wiley +1 more source
Evidence of Seasonal Uplift in the Argentière Glacier (Mont Blanc Area, France)
Abstract The hydromechanical processes by which basal water controls sliding at the glacier bed are poorly known, despite glacier basal motion being responsible for a large part of ice flux in temperate alpine glaciers. Previous studies suggest that sliding strongly relates to the quantity of water being stored at the ice‐bedrock interface.
Christian Vincent +12 more
wiley +1 more source
Ice‐Dynamical Glacier Evolution Modeling—A Review
Abstract Glaciers play a crucial role in the Earth System: they are important water suppliers to lower‐lying areas during hot and dry periods, and they are major contributors to the observed present‐day sea‐level rise. Glaciers can also act as a source of natural hazards and have a major touristic value.
H. Zekollari +3 more
wiley +1 more source
Abstract Dense seismic array monitoring combined with advanced processing can help retrieve and locate a variety of seismic sources with unprecedented resolution and spatial coverage. We present a methodology that goes beyond classical localization algorithms through gathering various types of sources (impulsive or continuous) using a single scheme ...
Ugo Nanni +3 more
wiley +1 more source
Do Existing Theories Explain Seasonal to Multi‐Decadal Changes in Glacier Basal Sliding Speed?
Abstract Theoretical descriptions of ice‐bed friction beneath glaciers and ice sheets are key to predict changes in sea level. Applicability of these theories at the natural landscape scale and over long periods has however not been tested. Here we test hard bed friction laws by analyzing a unique data set of in‐situ basal sliding measurements ...
F. Gimbert +4 more
wiley +1 more source
Glacier flow and slope instabilities in Alpine mountain areas represent a hazard issue. Sentinel-1 satellites provide regular Synthetic Aperture Radar (SAR) acquisitions that are potentially useful to monitor these areas, but they can be affected by ...
Matthias Jauvin +5 more
doaj +1 more source
Angelo Maria Spinazzi argentiere nella Roma del Settecento: la committenza portoghese
Viene qui presa in esame l’attività dell’argentiere Angelo Maria Spinazzi (1693, dopo il 1785 / prima del 1789) nell’ambito della committenza portoghese, a partire dai primissimi anni Venti, subito dopo aver ottenuto la patente di argentiere, Spinazzi lavorò per l’ambasciata portoghese nella città pontificia e negli anni Quaranta fu coinvolto nell ...
openaire +2 more sources
The subglacial observatory beneath the Argentière glacier provides a rare opportunity to study the interactions between glacier sliding velocity and subglacial runoff.
CHRISTIAN VINCENT, LUC MOREAU
doaj +1 more source

