Add to ORKGThe temperature regime of alpine permafrost is altered by the generally warmer atmospheric temperatures of recent decades. Eight boreholes, with depths between 100 and 130 m, have recently been drilled in European mountain permafrost as part of the Permafrost and Climate in Europe (PACE) project. They have been equipped with temperature sensors in order to better understand and quantify the effect of climate change on permafrost temperatures. Their interpretation with respect to signals of surface temperature histories is complicated by topographic effects. An apparent warming signal is present in all of the PACE boreholes but quantification of this effect in mountainous terrain remains difficult. The influence of topography and spatially-v...
The steep rockwalls of the Mont Blanc massif have been affected by an increase in rockfall activity ...
International audienceThe alpine permafrost has traditionally been thought as a geosystem mainly sen...
Recent ground temperature records from the 100-m-deep borehole near the Tarfala Research Station in ...
The temperature regime of alpine permafrost is altered by the generally warmer atmospheric temperatu...
The temperature regime of alpine permafrost is altered by the generally warmer atmospheric temperatu...
Here we present the first systematic measurements of European mountain permafrost temperatures from ...
Here we present a review of recent ground thermal data derived largely from the continent-scale netw...
The consequences of climate change are clearly visible in the Swiss Alps. In the past decades, incre...
In high mountain areas, permafrost is important because it influences the occurrence of natural haza...
Permafrost in the Alps occurs within three main landforms - rock glaciers, debris slopes and steep b...
In the Swiss Alps, permafrost occurs discontinuously and commonly has a temperature close to 0 °C. A...
Compared to lowland (polar) regions, permafrost in high mountain areas occurs in a large variety of ...
International audiencePermafrost and related thermo-hydro-mechanical processes are thought to influe...
The steep rockwalls of the Mont Blanc massif have been affected by an increase in rockfall activity ...
International audienceThe alpine permafrost has traditionally been thought as a geosystem mainly sen...
Recent ground temperature records from the 100-m-deep borehole near the Tarfala Research Station in ...
The temperature regime of alpine permafrost is altered by the generally warmer atmospheric temperatu...
The temperature regime of alpine permafrost is altered by the generally warmer atmospheric temperatu...
Here we present the first systematic measurements of European mountain permafrost temperatures from ...
Here we present a review of recent ground thermal data derived largely from the continent-scale netw...
The consequences of climate change are clearly visible in the Swiss Alps. In the past decades, incre...
In high mountain areas, permafrost is important because it influences the occurrence of natural haza...
Permafrost in the Alps occurs within three main landforms - rock glaciers, debris slopes and steep b...
In the Swiss Alps, permafrost occurs discontinuously and commonly has a temperature close to 0 °C. A...
Compared to lowland (polar) regions, permafrost in high mountain areas occurs in a large variety of ...
International audiencePermafrost and related thermo-hydro-mechanical processes are thought to influe...
The steep rockwalls of the Mont Blanc massif have been affected by an increase in rockfall activity ...
International audienceThe alpine permafrost has traditionally been thought as a geosystem mainly sen...
Recent ground temperature records from the 100-m-deep borehole near the Tarfala Research Station in ...