Very small glaciers (area <0.1 km2) have received increased scientific attention during recent years, both for their rapid responses to the climate forcing and because they are characterized by microclimatic conditions, often marginal to glacier formation. They are particularly sensitive to climate changes and characterized by a great mass turnover, particularly evident in maritime areas with high precipitation. Here we consider the evolution from 1920 of the ‘Canin Eastern Glacier’ (Italian Southeastern Alps) in order to correlate its evolution to the precipitation–temperature trends. We reconstructed a precipitation–temperature record at the altitude of the glacier, filling a lack of knowledge in this alpine sector. We observed a de...
To improve current understanding of ongoing deglaciation dynamics in relation to climatic forcing, i...
none3noThe variability of glacier response to atmospheric temperature rise in different topo-climati...
International audienceThe causes and timing of the Little Ice Age (fifteenth to nineteenth centuries...
Very small glaciers (area <0.1 km2) have received increased scientific attention during recent years...
Very small glaciers (area \u3c0.1 km2) have received increased scientific attention during recent ye...
Very small glaciers (<0.5 km2) account for more than 80% of the total number of glaciers and more...
In order to assess the climate-glacier relationship in the Southern European Alps, two small glacier...
We analyze a daily series of rainfall, snowfall, air temperature, and snow water equivalent at fixed...
We analyze a daily series of rainfall, snowfall, air temperature, and snow water equivalent at fixed...
Small, debris-covered and avalanche-fed glaciers are widespread in high-relief areas of the world. H...
The recent evolution of a representative subset of Alpine glaciers (i.e. 43 glaciers located in the ...
This paper describes the recent evolution of Italian glaciers through an analysis of all available...
In the southernmost tract of the Alps (Italian-French Maritime Alps), extensively covered by glacier...
Very small glaciers (<0.5 km2) account for more than 80% of the total number of glaciers and more th...
To improve current understanding of ongoing deglaciation dynamics in relation to climatic forcing, i...
none3noThe variability of glacier response to atmospheric temperature rise in different topo-climati...
International audienceThe causes and timing of the Little Ice Age (fifteenth to nineteenth centuries...
Very small glaciers (area <0.1 km2) have received increased scientific attention during recent years...
Very small glaciers (area \u3c0.1 km2) have received increased scientific attention during recent ye...
Very small glaciers (<0.5 km2) account for more than 80% of the total number of glaciers and more...
In order to assess the climate-glacier relationship in the Southern European Alps, two small glacier...
We analyze a daily series of rainfall, snowfall, air temperature, and snow water equivalent at fixed...
We analyze a daily series of rainfall, snowfall, air temperature, and snow water equivalent at fixed...
Small, debris-covered and avalanche-fed glaciers are widespread in high-relief areas of the world. H...
The recent evolution of a representative subset of Alpine glaciers (i.e. 43 glaciers located in the ...
This paper describes the recent evolution of Italian glaciers through an analysis of all available...
In the southernmost tract of the Alps (Italian-French Maritime Alps), extensively covered by glacier...
Very small glaciers (<0.5 km2) account for more than 80% of the total number of glaciers and more th...
To improve current understanding of ongoing deglaciation dynamics in relation to climatic forcing, i...
none3noThe variability of glacier response to atmospheric temperature rise in different topo-climati...
International audienceThe causes and timing of the Little Ice Age (fifteenth to nineteenth centuries...