Debris-covered glaciers are widespread in the mountain chains of Asia. They are also particularly common in New Zealand , in the Andes and in Alaska. Despite their relatively common occurrence, debris-covered glaciers have not been well studied. A debris cover that partially or completely masks the glacier ablation zone significantly influences the surface energy flux, the ablation rate and the discharge of meltwater streams. A multi-temporal analysis based on photogrammetry methodologies was used to assess changes volume and ablation rates.
Recent variations of a debris-covered glacier (Brenva glacier) in the Italian Alps monitored by comparison of maps and digital orthophotos / D'Agata, C; Smiraglia, C; Zanutta, A; Mancini, Francesco. - In: JOURNAL OF GLACIOLOGY. - ISSN 0022-1430. - STAMPA. - 51:172(2005), pp. 183-185. [10.3189/S0022143000215232]
Recent variations of a debris-covered glacier (Brenva glacier) in the Italian Alps monitored by comparison of maps and digital orthophotos
MANCINI, Francesco
2005
Abstract
Debris-covered glaciers are widespread in the mountain chains of Asia. They are also particularly common in New Zealand , in the Andes and in Alaska. Despite their relatively common occurrence, debris-covered glaciers have not been well studied. A debris cover that partially or completely masks the glacier ablation zone significantly influences the surface energy flux, the ablation rate and the discharge of meltwater streams. A multi-temporal analysis based on photogrammetry methodologies was used to assess changes volume and ablation rates.File | Dimensione | Formato | |
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