TY - JOUR
T1 - Suivi de l’évolution de la couverture détritique d’un glacier noir par photo-comparaison: Le glacier d’Estelette, Massif du Mont Blanc
AU - Mazuie, Romain
AU - Deline, Philip
AU - Kirkbride, Martin P.
N1 - dc.title.alternative: Survey of the evolution of a debris-covered glacier by comparison of photographs: Glacier D'Estelette (Mont Blanc Massif)
dc.ispartof: Collection EDYTEM;
Cahiers de Géographie;
PY - 2009
Y1 - 2009
N2 - As part of a research programme into the controls on the evolution of the supraglacial debris cover of Glacier d’Estelette, a study of debris cover extent has been conducted over two timescales, decennal and annual. By comparison of aerial photographs, a reduction (1952 - 1993) then extension (1993 - 2006) of the debris cover could be correlated with contemporary phases of glacier advance then retreat. Its proportion of the 2/3 glacier surface area has oscillated between 31.1% and 52.2%. A comparison of oblique terrestrial photographs has confirmed the increase of debris covered glacier which characterised the last half-century, with an increase of debris cover between 2006 and 2007. These results confirm that the climatic signal recorded by the glacier’s dynamic response is the principal control on the extent of the debris cover, via the intensity of ablation and the glacier velocity.
AB - As part of a research programme into the controls on the evolution of the supraglacial debris cover of Glacier d’Estelette, a study of debris cover extent has been conducted over two timescales, decennal and annual. By comparison of aerial photographs, a reduction (1952 - 1993) then extension (1993 - 2006) of the debris cover could be correlated with contemporary phases of glacier advance then retreat. Its proportion of the 2/3 glacier surface area has oscillated between 31.1% and 52.2%. A comparison of oblique terrestrial photographs has confirmed the increase of debris covered glacier which characterised the last half-century, with an increase of debris cover between 2006 and 2007. These results confirm that the climatic signal recorded by the glacier’s dynamic response is the principal control on the extent of the debris cover, via the intensity of ablation and the glacier velocity.
KW - Present-day
KW - Debris-covered glacier
KW - Comparison of photographs
KW - Mont Blanc Massif
M3 - Article
SN - 1762-4304
SP - 171
EP - 178
JO - Neige et Glace de Montagne: Reconstitution, Dynamique, Pratiques
JF - Neige et Glace de Montagne: Reconstitution, Dynamique, Pratiques
IS - 8
ER -