par Lorrain, Reginald ;Haeberli, Wilfried
Référence Annals of glaciology, 14, page (168-171)
Publication Publié, 1990
Référence Annals of glaciology, 14, page (168-171)
Publication Publié, 1990
Article révisé par les pairs
Résumé : | For the first time, a cold ice cover of a summit in the central Swiss Alps has been sampled from the surface to the bed for determining its isotopic composition in δD and δ18O. Results of the analyses show a striking decrease of δ-values with depth. The δ-value differences are greater than those explicable by a direct temperature effect, but a substantial increase in melt water percolation through the firn since the formation of the deepest ice layer may explain the situation of this high-altitude ice. -Authors |