Ice-volume changes of selected glaciers in the Swiss Alps since the end of the 19th century

• Published in: Annals of glaciology Vol. 46; pp. 145 - 149
• Main Authors: Bauder, Andreas, Funk, Martin, Huss, Matthias
• Format: Journal Article
• Language: English
• Published: 2007
• ISSN: 0260-3055; 1727-5644
• DOI: 10.3189/172756407782871701

Abstract The evolution of surface topography of glaciers in the Swiss Alps is well documented with high-resolution aerial photographs repeatedly recorded since the 1960s and further back in time with topographic maps including elevation contour lines first surveyed in the mid-19th century. In order to quantify and interpret glacier changes in the Swiss Alps, time series of volume changes over the last 100–150 years have been collected. The available datasets provide a detailed spatial resolution for the retreat period since the end of the Little Ice Age. The spatial distribution as well as temporal variations of the thickness change were analyzed. A significant ice loss since the end of the 19th century was observed in the ablation area, while the changes in the accumulation area were small. We found moderate negative secular rates until the 1960s, followed by steady to positive rates for about two decades and strong ice loss starting in the 1980s which has lasted until the present. An evaluation of 19 glaciers revealed a total ice volume loss of about 13km 3 since the 1870s, of which 8.7 km 3 occurred since the 1920s and 3.5 km 3 since 1980. Decadal mean net balance rates for the periods 1920–60, 1960–80 and 1980–present are –0.29, –0.03 and –0.53ma –1 w.e., respectively.