Tape downloads not available.Due to issues with our tape backend tape downloads are not available. We are working on a solution.
Database maintenance from 23-Oct-2024 to 30-Oct-2024From 23-Oct-2024 8:00 CEST to 30-Oct-2024 18:00 CEST we will migrate the WDCC database to a new server. During this time metadata input using the metaXA and citeXA applications and DOI registrations will not be available. Data download will still be possible but no new user accounts can be created during the maintenance.
Glaciers are the most visible indicators of global change. Mass balance data allow the calculation of the past and current contributions of land ice to the sea level change. Additionally, glaciological
The annual glacier mass balance of Hallstaetter Gletscher in Hohe Tauern is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year).
The annual glacier mass balance of Hintereisferner in the Oetztal Alps is measured since 1.10.1952 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year).
The annual glacier mass balance of Jamtalferner in Silvretta is measured since 1.10.1989 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year). The accumulation
The annual glacier mass balance of Kesselwandferner in the Oetztal Alps is measured since 1.10.1952 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year).
The annual glacier mass balance of Mullwitzkees in Hohe Tauern is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year). The accumulation
The annual glacier mass balance of Hallstaetter Glacier in Dachstein area is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year).
The data represent annual values of the glacier mass balance measured with the direct glaciological method. The mass balance is calculated from ablation of ice measured at about 50 stakes and accumulation
The data represent annual values of the glacier mass balance measured with the direct glaciological method. The mass balance is calculated from ablation of ice measured at about 20 stakes and accumulation
The data represent annual values of the glacier mass balance measured with the direct glaciological method. The mass balance is calculated from ablation of ice and accumulation of snow measured at about
The annual glacier mass balance of Mullwitzkees in Hohe Tauern is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year). The accumulation
The annual glacier mass balance of Hallstaetter Glacier in Dachstein area is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year).
The data represent annual values of the glacier mass balance measured with the direct glaciological method. The mass balance is calculated from ablation of ice measured at about 20 stakes and accumulation
The data represent annual values of the glacier mass balance measured with the direct glaciological method. The mass balance is calculated from ablation of ice and accumulation of snow measured at about
The annual glacier mass balance of Mullwitzkees in Hohe Tauern is measured since 1.10.2006 with the direct glaciological method in the fixed date system (1.10. to 30. 09. of the following year). The accumulation