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Institute for Meteorology and Geophysics Innsbruck

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  • 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 of snow is measured by determination of the water equivalent in 6 snow pits, the ice ablation is measured with 15 stakes drilled into the ice. Results are the annual net mass balance in kg, the total accumulation and ablation, the glacier area and the portions of the area which are subject to ablation and accumulation, the elevation of the equilibrium line and the specific mass balance in kg/m? (= mm w.e.). The accumulation during the winter is determined by the 1 May. The project homepage is located at http://imgi.uibk.ac.at . The project is funded by the Hydrographischer Dienst der Abteilung Wasserwirtschaft des Amtes der Tiroler Landesregierung and National Park Hohe Tauern. The measurements are carried out by the Institute of Meteorology and Geophysics of the University of Innsbruck.

  • 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 of snow is measured by determination of the water equivalent in 6 snow pits, the ice ablation is measured with 15 stakes drilled into the ice. Results are the annual net mass balance in kg, the total accumulation and ablation, the glacier area and the portions of the area which are subject to ablation and accumulation, the elevation of the equilibrium line and the specific mass balance in kg/m? (= mm w.e.). The accumulation during the winter is determined by the 1 May. The project homepage is located at http://imgi.uibk.ac.at . The project is funded by the Hydrographischer Dienst der Abteilung Wasserwirtschaft des Amtes der Tiroler Landesregierung and National Park Hohe Tauern. The measurements are carried out by the Institute of Meteorology and Geophysics of the University of Innsbruck.

  • 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 of snow measured in about 6 pits for the mass balance year from 1 October to 30 September of the following year. The data comprises the glacier area, the net mass balance for the total glacier area as well as specified for the ablation and accumulation area, the altitude of the equilibrium line (ELA) and the specific mass balance.

  • 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 of snow measured in about 9 pits for the mass balance year from 1 October to 30 September of the following year. The data comprises the glacier area, the net mass balance for the total glacier area as well as specified for the ablation and accumulation area, the altitude of the equilibrium line (ELA) and the specific mass balance.

  • 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 of snow measured in about 6 pits for the mass balance year from 1 October to 30 September of the following year. The data comprises the glacier area, the net mass balance for the total glacier area as well as specified for the ablation and accumulation area, the altitude of the equilibrium line (ELA) and the specific mass balance.

  • 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 of snow measured in about 9 pits for the mass balance year from 1 October to 30 September of the following year. The data comprises the glacier area, the net mass balance for the total glacier area as well as specified for the ablation and accumulation area, the altitude of the equilibrium line (ELA) and the specific mass balance.

  • 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 10 to 20 stakes for the mass balance year from 1 October to 30 September of the following year. The data comprises the glacier area, the net mass balance for the total glacier area as well as specified for the ablation and accumulation area, the altitude of the equilibrium line (ELA) and the specific mass balance.

  • 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 10 to 20 stakes for the mass balance year from 1 October to 30 September of the following year. The data comprises the glacier area, the net mass balance for the total glacier area as well as specified for the ablation and accumulation area, the altitude of the equilibrium line (ELA) and the specific mass balance.

  • 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 accumulation of snow is measured by determination of the water equivalent in 6 snow pits, the ice ablation is measured with 15 stakes drilled into the ice. Results are the annual net mass balance in kg, the total accumulation and ablation, the glacier area and the portions of the area which are subject to ablation and accumulation, the elevation of the equilibrium line and the specific mass balance in kg/m? (= mm w.e.). The accumulation during the winter is determined by the 1 May. The project homepage is located at http://imgi.uibk.ac.at . The project is funded by the Amt der Oberoesterreichischen Landesregierung and the Energie AG. The measurements are carried out by the Institute of Meteorology and Geophysics of the University of Innsbruck and the company Blue Sky in Gmunden, Austria.

  • 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 accumulation of snow is measured by determination of the water equivalent in 6 snow pits, the ice ablation is measured with 15 stakes drilled into the ice. Results are the annual net mass balance in kg, the total accumulation and ablation, the glacier area and the portions of the area which are subject to ablation and accumulation, the elevation of the equilibrium line and the specific mass balance in kg/m2 (= mm w.e.). The accumulation during the winter is determined by the 1 May. The project homepage is located at http://imgi.uibk.ac.at . The project is funded by the Amt der Oberoesterreichischen Landesregierung and the Energie AG. The measurements are carried out by the Institute of Meteorology and Geophysics of the University of Innsbruck and the company Blue Sky in Gmunden, Austria.