1,116 research outputs found

    Elevation zones Venedigerkees, Hohe Tauern, Austria, 2021/2022

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    The Venedigerkees in the Hohe Tauern National Park is the easternmost tributary glacier to the former tongue of Obersulzbachkees. As a result of the strong retreat of Obersulzbachkees, the glacier disintegrated into several tributary glaciers, with a large lake remaining at the location of a famous serac zone, the 'Türkische Zeltstadt'. Hydrological monitoring of the area is done by the Hydrological Survey of the Federal Government of Salzburg (DI Hans Wiesenegger) who initiated the mass balance monitoring programme together with Heinz Slupetzky and the Institute of Interdisciplinary Mountain Research of the Austrian Academy of Sciences. The mass balance of the Venedigerkees is measured since 2011/12 with the direct or glaciological method

    Glacier mass balance Venedigerkees, Hohe Tauern, Austria, 2021/2022

    No full text
    The Venedigerkees in the Hohe Tauern National Park is the easternmost tributary glacier to the former tongue of Obersulzbachkees. As a result of the strong retreat of Obersulzbachkees, the glacier disintegrated into several tributary glaciers, with a large lake remaining at the location of a famous serac zone, the 'Türkische Zeltstadt'. Hydrological monitoring of the area is done by the Hydrological Survey of the Federal Government of Salzburg (DI Hans Wiesenegger) who initiated the mass balance monitoring programme together with Heinz Slupetzky and the Institute of Interdisciplinary Mountain Research of the Austrian Academy of Sciences. The mass balance of the Venedigerkees is measured since 2011/12 with the direct or glaciological method

    Glacier mass balance Venedigerkees, Hohe Tauern, Austria, 2015/2016

    No full text
    In the past three periods, 2014/2015, 2015/2016 and 2016/2017, in the extrapolation of mass balance to total glacier area, zones with b=0 mm w.e. have been defined. In the current analysis, these areas have been changed to ablation zones with the lowest possible ablation of -25 mm w.e., to maintain the records consistency. Therefore, small changes have been applied to the mass balance data of the three years 2014/2015, 2015/2016 and 2016/2017 so that older versions of the time series and reports can slightly deviate. Changes affect the altitude levels 2925 to 2975 for the period 2014/2015, 2975 to 3175 for the period 2015/2016 and 2875 to 2975 for 2016/17

    Elevation zones Venedigerkees, Hohe Tauern, Austria, 2015/2016

    No full text
    This corrected version was uploaded on 2018-02-15. In the past three periods, 2014/2015, 2015/2016 and 2016/2017, in the extrapolation of mass balance to total glacier area, zones with b=0 mm w.e. have been defined. In the current analysis, these areas have been changed to ablation zones with the lowest possible ablation of -25 mm w.e., to maintain the records consistency. Therefore, small changes have been applied to the mass balance data of the three years 2014/2015, 2015/2016 and 2016/2017 so that older versions of the time series and reports can slightly deviate. Changes affect the altitude levels 2925 to 2975 for the period 2014/2015, 2975 to 3175 for the period 2015/2016 and 2875 to 2975 for 2016/17

    Glacier mass balances and elevation zones of Venedigerkees, Hohe Tauern, Austria, 2011/2012 et seq

    No full text
    The Venedigerkees in the Hohe Tauern National Park is the easternmost tributary glacier to the former tongue of Obersulzbachkees. As a result of the strong retreat of Obersulzbachkees, the glacier disintegrated into several tributary glaciers, with a large lake remaining at the location of a famous serac zone, the 'Türkische Zeltstadt'. Hydrological monitoring of the area is done by the Hydrological Survey of the Federal Government of Salzburg (DI Hans Wiesenegger) who initiated the mass balance monitoring programme together with Heinz Slupetzky and the Institute of Interdisciplinary Mountain Research of the Austrian Academy of Sciences. The mass balance of the Venedigerkees is measured since 2011/12 with the direct or glaciological method. New data will be added every year
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