Articles | Volume 7, issue 1
https://doi.org/10.5194/esurf-7-301-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esurf-7-301-2019
© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Development of proglacial lakes and evaluation of related outburst susceptibility at the Adygine ice-debris complex, northern Tien Shan
Kristyna Falatkova
CORRESPONDING AUTHOR
Department of Physical Geography and Geoecology, Charles University,
128 43 Prague, Czech Republic
Miroslav Šobr
Department of Physical Geography and Geoecology, Charles University,
128 43 Prague, Czech Republic
Anton Neureiter
Department of Climate Research, Zentralanstalt für Meteorologie
und Geodynamik, 1190 Vienna, Austria
Wolfgang Schöner
Department of Geography and Regional Science, University of Graz,
8010 Graz, Austria
Bohumír Janský
Department of Physical Geography and Geoecology, Charles University,
128 43 Prague, Czech Republic
Hermann Häusler
Department of Environmental Geosciences, University of Vienna, 1090
Vienna, Austria
Zbyněk Engel
Department of Physical Geography and Geoecology, Charles University,
128 43 Prague, Czech Republic
Vojtěch Beneš
G IMPULS Praha spol. s r.o., 170 00 Prague, Czech Republic
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Cited
21 citations as recorded by crossref.
- Inventory and GLOF susceptibility of glacial lakes in Chenab basin, Western Himalaya S. Das et al. 10.1080/19475705.2024.2356216
- Estimating glacier-bed overdeepenings as possible sites of future lakes in the de-glaciating Mont Blanc massif (Western European Alps) F. Magnin et al. 10.1016/j.geomorph.2019.106913
- Gulf of Alaska ice-marginal lake area change over the Landsat record and potential physical controls H. Field et al. 10.5194/tc-15-3255-2021
- Glacier thinning, recession and advance, and the associated evolution of a glacial lake between 1966 and 2021 atAusterdalsbreen, westernNorway G. Seier et al. 10.1002/ldr.4923
- Why are glacial lakes in the eastern Tianshan Mountains expanding at an accelerated rate? Q. Zhang et al. 10.1007/s11442-023-2076-z
- Simulation of Freeze–Thaw and Melting of Buried Ice in Longbasaba Moraine Dam in the Central Himalayas Between 1959 and 2100 Using COMSOL Multiphysics J. Wang et al. 10.1029/2022JF006848
- A conceptual model for glacial lake bathymetric distribution T. Zhang et al. 10.5194/tc-17-5137-2023
- Glacier–permafrost relations in a high-mountain environment: 5 decades of kinematic monitoring at the Gruben site, Swiss Alps I. Gärtner-Roer et al. 10.5194/tc-16-2083-2022
- UAV-based geomorphological evolution of the Terminus Area of the Hailuogou Glacier, Southeastern Tibetan Plateau between 2017 and 2020 S. Xu et al. 10.1016/j.geomorph.2022.108293
- Rock glaciers as proxy for machine learning based debris‐covered glacier mapping of Kinnaur District, Himachal Pradesh I. Pradhan et al. 10.1002/esp.5888
- Hydrological characterization and connectivity of proglacial lakes to a stream, Adygine ice-debris complex, northern Tien Shan K. Falatkova et al. 10.1080/02626667.2020.1711913
- Climate change impacts and adaptation to permafrost change in High Mountain Asia: a comprehensive review P. Baral et al. 10.1088/1748-9326/acf1b4
- Controls on Alpine Lake Dynamics, Tien Shan, Central Asia Q. Zhang et al. 10.3390/rs14194698
- Potential threats of glacial lake changes to the Sichuan-Tibet Railway M. Peng et al. 10.1017/jog.2024.40
- Thinning and dynamics of the glacier terminus at the Pasterze Glacier (Austria), 2016–2021 G. Seier et al. 10.1016/j.coldregions.2024.104198
- Geomorphological Evolution of the Terminus Area of the Hailuogou Glacier, Southeastern Tibetan Plateau S. XU et al. 10.2139/ssrn.3987974
- Discriminating viscous-creep features (rock glaciers) in mountain permafrost from debris-covered glaciers – a commented test at the Gruben and Yerba Loca sites, Swiss Alps and Chilean Andes W. Haeberli et al. 10.5194/tc-18-1669-2024
- Susceptibility Analysis of Glacier Debris Flow by Investigating the Changes in Glaciers Based on Remote Sensing: A Case Study R. Lin et al. 10.3390/su13137196
- A robust glacial lake outburst susceptibility assessment approach validated by GLOF event in 2020 in the Nidu Zangbo Basin, Tibetan Plateau D. Zhang et al. 10.1016/j.catena.2022.106734
- An integrative method for identifying potentially dangerous glacial lakes in the Himalayas T. Zhang et al. 10.1016/j.scitotenv.2021.150442
- Development of a Potentially Hazardous Pro-Glacial Lake in Aksay Valley, Kyrgyz Range, Northern Tien Shan V. Zaginaev et al. 10.3390/hydrology6010003
20 citations as recorded by crossref.
- Inventory and GLOF susceptibility of glacial lakes in Chenab basin, Western Himalaya S. Das et al. 10.1080/19475705.2024.2356216
- Estimating glacier-bed overdeepenings as possible sites of future lakes in the de-glaciating Mont Blanc massif (Western European Alps) F. Magnin et al. 10.1016/j.geomorph.2019.106913
- Gulf of Alaska ice-marginal lake area change over the Landsat record and potential physical controls H. Field et al. 10.5194/tc-15-3255-2021
- Glacier thinning, recession and advance, and the associated evolution of a glacial lake between 1966 and 2021 atAusterdalsbreen, westernNorway G. Seier et al. 10.1002/ldr.4923
- Why are glacial lakes in the eastern Tianshan Mountains expanding at an accelerated rate? Q. Zhang et al. 10.1007/s11442-023-2076-z
- Simulation of Freeze–Thaw and Melting of Buried Ice in Longbasaba Moraine Dam in the Central Himalayas Between 1959 and 2100 Using COMSOL Multiphysics J. Wang et al. 10.1029/2022JF006848
- A conceptual model for glacial lake bathymetric distribution T. Zhang et al. 10.5194/tc-17-5137-2023
- Glacier–permafrost relations in a high-mountain environment: 5 decades of kinematic monitoring at the Gruben site, Swiss Alps I. Gärtner-Roer et al. 10.5194/tc-16-2083-2022
- UAV-based geomorphological evolution of the Terminus Area of the Hailuogou Glacier, Southeastern Tibetan Plateau between 2017 and 2020 S. Xu et al. 10.1016/j.geomorph.2022.108293
- Rock glaciers as proxy for machine learning based debris‐covered glacier mapping of Kinnaur District, Himachal Pradesh I. Pradhan et al. 10.1002/esp.5888
- Hydrological characterization and connectivity of proglacial lakes to a stream, Adygine ice-debris complex, northern Tien Shan K. Falatkova et al. 10.1080/02626667.2020.1711913
- Climate change impacts and adaptation to permafrost change in High Mountain Asia: a comprehensive review P. Baral et al. 10.1088/1748-9326/acf1b4
- Controls on Alpine Lake Dynamics, Tien Shan, Central Asia Q. Zhang et al. 10.3390/rs14194698
- Potential threats of glacial lake changes to the Sichuan-Tibet Railway M. Peng et al. 10.1017/jog.2024.40
- Thinning and dynamics of the glacier terminus at the Pasterze Glacier (Austria), 2016–2021 G. Seier et al. 10.1016/j.coldregions.2024.104198
- Geomorphological Evolution of the Terminus Area of the Hailuogou Glacier, Southeastern Tibetan Plateau S. XU et al. 10.2139/ssrn.3987974
- Discriminating viscous-creep features (rock glaciers) in mountain permafrost from debris-covered glaciers – a commented test at the Gruben and Yerba Loca sites, Swiss Alps and Chilean Andes W. Haeberli et al. 10.5194/tc-18-1669-2024
- Susceptibility Analysis of Glacier Debris Flow by Investigating the Changes in Glaciers Based on Remote Sensing: A Case Study R. Lin et al. 10.3390/su13137196
- A robust glacial lake outburst susceptibility assessment approach validated by GLOF event in 2020 in the Nidu Zangbo Basin, Tibetan Plateau D. Zhang et al. 10.1016/j.catena.2022.106734
- An integrative method for identifying potentially dangerous glacial lakes in the Himalayas T. Zhang et al. 10.1016/j.scitotenv.2021.150442
Latest update: 20 Nov 2024
Short summary
In the last 50 years the Adygine glacier has been subject to relatively fast recession comparable to other glaciers in Tien Shan. As a consequence, a three-level cascade of glacial lakes formed, two of which were categorised as having medium outburst susceptibility. By 2050, the glacier is expected to have shrunk to 56–73 % of its 2012 extent. Further development of the site will result in formation of new lakes and probably also increase of outburst susceptibility due to permafrost degradation.
In the last 50 years the Adygine glacier has been subject to relatively fast recession...