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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 2
The Cryosphere, 11, 723–739, 2017
https://doi.org/10.5194/tc-11-723-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 11, 723–739, 2017
https://doi.org/10.5194/tc-11-723-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Mar 2017

Research article | 21 Mar 2017

Surge dynamics and lake outbursts of Kyagar Glacier, Karakoram

Vanessa Round et al.

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Barrand, N. E. and Murray, T.: Multivariate Controls on the Incidence of Glacier Surging in the Karakoram Himalaya, Arct. Antarct. Alp. Res., 38, 489–498, 2006.
Björnsson, H.: Hydrological characteristics of the drainage system beneath a surging glacier, Nature, 395, 771–774, 1998.
Björnsson, H.: Understanding jokulhlaups; from the tale to theory, J. Glaciol., 56, 1002–1010, 2010.
Björnsson, H., Pálsson, F., Sigurdsson, O., and Flowers, G. E.: Surges of glaciers in Iceland, Ann. Glaciol., 36, 82–90, 2003.
Boulton, G. S. and Jones, A. S.: Stability of temperate ice caps and ice sheets resting on beds of deformable sediment, J. Glaciol., 24, 29–43, 1979.
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Short summary
Recent surging of Kyagar Glacier (Karakoram) caused a hazardous ice-dammed lake to form and burst in 2015 and 2016. We use remotely sensed glacier surface velocities and surface elevation to observe dramatic changes in speed and mass distribution during the surge. The surge was hydrologically controlled with rapid summer onset and dramatic termination following lake outburst. Since the surge, the potential outburst hazard has remained high, and continued remote monitoring is crucial.
Recent surging of Kyagar Glacier (Karakoram) caused a hazardous ice-dammed lake to form and...
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