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Volume 9, issue 6
The Cryosphere, 9, 2201–2214, 2015
https://doi.org/10.5194/tc-9-2201-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 9, 2201–2214, 2015
https://doi.org/10.5194/tc-9-2201-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 26 Nov 2015

Research article | 26 Nov 2015

Revealing glacier flow and surge dynamics from animated satellite image sequences: examples from the Karakoram

F. Paul
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Cited articles  
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.
Baumann, S., Winkler, S., and Andreassen, L. M.: Mapping glaciers in Jotunheimen, South-Norway, during the "Little Ice Age" maximum, The Cryosphere, 3, 231–243, https://doi.org/10.5194/tc-3-231-2009, 2009.
Belò, M., Mayer, C., Smiraglia, C., and Tamburini, A.: The recent evolution of Liligo glacier, Karakoram, Pakistan, and its present quiescent phase, Ann. Glaciol., 48, 171–176, 2008.
Bhambri, R., Bolch, T., Kawishwar, P., Dobhal, D. P., Srivastava, D., and Pratap, B.: Heterogeneity in glacier response in the upper Shyok valley, northeast Karakoram, The Cryosphere, 7, 1385–1398, https://doi.org/10.5194/tc-7-1385-2013, 2013.
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This study uses animations of freely available Landsat images (acquired over 25 years) to reveal glacier flow and surge dynamics in the central Karakoram. The animations provide a holistic view on the timing and variability of glacier dynamics that is hard to obtain by other more quantitative methods. Among others, the study reveals that most surging glaciers are comparably small, steep and debris-free, with a wide range of advance rates and durations, overlapping with non-surge-type glaciers.
This study uses animations of freely available Landsat images (acquired over 25 years) to reveal...
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