Articles | Volume 16, issue 11
The Cryosphere, 16, 4701–4725, 2022
https://doi.org/10.5194/tc-16-4701-2022
The Cryosphere, 16, 4701–4725, 2022
https://doi.org/10.5194/tc-16-4701-2022
Research article
11 Nov 2022
Research article | 11 Nov 2022

Sub-seasonal variability of supraglacial ice cliff melt rates and associated processes from time-lapse photogrammetry

Marin Kneib et al.

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Cited articles

Anderson, L. S., Armstrong, W. H., Anderson, R. S., and Buri, P.: Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates, The Cryosphere, 15, 265–282, https://doi.org/10.5194/tc-15-265-2021, 2021. 
Armstrong, L., Lacelle, D., Fraser, R. H., Kokelj, S., and Knudby, A.: Thaw slump activity measured using stationary cameras in time-lapse and Structure-from-Motion photogrammetry, Antarct. Sci., 4, 827–845, https://doi.org/10.1139/as-2018-0016, 2018. 
Bartlett, O. T., Ng, F. S. L., and Rowan, A. V.: Morphology and evolution of supraglacial hummocks on debris-covered Himalayan glaciers, Earth Surf. Proc. Land., 46, esp.5043, https://doi.org/10.1002/esp.5043, 2020. 
Beyer, R. A., Alexandrov, O., and McMichael, S.: The Ames Stereo Pipeline: NASA's Open Source Software for Deriving and Processing Terrain Data, Earth Sp. Sci., 5, 537–548, https://doi.org/10.1029/2018EA000409, 2018. 
Bonekamp, P. N. J., van Heerwaarden, C. C., Steiner, J. F., and Immerzeel, W. W.: Using 3D turbulence-resolving simulations to understand the impact of surface properties on the energy balance of a debris-covered glacier, The Cryosphere, 14, 1611–1632, https://doi.org/10.5194/tc-14-1611-2020, 2020. 
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Short summary
Ice cliffs are believed to be important contributors to the melt of debris-covered glaciers, but this has rarely been quantified as the cliffs can disappear or rapidly expand within a few weeks. We used photogrammetry techniques to quantify the weekly evolution and melt of four cliffs. We found that their behaviour and melt during the monsoon is strongly controlled by supraglacial debris, streams and ponds, thus providing valuable insights on the melt and evolution of debris-covered glaciers.