Articles | Volume 10, issue 3
https://doi.org/10.5194/tc-10-1105-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/tc-10-1105-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Modeling debris-covered glaciers: response to steady debris deposition
Institute of Earth Sciences, University of Iceland, Askja,
Sturlugötu 7, 101 Reykjavìk, Iceland
Robert S. Anderson
Institute of Arctic
and Alpine Research, and Department of Geological Sciences, University of
Colorado, Campus Box 450, Boulder, Colorado, CO 80309, USA
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- Understanding the spatial distribution and plausible genesis of supraglacial debris over the Himalaya-Karakoram region M. Srigyan et al. 10.1080/02723646.2023.2202934
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- Meteorological impacts of a novel debris‐covered glacier category in a regional climate model across a Himalayan catchment E. Potter et al. 10.1002/asl.1018
- Evolution of the sparse debris cover during the ablation season at two small Alpine glaciers (Gran Zebrù and Sforzellina, Ortles-Cevedale group) G. Tarca & M. Guglielmin 10.1016/j.geomorph.2022.108268
- Understanding Complex Debris-Covered Glaciers: Concepts, Issues, and Research Directions D. Huo et al. 10.3389/feart.2021.652279
- Elevation Change Rates of Glaciers in the Lahaul-Spiti (Western Himalaya, India) during 2000–2012 and 2012–2013 S. Vijay & M. Braun 10.3390/rs8121038
- Estimation of the total sub-debris ablation from point-scale ablation data on a debris-covered glacier S. Shah et al. 10.1017/jog.2019.48
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- Impact of glacier loss and vegetation succession on annual basin runoff E. Carnahan et al. 10.5194/hess-23-1667-2019
- Contrasting Meteorological Drivers of the Glacier Mass Balance Between the Karakoram and Central Himalaya P. Bonekamp et al. 10.3389/feart.2019.00107
- Reversible glacial-periglacial transition in response to climate changes and paraglacial dynamics: A case study from Héðinsdalsjökull (northern Iceland) D. Palacios et al. 10.1016/j.geomorph.2021.107787
- Debris cover effect on the evolution of Northern Caucasus glaciers in the 21st century T. Postnikova et al. 10.3389/feart.2023.1256696
- The sustainability of water resources in High Mountain Asia in the context of recent and future glacier change A. Rowan et al. 10.1144/SP462.12
- An efficient representation of glacier dynamics in a semi-distributed hydrological model to bridge glacier and river catchment scales M. Wortmann et al. 10.1016/j.jhydrol.2019.03.006
- Early 21st century spatially detailed elevation changes of Jammu and Kashmir glaciers (Karakoram–Himalaya) S. Vijay & M. Braun 10.1016/j.gloplacha.2018.03.014
- Debris thickness patterns on debris-covered glaciers L. Anderson & R. Anderson 10.1016/j.geomorph.2018.03.014
- Ice cliff contribution to the tongue-wide ablation of Changri Nup Glacier, Nepal, central Himalaya F. Brun et al. 10.5194/tc-12-3439-2018
- Constraints on the timing of debris-covered and rock glaciers: An exploratory case study in the Hólar area, northern Iceland J. Fernández-Fernández et al. 10.1016/j.geomorph.2020.107196
- Brief communication: Thinning of debris-covered and debris-free glaciers in a warming climate A. Banerjee 10.5194/tc-11-133-2017
- Volume-area scaling for debris-covered glaciers A. Banerjee 10.1017/jog.2020.69
- Debris Cover Limits Subglacial Erosion and Promotes Till Accumulation I. Delaney & L. Anderson 10.1029/2022GL099049
- Modelling debris transport within glaciers by advection in a full-Stokes ice flow model A. Wirbel et al. 10.5194/tc-12-189-2018
- The sensitivity and evolutionary trajectory of the mountain cryosphere: Implications for mountain geomorphic systems and hazards J. Knight & S. Harrison 10.1002/ldr.4630
- Reversed Surface-Mass-Balance Gradients on Himalayan Debris-Covered Glaciers Inferred from Remote Sensing R. Bisset et al. 10.3390/rs12101563
- The origin and collapse of rock glaciers during the Bølling-Allerød interstadial: A new study case from the Cantabrian Mountains (Spain) J. Santos-González et al. 10.1016/j.geomorph.2022.108112
- Thickness estimation of supraglacial debris above ice cliff exposures using a high-resolution digital surface model derived from terrestrial photography L. NICHOLSON & J. MERTES 10.1017/jog.2017.68
- Glaciological and meteorological investigations of an Alpine debris-covered glacier: the case study of Amola Glacier (Italy) D. Fugazza et al. 10.1016/j.coldregions.2023.104008
- An integrated deep learning and object-based image analysis approach for mapping debris-covered glaciers D. Thomas et al. 10.3389/frsen.2023.1161530
- Object-based analysis of unmanned aerial vehicle imagery to map and characterise surface features on a debris-covered glacier P. Kraaijenbrink et al. 10.1016/j.rse.2016.09.013
- Stability of supraglacial debris P. Moore 10.1002/esp.4244
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Short summary
Mountains erode and shed rocks down slope. When these rocks (debris) fall on glacier ice they can suppress ice melt. By protecting glaciers from melt, debris can make glaciers extend to lower elevations. Using mathematical models of glaciers and debris deposition, we find that debris can more than double the length of glaciers. The amount of debris deposited on the glacier, which scales with mountain height and steepness, is the most important control on debris-covered glacier length and volume.
Mountains erode and shed rocks down slope. When these rocks (debris) fall on glacier ice they...