4.6 Article

Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates

Journal

CRYOSPHERE
Volume 15, Issue 1, Pages 265-282

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/tc-15-265-2021

Keywords

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Funding

  1. 2011 Muire Science and Learning Center Fellowship
  2. European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program [759639, 851614]
  3. NSF [DGE-1144083, EAR-1239281, EAR-1123855, OPP-1821002]
  4. University of Colorado at Boulder's Earth Lab initiative
  5. European Research Council (ERC) [851614, 759639] Funding Source: European Research Council (ERC)

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The study quantified the melt across the debris-covered tongue of Kennicott Glacier, revealing that ice cliffs contribute 26% of total melt across the glacier tongue. Despite the significant importance of ice cliffs to area-average melt, the absolute area-averaged melt is dominated by debris.
Many glaciers are thinning rapidly beneath meltreducing debris cover, including Kennicott Glacier in Alaska where glacier-wide maximum thinning also occurs under debris. This contradiction has been explained by melt hotspots, such as ice cliffs, scattered within the debris cover. However, melt hotspots alone cannot account for the rapid thinning at Kennicott Glacier. We consider the significance of ice cliffs, debris, and ice dynamics in addressing this outstanding problem. We collected abundant in situ measurements of debris thickness, sub-debris melt, and ice cliff backwasting, allowing for extrapolation across the debris-covered tongue (the study area and the lower 24.2 km(2) of the 387 km(2) glacier). A newly developed automatic ice cliff delineation method is the first to use only optical satellite imagery. The adaptive binary threshold method accurately estimates ice cliff coverage even where ice cliffs are small and debris color varies. Kennicott Glacier exhibits the highest fractional area of ice cliffs (11.7 %) documented to date. Ice cliffs contribute 26 % of total melt across the glacier tongue. Although the relative importance of ice cliffs to area-average melt is significant, the absolute area-averaged melt is dominated by debris. At Kennicott Glacier, glacier-wide melt rates are not maximized in the zone of maximum thinning Declining ice discharge through time therefore explains the rapid thinning There is more debris-covered ice in Alaska than in any other region on Earth. Through this study, Kennicott Glacier is the first glacier in Alaska, and the largest glacier globally, where melt across its debris-covered tongue has been rigorously quantified.

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