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

<p>Many glaciers are thinning rapidly beneath melt-reducing 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,...

Full description

Bibliographic Details
Main Authors: L. S. Anderson, W. H. Armstrong, R. S. Anderson, P. Buri
Format: Article
Language:English
Published: Copernicus Publications 2021-01-01
Series:The Cryosphere
Online Access:https://tc.copernicus.org/articles/15/265/2021/tc-15-265-2021.pdf
id doaj-57a08802df7743678bab513ead42c7ba
record_format Article
spelling doaj-57a08802df7743678bab513ead42c7ba2021-01-19T12:49:10ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242021-01-011526528210.5194/tc-15-265-2021Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimatesL. S. Anderson0L. S. Anderson1W. H. Armstrong2W. H. Armstrong3R. S. Anderson4P. Buri5Department of Geological Sciences and Institute of Arctic and Alpine Research, University of Colorado Campus Box 450, Boulder, CO 80309-0450, USAGFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyDepartment of Geological Sciences and Institute of Arctic and Alpine Research, University of Colorado Campus Box 450, Boulder, CO 80309-0450, USADepartment of Geological and Environmental Sciences, Appalachian State University, 033 Rankin Science West, ASU Box 32067, Boone, NC 28608-2067, USADepartment of Geological Sciences and Institute of Arctic and Alpine Research, University of Colorado Campus Box 450, Boulder, CO 80309-0450, USAGeophysical Institute, University of Alaska-Fairbanks, 2156 Koyukuk Drive, Fairbanks, AK 99775, USA<p>Many glaciers are thinning rapidly beneath melt-reducing 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.</p> <p>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<span class="inline-formula"><sup>2</sup></span> of the 387 km<span class="inline-formula"><sup>2</sup></span> 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.</p> <p>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 <i>relative</i> importance of ice cliffs to area-average melt is significant, the <i>absolute</i> area-averaged melt is dominated by debris.</p> <p>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.</p>https://tc.copernicus.org/articles/15/265/2021/tc-15-265-2021.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. S. Anderson
L. S. Anderson
W. H. Armstrong
W. H. Armstrong
R. S. Anderson
P. Buri
spellingShingle L. S. Anderson
L. S. Anderson
W. H. Armstrong
W. H. Armstrong
R. S. Anderson
P. Buri
Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates
The Cryosphere
author_facet L. S. Anderson
L. S. Anderson
W. H. Armstrong
W. H. Armstrong
R. S. Anderson
P. Buri
author_sort L. S. Anderson
title Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates
title_short Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates
title_full Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates
title_fullStr Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates
title_full_unstemmed Debris cover and the thinning of Kennicott Glacier, Alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates
title_sort debris cover and the thinning of kennicott glacier, alaska: in situ measurements, automated ice cliff delineation and distributed melt estimates
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2021-01-01
description <p>Many glaciers are thinning rapidly beneath melt-reducing 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.</p> <p>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<span class="inline-formula"><sup>2</sup></span> of the 387 km<span class="inline-formula"><sup>2</sup></span> 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.</p> <p>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 <i>relative</i> importance of ice cliffs to area-average melt is significant, the <i>absolute</i> area-averaged melt is dominated by debris.</p> <p>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.</p>
url https://tc.copernicus.org/articles/15/265/2021/tc-15-265-2021.pdf
work_keys_str_mv AT lsanderson debriscoverandthethinningofkennicottglacieralaskainsitumeasurementsautomatedicecliffdelineationanddistributedmeltestimates
AT lsanderson debriscoverandthethinningofkennicottglacieralaskainsitumeasurementsautomatedicecliffdelineationanddistributedmeltestimates
AT wharmstrong debriscoverandthethinningofkennicottglacieralaskainsitumeasurementsautomatedicecliffdelineationanddistributedmeltestimates
AT wharmstrong debriscoverandthethinningofkennicottglacieralaskainsitumeasurementsautomatedicecliffdelineationanddistributedmeltestimates
AT rsanderson debriscoverandthethinningofkennicottglacieralaskainsitumeasurementsautomatedicecliffdelineationanddistributedmeltestimates
AT pburi debriscoverandthethinningofkennicottglacieralaskainsitumeasurementsautomatedicecliffdelineationanddistributedmeltestimates
_version_ 1724331817856663552