Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources

We analyzed glacier surface elevations (1957, 2010 and 2015) and surface mass-balance measurements (2008–2015) on the 30 km2 Eklutna Glacier, in the Chugach Mountains of southcentral Alaska. The geodetic mass balances from 1957 to 2010 and 2010 to 2015 are −0.52 ± 0.46 and −0.74 ± 0.10 m w.e. a−1, r...

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Main Authors: LOUIS C. SASS, MICHAEL G. LOSO, JASON GECK, EVAN E. THOMS, DANIEL MCGRATH
Format: Article
Language:English
Published: Cambridge University Press 2017-04-01
Series:Journal of Glaciology
Subjects:
Online Access:https://www.cambridge.org/core/product/identifier/S0022143016001465/type/journal_article
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author LOUIS C. SASS
MICHAEL G. LOSO
JASON GECK
EVAN E. THOMS
DANIEL MCGRATH
author_facet LOUIS C. SASS
MICHAEL G. LOSO
JASON GECK
EVAN E. THOMS
DANIEL MCGRATH
author_sort LOUIS C. SASS
collection DOAJ
description We analyzed glacier surface elevations (1957, 2010 and 2015) and surface mass-balance measurements (2008–2015) on the 30 km2 Eklutna Glacier, in the Chugach Mountains of southcentral Alaska. The geodetic mass balances from 1957 to 2010 and 2010 to 2015 are −0.52 ± 0.46 and −0.74 ± 0.10 m w.e. a−1, respectively. The glaciological mass balance of −0.73 m w.e. a−1 from 2010 to 2015 is indistinguishable from the geodetic value. Even after accounting for loss of firn in the accumulation zone, we found most of the mass loss over both time periods was from a broad, low-slope basin that includes much of the accumulation zone of the main branch. Ice-equivalent surface elevation changes in the basin were −1.0 ± 0.8 m a−1 from 1957 to 2010, and −0.6 ± 0.1 m a−1 from 2010 to 2015, shifting the glacier hypsometry downward and resulting in more negative mass balances: an altitude-mass-balance feedback. Net mass loss from Eklutna Glacier accounts for 7 ± 1% of the average inflow to Eklutna Reservoir, which is entirely used for water and power by Anchorage, Alaska's largest city. If the altitude-mass-balance feedback continues, this ‘deglaciation discharge dividend’ is likely to increase over the short-term before it eventually decreases due to diminishing glacier area.
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spelling doaj.art-55c8acbcc9724b4282d17a136f996c272023-03-09T12:40:20ZengCambridge University PressJournal of Glaciology0022-14301727-56522017-04-016334335410.1017/jog.2016.146Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resourcesLOUIS C. SASS0https://orcid.org/0000-0003-4677-029XMICHAEL G. LOSO1JASON GECK2EVAN E. THOMS3DANIEL MCGRATH4Alaska Science Center, U.S. Geological Survey, Anchorage, AK, USA Environmental Science, Alaska Pacific University, Anchorage, AK, USAEnvironmental Science, Alaska Pacific University, Anchorage, AK, USA Inventory and Monitoring Program, Wrangell-St. Elias National Park and Preserve, Copper Center, AK, USAEnvironmental Science, Alaska Pacific University, Anchorage, AK, USAAlaska Science Center, U.S. Geological Survey, Anchorage, AK, USAAlaska Science Center, U.S. Geological Survey, Anchorage, AK, USA Geosciences Department, Colorado State University, Fort Collins, CO, USAWe analyzed glacier surface elevations (1957, 2010 and 2015) and surface mass-balance measurements (2008–2015) on the 30 km2 Eklutna Glacier, in the Chugach Mountains of southcentral Alaska. The geodetic mass balances from 1957 to 2010 and 2010 to 2015 are −0.52 ± 0.46 and −0.74 ± 0.10 m w.e. a−1, respectively. The glaciological mass balance of −0.73 m w.e. a−1 from 2010 to 2015 is indistinguishable from the geodetic value. Even after accounting for loss of firn in the accumulation zone, we found most of the mass loss over both time periods was from a broad, low-slope basin that includes much of the accumulation zone of the main branch. Ice-equivalent surface elevation changes in the basin were −1.0 ± 0.8 m a−1 from 1957 to 2010, and −0.6 ± 0.1 m a−1 from 2010 to 2015, shifting the glacier hypsometry downward and resulting in more negative mass balances: an altitude-mass-balance feedback. Net mass loss from Eklutna Glacier accounts for 7 ± 1% of the average inflow to Eklutna Reservoir, which is entirely used for water and power by Anchorage, Alaska's largest city. If the altitude-mass-balance feedback continues, this ‘deglaciation discharge dividend’ is likely to increase over the short-term before it eventually decreases due to diminishing glacier area.https://www.cambridge.org/core/product/identifier/S0022143016001465/type/journal_articleapplied glaciologyclimate changeglacier mass balanceglacier volumemountain glaciers
spellingShingle LOUIS C. SASS
MICHAEL G. LOSO
JASON GECK
EVAN E. THOMS
DANIEL MCGRATH
Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
Journal of Glaciology
applied glaciology
climate change
glacier mass balance
glacier volume
mountain glaciers
title Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
title_full Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
title_fullStr Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
title_full_unstemmed Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
title_short Geometry, mass balance and thinning at Eklutna Glacier, Alaska: an altitude-mass-balance feedback with implications for water resources
title_sort geometry mass balance and thinning at eklutna glacier alaska an altitude mass balance feedback with implications for water resources
topic applied glaciology
climate change
glacier mass balance
glacier volume
mountain glaciers
url https://www.cambridge.org/core/product/identifier/S0022143016001465/type/journal_article
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