Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century

The large Juneau and Stikine icefields (Alaska) lost mass rapidly in the second part of the 20th century. Laser altimetry, gravimetry and field measurements suggest continuing mass loss in the early 21st century. However, two recent studies based on time series of Shuttle Radar Topographic Missio...

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Main Authors: E. Berthier, C. Larsen, W. J. Durkin, M. J. Willis, M. E. Pritchard
Format: Article
Language:English
Published: Copernicus Publications 2018-04-01
Series:The Cryosphere
Online Access:https://www.the-cryosphere.net/12/1523/2018/tc-12-1523-2018.pdf
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spelling doaj-4305774121374a5e9c91a2d9490a8c1b2020-11-24T22:36:38ZengCopernicus PublicationsThe Cryosphere1994-04161994-04242018-04-01121523153010.5194/tc-12-1523-2018Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st centuryE. Berthier0C. Larsen1W. J. Durkin2M. J. Willis3M. E. Pritchard4LEGOS, Université de Toulouse, CNES, CNRS, IRD, UPS, 31400 Toulouse, FranceGeophysical Institute, University of Alaska Fairbanks, Fairbanks, AK, USAEarth and Atmospheric Sciences Department, Cornell University, Ithaca, NY, USACooperative Institute for Research in Environmental Sciences (CIRES), University of Colorado, Boulder, CO, USAEarth and Atmospheric Sciences Department, Cornell University, Ithaca, NY, USAThe large Juneau and Stikine icefields (Alaska) lost mass rapidly in the second part of the 20th century. Laser altimetry, gravimetry and field measurements suggest continuing mass loss in the early 21st century. However, two recent studies based on time series of Shuttle Radar Topographic Mission (SRTM) and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) digital elevation models (DEMs) indicate a slowdown in mass loss after 2000. Here, the ASTER-based geodetic mass balances are recalculated carefully avoiding the use of the SRTM DEM because of the unknown penetration depth of the C-band radar signal. We find strongly negative mass balances from 2000 to 2016 (−0.68 ± 0.15 m w.e. a<sup>−1</sup> for the Juneau Icefield and −0.83 ± 0.12 m w.e. a<sup>−1</sup> for the Stikine Icefield), in agreement with laser altimetry, confirming that mass losses are continuing at unabated rates for both icefields. The SRTM DEM should be avoided or used very cautiously to estimate glacier volume change, especially in the North Hemisphere and over timescales of less than  ∼  20 years.https://www.the-cryosphere.net/12/1523/2018/tc-12-1523-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author E. Berthier
C. Larsen
W. J. Durkin
M. J. Willis
M. E. Pritchard
spellingShingle E. Berthier
C. Larsen
W. J. Durkin
M. J. Willis
M. E. Pritchard
Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century
The Cryosphere
author_facet E. Berthier
C. Larsen
W. J. Durkin
M. J. Willis
M. E. Pritchard
author_sort E. Berthier
title Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century
title_short Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century
title_full Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century
title_fullStr Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century
title_full_unstemmed Brief communication: Unabated wastage of the Juneau and Stikine icefields (southeast Alaska) in the early 21st century
title_sort brief communication: unabated wastage of the juneau and stikine icefields (southeast alaska) in the early 21st century
publisher Copernicus Publications
series The Cryosphere
issn 1994-0416
1994-0424
publishDate 2018-04-01
description The large Juneau and Stikine icefields (Alaska) lost mass rapidly in the second part of the 20th century. Laser altimetry, gravimetry and field measurements suggest continuing mass loss in the early 21st century. However, two recent studies based on time series of Shuttle Radar Topographic Mission (SRTM) and Advanced Spaceborne Thermal Emission and Reflection Radiometer (ASTER) digital elevation models (DEMs) indicate a slowdown in mass loss after 2000. Here, the ASTER-based geodetic mass balances are recalculated carefully avoiding the use of the SRTM DEM because of the unknown penetration depth of the C-band radar signal. We find strongly negative mass balances from 2000 to 2016 (−0.68 ± 0.15 m w.e. a<sup>−1</sup> for the Juneau Icefield and −0.83 ± 0.12 m w.e. a<sup>−1</sup> for the Stikine Icefield), in agreement with laser altimetry, confirming that mass losses are continuing at unabated rates for both icefields. The SRTM DEM should be avoided or used very cautiously to estimate glacier volume change, especially in the North Hemisphere and over timescales of less than  ∼  20 years.
url https://www.the-cryosphere.net/12/1523/2018/tc-12-1523-2018.pdf
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