The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat

Humboldt Glacier, northern Greenland, has retreated and accelerated through the 21st century, raising concerns that it could be a significant contributor to future sea-level rise. We use a data-constrained ensemble of three-dimensional higher-order ice sheet model simulations to estimate the likely...

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Published in:The Cryosphere
Main Authors: Hillebrand, Trevor R., Hoffman, Matthew J., Perego, Mauro, Price, Stephen F., Howat, Ian M.
Format: Text
Language:English
Published: 2022
Subjects:
Online Access:https://doi.org/10.5194/tc-16-4679-2022
https://tc.copernicus.org/articles/16/4679/2022/
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spelling ftcopernicus:oai:publications.copernicus.org:tc101096 2023-05-15T16:21:17+02:00 The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat Hillebrand, Trevor R. Hoffman, Matthew J. Perego, Mauro Price, Stephen F. Howat, Ian M. 2022-11-11 application/pdf https://doi.org/10.5194/tc-16-4679-2022 https://tc.copernicus.org/articles/16/4679/2022/ eng eng doi:10.5194/tc-16-4679-2022 https://tc.copernicus.org/articles/16/4679/2022/ eISSN: 1994-0424 Text 2022 ftcopernicus https://doi.org/10.5194/tc-16-4679-2022 2022-11-14T17:22:41Z Humboldt Glacier, northern Greenland, has retreated and accelerated through the 21st century, raising concerns that it could be a significant contributor to future sea-level rise. We use a data-constrained ensemble of three-dimensional higher-order ice sheet model simulations to estimate the likely range of sea-level rise from the continued retreat of Humboldt Glacier. We first solve for basal traction using observed ice thickness, bed topography, and ice surface velocity from the year 2007 in a PDE-constrained (partial differential equation) optimization. Next, we impose calving rates to match mean observed retreat rates from winter 2007–2008 to winter 2017–2018 in a transient calibration of the exponent in the power-law basal friction relationship. We find that power-law exponents in the range of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">7</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="29d80a96c1e485b2ea8e9894bab6fe24"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-4679-2022-ie00001.svg" width="20pt" height="14pt" src="tc-16-4679-2022-ie00001.png"/></svg:svg> – <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">5</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="215b47dca0c01018ce05fbe844dd5ae6"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-4679-2022-ie00002.svg" width="20pt" height="14pt" src="tc-16-4679-2022-ie00002.png"/></svg:svg> – rather than the commonly ... Text glacier Greenland Humboldt Glacier Ice Sheet Copernicus Publications: E-Journals Greenland The Cryosphere 16 11 4679 4700
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Humboldt Glacier, northern Greenland, has retreated and accelerated through the 21st century, raising concerns that it could be a significant contributor to future sea-level rise. We use a data-constrained ensemble of three-dimensional higher-order ice sheet model simulations to estimate the likely range of sea-level rise from the continued retreat of Humboldt Glacier. We first solve for basal traction using observed ice thickness, bed topography, and ice surface velocity from the year 2007 in a PDE-constrained (partial differential equation) optimization. Next, we impose calving rates to match mean observed retreat rates from winter 2007–2008 to winter 2017–2018 in a transient calibration of the exponent in the power-law basal friction relationship. We find that power-law exponents in the range of <math xmlns="http://www.w3.org/1998/Math/MathML" id="M1" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">7</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="29d80a96c1e485b2ea8e9894bab6fe24"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-4679-2022-ie00001.svg" width="20pt" height="14pt" src="tc-16-4679-2022-ie00001.png"/></svg:svg> – <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mn mathvariant="normal">1</mn><mo>/</mo><mn mathvariant="normal">5</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="20pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="215b47dca0c01018ce05fbe844dd5ae6"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="tc-16-4679-2022-ie00002.svg" width="20pt" height="14pt" src="tc-16-4679-2022-ie00002.png"/></svg:svg> – rather than the commonly ...
format Text
author Hillebrand, Trevor R.
Hoffman, Matthew J.
Perego, Mauro
Price, Stephen F.
Howat, Ian M.
spellingShingle Hillebrand, Trevor R.
Hoffman, Matthew J.
Perego, Mauro
Price, Stephen F.
Howat, Ian M.
The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat
author_facet Hillebrand, Trevor R.
Hoffman, Matthew J.
Perego, Mauro
Price, Stephen F.
Howat, Ian M.
author_sort Hillebrand, Trevor R.
title The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat
title_short The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat
title_full The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat
title_fullStr The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat
title_full_unstemmed The contribution of Humboldt Glacier, northern Greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat
title_sort contribution of humboldt glacier, northern greenland, to sea-level rise through 2100 constrained by recent observations of speedup and retreat
publishDate 2022
url https://doi.org/10.5194/tc-16-4679-2022
https://tc.copernicus.org/articles/16/4679/2022/
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
Humboldt Glacier
Ice Sheet
genre_facet glacier
Greenland
Humboldt Glacier
Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-16-4679-2022
https://tc.copernicus.org/articles/16/4679/2022/
op_doi https://doi.org/10.5194/tc-16-4679-2022
container_title The Cryosphere
container_volume 16
container_issue 11
container_start_page 4679
op_container_end_page 4700
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