Glacier thickness estimations of alpine glaciers using data and modeling constraints

Advanced knowledge of the ice thickness distribution within glaciers is of fundamental importance for several purposes, such as water resource management and the study of the impact of climate change. Ice thicknesses can be modeled using ice surface features, but the resulting models can be prone to...

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Main Authors: Langhammer, Lisbeth, Grab, Melchior, Bauder, Andreas, Maurer, Hansruedi
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus 2019
Subjects:
Online Access:https://hdl.handle.net/20.500.11850/361623
https://doi.org/10.3929/ethz-b-000361623
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spelling ftethz:oai:www.research-collection.ethz.ch:20.500.11850/361623 2023-05-15T18:32:14+02:00 Glacier thickness estimations of alpine glaciers using data and modeling constraints Langhammer, Lisbeth Grab, Melchior Bauder, Andreas Maurer, Hansruedi 2019 application/application/pdf https://hdl.handle.net/20.500.11850/361623 https://doi.org/10.3929/ethz-b-000361623 en eng Copernicus info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-13-2189-2019 info:eu-repo/semantics/altIdentifier/wos/000481989700002 http://hdl.handle.net/20.500.11850/361623 doi:10.3929/ethz-b-000361623 info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by/4.0/ Creative Commons Attribution 4.0 International CC-BY The Cryosphere, 13 (8) info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftethz https://doi.org/20.500.11850/361623 https://doi.org/10.3929/ethz-b-000361623 https://doi.org/10.5194/tc-13-2189-2019 2022-04-25T13:54:01Z Advanced knowledge of the ice thickness distribution within glaciers is of fundamental importance for several purposes, such as water resource management and the study of the impact of climate change. Ice thicknesses can be modeled using ice surface features, but the resulting models can be prone to considerable uncertainties. Alternatively, it is possible to measure ice thicknesses, for example, with ground-penetrating radar (GPR). Such measurements are typically restricted to a few profiles, with which it is not possible to obtain spatially unaliased subsurface images. We developed the Glacier Thickness Estimation algorithm (GlaTE), which optimally combines modeling results and measured ice thicknesses in an inversion procedure to obtain overall thickness distributions. GlaTE offers the flexibility of being able to add any existing modeling algorithm, and any further constraints can be added in a straightforward manner. Furthermore, it accounts for the uncertainties associated with the individual constraints. Properties and benefits of GlaTE are demonstrated with three case studies performed on different types of alpine glaciers. In all three cases, subsurface models could be found that are consistent with glaciological modeling and GPR data constraints. Since acquiring GPR data on glaciers can be an expensive endeavor, we additionally employed elements of sequential optimized experimental design (SOED) for determining cost-optimized GPR survey layouts. The calculated cost–benefit curves indicate that a relatively large amount of data can be acquired before redundant information is collected with any additional profiles, and it becomes increasingly expensive to obtain further information. ISSN:1994-0416 ISSN:1994-0424 Article in Journal/Newspaper The Cryosphere ETH Zürich Research Collection
institution Open Polar
collection ETH Zürich Research Collection
op_collection_id ftethz
language English
description Advanced knowledge of the ice thickness distribution within glaciers is of fundamental importance for several purposes, such as water resource management and the study of the impact of climate change. Ice thicknesses can be modeled using ice surface features, but the resulting models can be prone to considerable uncertainties. Alternatively, it is possible to measure ice thicknesses, for example, with ground-penetrating radar (GPR). Such measurements are typically restricted to a few profiles, with which it is not possible to obtain spatially unaliased subsurface images. We developed the Glacier Thickness Estimation algorithm (GlaTE), which optimally combines modeling results and measured ice thicknesses in an inversion procedure to obtain overall thickness distributions. GlaTE offers the flexibility of being able to add any existing modeling algorithm, and any further constraints can be added in a straightforward manner. Furthermore, it accounts for the uncertainties associated with the individual constraints. Properties and benefits of GlaTE are demonstrated with three case studies performed on different types of alpine glaciers. In all three cases, subsurface models could be found that are consistent with glaciological modeling and GPR data constraints. Since acquiring GPR data on glaciers can be an expensive endeavor, we additionally employed elements of sequential optimized experimental design (SOED) for determining cost-optimized GPR survey layouts. The calculated cost–benefit curves indicate that a relatively large amount of data can be acquired before redundant information is collected with any additional profiles, and it becomes increasingly expensive to obtain further information. ISSN:1994-0416 ISSN:1994-0424
format Article in Journal/Newspaper
author Langhammer, Lisbeth
Grab, Melchior
Bauder, Andreas
Maurer, Hansruedi
spellingShingle Langhammer, Lisbeth
Grab, Melchior
Bauder, Andreas
Maurer, Hansruedi
Glacier thickness estimations of alpine glaciers using data and modeling constraints
author_facet Langhammer, Lisbeth
Grab, Melchior
Bauder, Andreas
Maurer, Hansruedi
author_sort Langhammer, Lisbeth
title Glacier thickness estimations of alpine glaciers using data and modeling constraints
title_short Glacier thickness estimations of alpine glaciers using data and modeling constraints
title_full Glacier thickness estimations of alpine glaciers using data and modeling constraints
title_fullStr Glacier thickness estimations of alpine glaciers using data and modeling constraints
title_full_unstemmed Glacier thickness estimations of alpine glaciers using data and modeling constraints
title_sort glacier thickness estimations of alpine glaciers using data and modeling constraints
publisher Copernicus
publishDate 2019
url https://hdl.handle.net/20.500.11850/361623
https://doi.org/10.3929/ethz-b-000361623
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, 13 (8)
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/tc-13-2189-2019
info:eu-repo/semantics/altIdentifier/wos/000481989700002
http://hdl.handle.net/20.500.11850/361623
doi:10.3929/ethz-b-000361623
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by/4.0/
Creative Commons Attribution 4.0 International
op_rightsnorm CC-BY
op_doi https://doi.org/20.500.11850/361623
https://doi.org/10.3929/ethz-b-000361623
https://doi.org/10.5194/tc-13-2189-2019
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