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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Published in:The Cryosphere
Main Authors: L. Langhammer, M. Grab, A. Bauder, H. Maurer
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-13-2189-2019
https://www.the-cryosphere.net/13/2189/2019/tc-13-2189-2019.pdf
https://doaj.org/article/93e29f7eab4349b6b6bea057f328b777
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record_format openpolar
spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:93e29f7eab4349b6b6bea057f328b777 2023-05-15T18:32:18+02:00 Glacier thickness estimations of alpine glaciers using data and modeling constraints L. Langhammer M. Grab A. Bauder H. Maurer 2019-08-01 https://doi.org/10.5194/tc-13-2189-2019 https://www.the-cryosphere.net/13/2189/2019/tc-13-2189-2019.pdf https://doaj.org/article/93e29f7eab4349b6b6bea057f328b777 en eng Copernicus Publications doi:10.5194/tc-13-2189-2019 1994-0416 1994-0424 https://www.the-cryosphere.net/13/2189/2019/tc-13-2189-2019.pdf https://doaj.org/article/93e29f7eab4349b6b6bea057f328b777 undefined The Cryosphere, Vol 13, Pp 2189-2202 (2019) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2019 fttriple https://doi.org/10.5194/tc-13-2189-2019 2023-01-22T19:27:51Z 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. Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 13 8 2189 2202
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
L. Langhammer
M. Grab
A. Bauder
H. Maurer
Glacier thickness estimations of alpine glaciers using data and modeling constraints
topic_facet geo
envir
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.
format Article in Journal/Newspaper
author L. Langhammer
M. Grab
A. Bauder
H. Maurer
author_facet L. Langhammer
M. Grab
A. Bauder
H. Maurer
author_sort L. Langhammer
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 Publications
publishDate 2019
url https://doi.org/10.5194/tc-13-2189-2019
https://www.the-cryosphere.net/13/2189/2019/tc-13-2189-2019.pdf
https://doaj.org/article/93e29f7eab4349b6b6bea057f328b777
genre The Cryosphere
genre_facet The Cryosphere
op_source The Cryosphere, Vol 13, Pp 2189-2202 (2019)
op_relation doi:10.5194/tc-13-2189-2019
1994-0416
1994-0424
https://www.the-cryosphere.net/13/2189/2019/tc-13-2189-2019.pdf
https://doaj.org/article/93e29f7eab4349b6b6bea057f328b777
op_rights undefined
op_doi https://doi.org/10.5194/tc-13-2189-2019
container_title The Cryosphere
container_volume 13
container_issue 8
container_start_page 2189
op_container_end_page 2202
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