A Bayesian ice thickness estimation model for large-scale applications

Abstract Accurate estimations of ice thickness and volume are indispensable for ice flow modelling, hydrological forecasts and sea-level rise projections. We present a new ice thickness estimation model based on a mass-conserving forward model and a Bayesian inversion scheme. The forward model calcu...

Full description

Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Werder, Mauro A., Huss, Matthias, Paul, Frank, Dehecq, Amaury, Farinotti, Daniel
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2019
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2019.93
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143019000935
id crcambridgeupr:10.1017/jog.2019.93
record_format openpolar
spelling crcambridgeupr:10.1017/jog.2019.93 2024-09-15T18:15:38+00:00 A Bayesian ice thickness estimation model for large-scale applications Werder, Mauro A. Huss, Matthias Paul, Frank Dehecq, Amaury Farinotti, Daniel 2019 http://dx.doi.org/10.1017/jog.2019.93 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143019000935 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 66, issue 255, page 137-152 ISSN 0022-1430 1727-5652 journal-article 2019 crcambridgeupr https://doi.org/10.1017/jog.2019.93 2024-07-24T04:04:08Z Abstract Accurate estimations of ice thickness and volume are indispensable for ice flow modelling, hydrological forecasts and sea-level rise projections. We present a new ice thickness estimation model based on a mass-conserving forward model and a Bayesian inversion scheme. The forward model calculates flux in an elevation-band flow-line model, and translates this into ice thickness and surface ice speed using a shallow ice formulation. Both ice thickness and speed are then extrapolated to the map plane. The model assimilates observations of ice thickness and speed using a Bayesian scheme implemented with a Markov chain Monte Carlo method, which calculates estimates of ice thickness and their error. We illustrate the model's capabilities by applying it to a mountain glacier, validate the model using 733 glaciers from four regions with ice thickness measurements, and demonstrate that the model can be used for large-scale studies by fitting it to over 30 000 glaciers from five regions. The results show that the model performs best when a few thickness observations are available; that the proposed scheme by which parameter-knowledge from a set of glaciers is transferred to others works but has room for improvements; and that the inferred regional ice volumes are consistent with recent estimates. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 66 255 137 152
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Accurate estimations of ice thickness and volume are indispensable for ice flow modelling, hydrological forecasts and sea-level rise projections. We present a new ice thickness estimation model based on a mass-conserving forward model and a Bayesian inversion scheme. The forward model calculates flux in an elevation-band flow-line model, and translates this into ice thickness and surface ice speed using a shallow ice formulation. Both ice thickness and speed are then extrapolated to the map plane. The model assimilates observations of ice thickness and speed using a Bayesian scheme implemented with a Markov chain Monte Carlo method, which calculates estimates of ice thickness and their error. We illustrate the model's capabilities by applying it to a mountain glacier, validate the model using 733 glaciers from four regions with ice thickness measurements, and demonstrate that the model can be used for large-scale studies by fitting it to over 30 000 glaciers from five regions. The results show that the model performs best when a few thickness observations are available; that the proposed scheme by which parameter-knowledge from a set of glaciers is transferred to others works but has room for improvements; and that the inferred regional ice volumes are consistent with recent estimates.
format Article in Journal/Newspaper
author Werder, Mauro A.
Huss, Matthias
Paul, Frank
Dehecq, Amaury
Farinotti, Daniel
spellingShingle Werder, Mauro A.
Huss, Matthias
Paul, Frank
Dehecq, Amaury
Farinotti, Daniel
A Bayesian ice thickness estimation model for large-scale applications
author_facet Werder, Mauro A.
Huss, Matthias
Paul, Frank
Dehecq, Amaury
Farinotti, Daniel
author_sort Werder, Mauro A.
title A Bayesian ice thickness estimation model for large-scale applications
title_short A Bayesian ice thickness estimation model for large-scale applications
title_full A Bayesian ice thickness estimation model for large-scale applications
title_fullStr A Bayesian ice thickness estimation model for large-scale applications
title_full_unstemmed A Bayesian ice thickness estimation model for large-scale applications
title_sort bayesian ice thickness estimation model for large-scale applications
publisher Cambridge University Press (CUP)
publishDate 2019
url http://dx.doi.org/10.1017/jog.2019.93
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143019000935
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 66, issue 255, page 137-152
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2019.93
container_title Journal of Glaciology
container_volume 66
container_issue 255
container_start_page 137
op_container_end_page 152
_version_ 1810453525593849856