Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE

Information about subglacial topography is essential for modelling ice flow and estimating the potential contribution of glaciers to sea-level rise. In-situ measurements of glacier bed elevation are costly, cumbersome and only sparsely available for mountain glaciers and ice caps. Here, we present t...

Full description

Bibliographic Details
Main Author: Gregor, Philipp
Format: Master Thesis
Language:English
Published: 2018
Subjects:
bed
Online Access:https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-32546
id ftunivinnsbruck:oai:diglib.uibk.ac.at/:3086935
record_format openpolar
spelling ftunivinnsbruck:oai:diglib.uibk.ac.at/:3086935 2023-10-01T03:56:37+02:00 Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE Inversion of glacier bed from surface observations by cost minimization – introducing the open source model COMBINE Gregor, Philipp Innsbruck 38.82 38.03 38.79 38.99 38.84 RB 10372 UI:GA:MG December 2018 iv, 79 Seiten text/html Illustrationen, Diagramme https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-32546 eng eng vignette : https://diglib.uibk.ac.at/titlepage/urn/urn:nbn:at:at-ubi:1-32546/128 urn:nbn:at:at-ubi:1-32546 https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-32546 local:99144876537903331 system:AC15261214 cc-by_4 Gletscher Eiskappe Inversion Modellierung Bett Kostenfunktion Minimierung Optimierung Variationell glacier ice cap modeling bed subglacial topography variational minimization optimization cost function automatic differentiation Text Thesis Hochschulschrift MasterThesis 2018 ftunivinnsbruck 2023-09-04T22:07:43Z Information about subglacial topography is essential for modelling ice flow and estimating the potential contribution of glaciers to sea-level rise. In-situ measurements of glacier bed elevation are costly, cumbersome and only sparsely available for mountain glaciers and ice caps. Here, we present the Cost Minimization Bed Inversion model (COMBINE), which estimates bed topography from surface topography and glacier outlines alone. A distributed shallow ice model (forward model) provides an estimate of the ice surface topography as a function of the unknown bed topography. A coarse first guess of the bed elevation is then iteratively optimized by minimizing a cost function of surface misfit. The gradient of the cost function obtained by Automatic Differentiation (AD) is used by the minimization algorithm to efficiently converge to a (local) cost minimum. To test the method, two synthetic ice caps were created using the forward model driven by a prescribed climate and realistic topography. In this surrogate world where everything is known a priori, the performance of COMBINE can be assessed in various use case scenarios. With perfectly known surface elevation, errors in the reconstructed bed are found to be small and comparable to uncertainties obtained by GPR measurements. Repeating these experiments with varying first guess gives similar results, indicating that the method is robust to this arbitrary choice. Further experiments with noise imposed on the provided surface elevation show decreasing performance of the bed inversion with increasing noise. However, COMBINE is able to partly compensate for this noise by imposing physical constraints on unrealistic inputs. COMBINE can also be extended to use ice thickness observations to better constrain the bed estimation ("data assimilation"). This leads to an improvement of the bed reconstruction but depends on the location and extent of the observations. COMBINE and its variational principle can be used on real mountain by Philipp Gregor Abweichender Titel laut ... Master Thesis Ice cap University of Innsbruck: Digital Library (Universitäts- und Landesbibliothek Tirol)
institution Open Polar
collection University of Innsbruck: Digital Library (Universitäts- und Landesbibliothek Tirol)
op_collection_id ftunivinnsbruck
language English
topic Gletscher
Eiskappe
Inversion
Modellierung
Bett
Kostenfunktion
Minimierung
Optimierung
Variationell
glacier
ice cap
modeling
bed
subglacial topography
variational
minimization
optimization
cost function
automatic differentiation
spellingShingle Gletscher
Eiskappe
Inversion
Modellierung
Bett
Kostenfunktion
Minimierung
Optimierung
Variationell
glacier
ice cap
modeling
bed
subglacial topography
variational
minimization
optimization
cost function
automatic differentiation
Gregor, Philipp
Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE
topic_facet Gletscher
Eiskappe
Inversion
Modellierung
Bett
Kostenfunktion
Minimierung
Optimierung
Variationell
glacier
ice cap
modeling
bed
subglacial topography
variational
minimization
optimization
cost function
automatic differentiation
description Information about subglacial topography is essential for modelling ice flow and estimating the potential contribution of glaciers to sea-level rise. In-situ measurements of glacier bed elevation are costly, cumbersome and only sparsely available for mountain glaciers and ice caps. Here, we present the Cost Minimization Bed Inversion model (COMBINE), which estimates bed topography from surface topography and glacier outlines alone. A distributed shallow ice model (forward model) provides an estimate of the ice surface topography as a function of the unknown bed topography. A coarse first guess of the bed elevation is then iteratively optimized by minimizing a cost function of surface misfit. The gradient of the cost function obtained by Automatic Differentiation (AD) is used by the minimization algorithm to efficiently converge to a (local) cost minimum. To test the method, two synthetic ice caps were created using the forward model driven by a prescribed climate and realistic topography. In this surrogate world where everything is known a priori, the performance of COMBINE can be assessed in various use case scenarios. With perfectly known surface elevation, errors in the reconstructed bed are found to be small and comparable to uncertainties obtained by GPR measurements. Repeating these experiments with varying first guess gives similar results, indicating that the method is robust to this arbitrary choice. Further experiments with noise imposed on the provided surface elevation show decreasing performance of the bed inversion with increasing noise. However, COMBINE is able to partly compensate for this noise by imposing physical constraints on unrealistic inputs. COMBINE can also be extended to use ice thickness observations to better constrain the bed estimation ("data assimilation"). This leads to an improvement of the bed reconstruction but depends on the location and extent of the observations. COMBINE and its variational principle can be used on real mountain by Philipp Gregor Abweichender Titel laut ...
format Master Thesis
author Gregor, Philipp
author_facet Gregor, Philipp
author_sort Gregor, Philipp
title Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE
title_short Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE
title_full Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE
title_fullStr Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE
title_full_unstemmed Inversion of glacier bed from surface observations by cost minimization : introducing the open source model COMBINE
title_sort inversion of glacier bed from surface observations by cost minimization : introducing the open source model combine
publishDate 2018
url https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-32546
op_coverage Innsbruck
38.82
38.03
38.79
38.99
38.84
RB 10372
UI:GA:MG
genre Ice cap
genre_facet Ice cap
op_relation vignette : https://diglib.uibk.ac.at/titlepage/urn/urn:nbn:at:at-ubi:1-32546/128
urn:nbn:at:at-ubi:1-32546
https://resolver.obvsg.at/urn:nbn:at:at-ubi:1-32546
local:99144876537903331
system:AC15261214
op_rights cc-by_4
_version_ 1778526604531597312