Variational inference of ice shelf rheology with physics-informed machine learning

Abstract Floating ice shelves that fringe the coast of Antarctica resist the flow of grounded ice into the ocean. One of the key factors governing the amount of flow resistance an ice shelf provides is the rigidity (related to viscosity) of the ice that constitutes it. Ice rigidity is highly heterog...

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Published in:Journal of Glaciology
Main Authors: Riel, Bryan, Minchew, Brent
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 2023
Subjects:
Online Access:http://dx.doi.org/10.1017/jog.2023.8
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000084
id crcambridgeupr:10.1017/jog.2023.8
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spelling crcambridgeupr:10.1017/jog.2023.8 2024-06-23T07:46:09+00:00 Variational inference of ice shelf rheology with physics-informed machine learning Riel, Bryan Minchew, Brent 2023 http://dx.doi.org/10.1017/jog.2023.8 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000084 en eng Cambridge University Press (CUP) http://creativecommons.org/licenses/by/4.0/ Journal of Glaciology volume 69, issue 277, page 1167-1186 ISSN 0022-1430 1727-5652 journal-article 2023 crcambridgeupr https://doi.org/10.1017/jog.2023.8 2024-06-12T04:04:31Z Abstract Floating ice shelves that fringe the coast of Antarctica resist the flow of grounded ice into the ocean. One of the key factors governing the amount of flow resistance an ice shelf provides is the rigidity (related to viscosity) of the ice that constitutes it. Ice rigidity is highly heterogeneous and must be calibrated from spatially continuous surface observations assimilated into an ice-flow model. Realistic uncertainties in calibrated rigidity values are needed to quantify uncertainties in ice sheet and sea-level forecasts. Here, we present a physics-informed machine learning framework for inferring the full probability distribution of rigidity values for a given ice shelf, conditioned on ice surface velocity and thickness fields derived from remote-sensing data. We employ variational inference to jointly train neural networks and a variational Gaussian Process to reconstruct surface observations, rigidity values and uncertainties. Applying the framework to synthetic and large ice shelves in Antarctica demonstrates that rigidity is well-constrained where ice deformation is measurable within the noise level of the observations. Further reduction in uncertainties can be achieved by complementing variational inference with conventional inversion methods. Our results demonstrate a path forward for continuously updated calibrations of ice flow parameters from remote-sensing observations. Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Ice Shelf Ice Shelves Journal of Glaciology Cambridge University Press Journal of Glaciology 1 20
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
description Abstract Floating ice shelves that fringe the coast of Antarctica resist the flow of grounded ice into the ocean. One of the key factors governing the amount of flow resistance an ice shelf provides is the rigidity (related to viscosity) of the ice that constitutes it. Ice rigidity is highly heterogeneous and must be calibrated from spatially continuous surface observations assimilated into an ice-flow model. Realistic uncertainties in calibrated rigidity values are needed to quantify uncertainties in ice sheet and sea-level forecasts. Here, we present a physics-informed machine learning framework for inferring the full probability distribution of rigidity values for a given ice shelf, conditioned on ice surface velocity and thickness fields derived from remote-sensing data. We employ variational inference to jointly train neural networks and a variational Gaussian Process to reconstruct surface observations, rigidity values and uncertainties. Applying the framework to synthetic and large ice shelves in Antarctica demonstrates that rigidity is well-constrained where ice deformation is measurable within the noise level of the observations. Further reduction in uncertainties can be achieved by complementing variational inference with conventional inversion methods. Our results demonstrate a path forward for continuously updated calibrations of ice flow parameters from remote-sensing observations.
format Article in Journal/Newspaper
author Riel, Bryan
Minchew, Brent
spellingShingle Riel, Bryan
Minchew, Brent
Variational inference of ice shelf rheology with physics-informed machine learning
author_facet Riel, Bryan
Minchew, Brent
author_sort Riel, Bryan
title Variational inference of ice shelf rheology with physics-informed machine learning
title_short Variational inference of ice shelf rheology with physics-informed machine learning
title_full Variational inference of ice shelf rheology with physics-informed machine learning
title_fullStr Variational inference of ice shelf rheology with physics-informed machine learning
title_full_unstemmed Variational inference of ice shelf rheology with physics-informed machine learning
title_sort variational inference of ice shelf rheology with physics-informed machine learning
publisher Cambridge University Press (CUP)
publishDate 2023
url http://dx.doi.org/10.1017/jog.2023.8
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143023000084
genre Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Journal of Glaciology
genre_facet Antarc*
Antarctica
Ice Sheet
Ice Shelf
Ice Shelves
Journal of Glaciology
op_source Journal of Glaciology
volume 69, issue 277, page 1167-1186
ISSN 0022-1430 1727-5652
op_rights http://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.1017/jog.2023.8
container_title Journal of Glaciology
container_start_page 1
op_container_end_page 20
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