Inversion of a Stokes glacier flow model emulated by deep learning

Data assimilation in high-order ice flow modeling is a challenging and computationally costly task, yet crucial to find ice thickness and ice flow parameter distributions that are consistent with ice flow mechanics and mass balance while best matching observations. Failing to find these distribution...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Guillaume Jouvet
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2023
Subjects:
Online Access:https://doi.org/10.1017/jog.2022.41
https://doaj.org/article/bd1a7116868b4c0a8b55868becb73ae6
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spelling ftdoajarticles:oai:doaj.org/article:bd1a7116868b4c0a8b55868becb73ae6 2023-05-15T16:57:33+02:00 Inversion of a Stokes glacier flow model emulated by deep learning Guillaume Jouvet 2023-02-01T00:00:00Z https://doi.org/10.1017/jog.2022.41 https://doaj.org/article/bd1a7116868b4c0a8b55868becb73ae6 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000417/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.41 0022-1430 1727-5652 https://doaj.org/article/bd1a7116868b4c0a8b55868becb73ae6 Journal of Glaciology, Vol 69, Pp 13-26 (2023) Glacier flow glacier mechanics glacier modeling ground-penetrating radar ice dynamics Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2023 ftdoajarticles https://doi.org/10.1017/jog.2022.41 2023-03-12T01:30:54Z Data assimilation in high-order ice flow modeling is a challenging and computationally costly task, yet crucial to find ice thickness and ice flow parameter distributions that are consistent with ice flow mechanics and mass balance while best matching observations. Failing to find these distributions that are required as initial conditions leads to a disequilibrium between mass balance and ice flow, resulting in nonphysical transient effects in the prognostic model. Here we tackle this problem by inverting an emulator of the Stokes ice flow model based on deep learning. By substituting the ice flow equations using a convolutional neural network emulator, we simplify, make more robust and dramatically speed up the solving of the underlying optimization problem thanks to automatic differentiation, stochastic gradient methods and implementation of graphics processing unit (GPU). We demonstrate this process by simultaneously inferring the ice thickness distribution, ice flow parametrization and ice surface of ten of the largest glaciers in Switzerland. As a result, we obtain a high degree of assimilation while guaranteeing an equilibrium between mass-balance and ice flow mechanics. The code runs very efficiently (optimizing one large-size glacier at 100 m takes < 1 min on a laptop) while it is open-source and publicly available. Article in Journal/Newspaper Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Journal of Glaciology 69 273 13 26
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Glacier flow
glacier mechanics
glacier modeling
ground-penetrating radar
ice dynamics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Glacier flow
glacier mechanics
glacier modeling
ground-penetrating radar
ice dynamics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Guillaume Jouvet
Inversion of a Stokes glacier flow model emulated by deep learning
topic_facet Glacier flow
glacier mechanics
glacier modeling
ground-penetrating radar
ice dynamics
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description Data assimilation in high-order ice flow modeling is a challenging and computationally costly task, yet crucial to find ice thickness and ice flow parameter distributions that are consistent with ice flow mechanics and mass balance while best matching observations. Failing to find these distributions that are required as initial conditions leads to a disequilibrium between mass balance and ice flow, resulting in nonphysical transient effects in the prognostic model. Here we tackle this problem by inverting an emulator of the Stokes ice flow model based on deep learning. By substituting the ice flow equations using a convolutional neural network emulator, we simplify, make more robust and dramatically speed up the solving of the underlying optimization problem thanks to automatic differentiation, stochastic gradient methods and implementation of graphics processing unit (GPU). We demonstrate this process by simultaneously inferring the ice thickness distribution, ice flow parametrization and ice surface of ten of the largest glaciers in Switzerland. As a result, we obtain a high degree of assimilation while guaranteeing an equilibrium between mass-balance and ice flow mechanics. The code runs very efficiently (optimizing one large-size glacier at 100 m takes < 1 min on a laptop) while it is open-source and publicly available.
format Article in Journal/Newspaper
author Guillaume Jouvet
author_facet Guillaume Jouvet
author_sort Guillaume Jouvet
title Inversion of a Stokes glacier flow model emulated by deep learning
title_short Inversion of a Stokes glacier flow model emulated by deep learning
title_full Inversion of a Stokes glacier flow model emulated by deep learning
title_fullStr Inversion of a Stokes glacier flow model emulated by deep learning
title_full_unstemmed Inversion of a Stokes glacier flow model emulated by deep learning
title_sort inversion of a stokes glacier flow model emulated by deep learning
publisher Cambridge University Press
publishDate 2023
url https://doi.org/10.1017/jog.2022.41
https://doaj.org/article/bd1a7116868b4c0a8b55868becb73ae6
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology, Vol 69, Pp 13-26 (2023)
op_relation https://www.cambridge.org/core/product/identifier/S0022143022000417/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2022.41
0022-1430
1727-5652
https://doaj.org/article/bd1a7116868b4c0a8b55868becb73ae6
op_doi https://doi.org/10.1017/jog.2022.41
container_title Journal of Glaciology
container_volume 69
container_issue 273
container_start_page 13
op_container_end_page 26
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