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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Cambridge University Press
2023
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Online Access: | https://doi.org/10.1017/jog.2022.41 https://doaj.org/article/bd1a7116868b4c0a8b55868becb73ae6 |
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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 |
_version_ |
1766049113012436992 |