Predicting ocean-induced ice-shelf melt rates using deep learning

Through their role in buttressing upstream ice flow, Antarctic ice shelves play an important part in regulating future sea-level change. Reduction in ice-shelf buttressing caused by increased ocean-induced melt along their undersides is now understood to be one of the key drivers of ice loss from th...

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Published in:The Cryosphere
Main Authors: Rosier, Sebastian H. R., Bull, Christopher Y. S., Woo, Wai L., Gudmundsson, G. Hilmar
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-17-499-2023
https://tc.copernicus.org/articles/17/499/2023/
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spelling ftcopernicus:oai:publications.copernicus.org:tc100505 2023-05-15T13:38:41+02:00 Predicting ocean-induced ice-shelf melt rates using deep learning Rosier, Sebastian H. R. Bull, Christopher Y. S. Woo, Wai L. Gudmundsson, G. Hilmar 2023-02-07 application/pdf https://doi.org/10.5194/tc-17-499-2023 https://tc.copernicus.org/articles/17/499/2023/ eng eng doi:10.5194/tc-17-499-2023 https://tc.copernicus.org/articles/17/499/2023/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-17-499-2023 2023-02-13T17:22:57Z Through their role in buttressing upstream ice flow, Antarctic ice shelves play an important part in regulating future sea-level change. Reduction in ice-shelf buttressing caused by increased ocean-induced melt along their undersides is now understood to be one of the key drivers of ice loss from the Antarctic ice sheet. However, despite the importance of this forcing mechanism, most ice-sheet simulations currently rely on simple melt parameterisations of this ocean-driven process since a fully coupled ice–ocean modelling framework is prohibitively computationally expensive. Here, we provide an alternative approach that is able to capture the greatly improved physical description of this process provided by large-scale ocean-circulation models over currently employed melt parameterisations but with trivial computational expense. This new method brings together deep learning and physical modelling to develop a deep neural network framework, MELTNET, that can emulate ocean model predictions of sub-ice-shelf melt rates. We train MELTNET on synthetic geometries, using the NEMO ocean model as a ground truth in lieu of observations to provide melt rates both for training and for evaluation of the performance of the trained network. We show that MELTNET can accurately predict melt rates for a wide range of complex synthetic geometries, with a normalised root mean squared error of 0.11 m yr −1 compared to the ocean model. MELTNET calculates melt rates several orders of magnitude faster than the ocean model and outperforms more traditional parameterisations for > 96 % of geometries tested. Furthermore, we find MELTNET's melt rate estimates show sensitivity to established physical relationships such as changes in thermal forcing and ice-shelf slope. This study demonstrates the potential for a deep learning framework to calculate melt rates with almost no computational expense, which could in the future be used in conjunction with an ice sheet model to provide predictions for large-scale ice sheet models. Text Antarc* Antarctic Ice Sheet Ice Shelf Ice Shelves Copernicus Publications: E-Journals Antarctic The Antarctic The Cryosphere 17 2 499 518
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Through their role in buttressing upstream ice flow, Antarctic ice shelves play an important part in regulating future sea-level change. Reduction in ice-shelf buttressing caused by increased ocean-induced melt along their undersides is now understood to be one of the key drivers of ice loss from the Antarctic ice sheet. However, despite the importance of this forcing mechanism, most ice-sheet simulations currently rely on simple melt parameterisations of this ocean-driven process since a fully coupled ice–ocean modelling framework is prohibitively computationally expensive. Here, we provide an alternative approach that is able to capture the greatly improved physical description of this process provided by large-scale ocean-circulation models over currently employed melt parameterisations but with trivial computational expense. This new method brings together deep learning and physical modelling to develop a deep neural network framework, MELTNET, that can emulate ocean model predictions of sub-ice-shelf melt rates. We train MELTNET on synthetic geometries, using the NEMO ocean model as a ground truth in lieu of observations to provide melt rates both for training and for evaluation of the performance of the trained network. We show that MELTNET can accurately predict melt rates for a wide range of complex synthetic geometries, with a normalised root mean squared error of 0.11 m yr −1 compared to the ocean model. MELTNET calculates melt rates several orders of magnitude faster than the ocean model and outperforms more traditional parameterisations for > 96 % of geometries tested. Furthermore, we find MELTNET's melt rate estimates show sensitivity to established physical relationships such as changes in thermal forcing and ice-shelf slope. This study demonstrates the potential for a deep learning framework to calculate melt rates with almost no computational expense, which could in the future be used in conjunction with an ice sheet model to provide predictions for large-scale ice sheet models.
format Text
author Rosier, Sebastian H. R.
Bull, Christopher Y. S.
Woo, Wai L.
Gudmundsson, G. Hilmar
spellingShingle Rosier, Sebastian H. R.
Bull, Christopher Y. S.
Woo, Wai L.
Gudmundsson, G. Hilmar
Predicting ocean-induced ice-shelf melt rates using deep learning
author_facet Rosier, Sebastian H. R.
Bull, Christopher Y. S.
Woo, Wai L.
Gudmundsson, G. Hilmar
author_sort Rosier, Sebastian H. R.
title Predicting ocean-induced ice-shelf melt rates using deep learning
title_short Predicting ocean-induced ice-shelf melt rates using deep learning
title_full Predicting ocean-induced ice-shelf melt rates using deep learning
title_fullStr Predicting ocean-induced ice-shelf melt rates using deep learning
title_full_unstemmed Predicting ocean-induced ice-shelf melt rates using deep learning
title_sort predicting ocean-induced ice-shelf melt rates using deep learning
publishDate 2023
url https://doi.org/10.5194/tc-17-499-2023
https://tc.copernicus.org/articles/17/499/2023/
geographic Antarctic
The Antarctic
geographic_facet Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
genre_facet Antarc*
Antarctic
Ice Sheet
Ice Shelf
Ice Shelves
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-17-499-2023
https://tc.copernicus.org/articles/17/499/2023/
op_doi https://doi.org/10.5194/tc-17-499-2023
container_title The Cryosphere
container_volume 17
container_issue 2
container_start_page 499
op_container_end_page 518
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