Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion

We present a novel thickness inversion approach that leverages globally available satellite products and state-of-the-art ice flow models to produce distributed maps of subglacial topography independent of bed observations. While the method can use any complexity of ice physics as represented in ice...

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Main Authors: Frank, Thomas, Pelt, Ward J. J., Kohler, Jack
Format: Text
Language:English
Published: 2023
Subjects:
Online Access:https://doi.org/10.5194/tc-2023-43
https://tc.copernicus.org/preprints/tc-2023-43/
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spelling ftcopernicus:oai:publications.copernicus.org:tcd109999 2023-05-15T16:22:14+02:00 Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion Frank, Thomas Pelt, Ward J. J. Kohler, Jack 2023-04-04 application/pdf https://doi.org/10.5194/tc-2023-43 https://tc.copernicus.org/preprints/tc-2023-43/ eng eng doi:10.5194/tc-2023-43 https://tc.copernicus.org/preprints/tc-2023-43/ eISSN: 1994-0424 Text 2023 ftcopernicus https://doi.org/10.5194/tc-2023-43 2023-04-10T16:23:11Z We present a novel thickness inversion approach that leverages globally available satellite products and state-of-the-art ice flow models to produce distributed maps of subglacial topography independent of bed observations. While the method can use any complexity of ice physics as represented in ice dynamical models, it is computationally cheap, enabling applications both on local and large scales. Using the mismatch between observed and modelled rates of surface elevation change ( dh / dt ) as the misfit functional, iterative pointwise updates to an initial guess of bed topography are made, while mismatches between observed and modelled velocities are used to simultaneously infer basal friction. The final product of the inversion is not only a map of ice thickness, but a fully spun-up glacier model representing the dynamic state of a given glacier. We here present the method, and use an artificial ice-cap built inside a numerical model to test it and conduct sensitivity experiments. Even under a range of perturbations, the method is stable and fast. Finally, we apply the approach to the tidewater glacier Kronebreen on Svalbard. Ultimately, our method shown here represents a fast way of inferring ice thickness where the final output forms a consistent picture of model physics, input observations and bed topography. Text glacier Ice cap Svalbard Tidewater Copernicus Publications: E-Journals Kronebreen ENVELOPE(13.333,13.333,78.833,78.833) Svalbard
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description We present a novel thickness inversion approach that leverages globally available satellite products and state-of-the-art ice flow models to produce distributed maps of subglacial topography independent of bed observations. While the method can use any complexity of ice physics as represented in ice dynamical models, it is computationally cheap, enabling applications both on local and large scales. Using the mismatch between observed and modelled rates of surface elevation change ( dh / dt ) as the misfit functional, iterative pointwise updates to an initial guess of bed topography are made, while mismatches between observed and modelled velocities are used to simultaneously infer basal friction. The final product of the inversion is not only a map of ice thickness, but a fully spun-up glacier model representing the dynamic state of a given glacier. We here present the method, and use an artificial ice-cap built inside a numerical model to test it and conduct sensitivity experiments. Even under a range of perturbations, the method is stable and fast. Finally, we apply the approach to the tidewater glacier Kronebreen on Svalbard. Ultimately, our method shown here represents a fast way of inferring ice thickness where the final output forms a consistent picture of model physics, input observations and bed topography.
format Text
author Frank, Thomas
Pelt, Ward J. J.
Kohler, Jack
spellingShingle Frank, Thomas
Pelt, Ward J. J.
Kohler, Jack
Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion
author_facet Frank, Thomas
Pelt, Ward J. J.
Kohler, Jack
author_sort Frank, Thomas
title Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion
title_short Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion
title_full Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion
title_fullStr Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion
title_full_unstemmed Reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion
title_sort reconciling ice dynamics and bed topography with a versatile and fast ice thickness inversion
publishDate 2023
url https://doi.org/10.5194/tc-2023-43
https://tc.copernicus.org/preprints/tc-2023-43/
long_lat ENVELOPE(13.333,13.333,78.833,78.833)
geographic Kronebreen
Svalbard
geographic_facet Kronebreen
Svalbard
genre glacier
Ice cap
Svalbard
Tidewater
genre_facet glacier
Ice cap
Svalbard
Tidewater
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-2023-43
https://tc.copernicus.org/preprints/tc-2023-43/
op_doi https://doi.org/10.5194/tc-2023-43
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