agstub/subglacial-inversion: First release of subglacial parameter inversion code

This python code inverts ice-sheet altimetry data for two types of subglacial parameters: the basal vertical velocity or basal drag coefficient field. The forward model is based on a small-perturbation approximation of the Stokes equations, and the least-squares inverse problem is solved with the co...

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Main Author: Aaron Stubblefield
Format: Software
Language:unknown
Published: 2021
Subjects:
Online Access:https://zenodo.org/record/5775178
https://doi.org/10.5281/zenodo.5775178
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record_format openpolar
spelling ftzenodo:oai:zenodo.org:5775178 2023-06-06T11:55:02+02:00 agstub/subglacial-inversion: First release of subglacial parameter inversion code Aaron Stubblefield 2021-12-12 https://zenodo.org/record/5775178 https://doi.org/10.5281/zenodo.5775178 unknown https://github.com/agstub/subglacial-inversion/tree/v1.0.0 doi:10.5281/zenodo.5775177 https://zenodo.org/record/5775178 https://doi.org/10.5281/zenodo.5775178 oai:zenodo.org:5775178 info:eu-repo/semantics/openAccess info:eu-repo/semantics/other software 2021 ftzenodo https://doi.org/10.5281/zenodo.577517810.5281/zenodo.5775177 2023-04-13T23:25:35Z This python code inverts ice-sheet altimetry data for two types of subglacial parameters: the basal vertical velocity or basal drag coefficient field. The forward model is based on a small-perturbation approximation of the Stokes equations, and the least-squares inverse problem is solved with the conjugate gradient method. The primary operations involve map-plane Fourier transforms and convolution over time, which are implemented with SciPy's FFT methods. The complete details are included in a forthcoming manuscript. The Jupyter notebooks in the "notebooks" directory reproduce the computational examples from the manuscript. Software Ice Sheet Zenodo
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description This python code inverts ice-sheet altimetry data for two types of subglacial parameters: the basal vertical velocity or basal drag coefficient field. The forward model is based on a small-perturbation approximation of the Stokes equations, and the least-squares inverse problem is solved with the conjugate gradient method. The primary operations involve map-plane Fourier transforms and convolution over time, which are implemented with SciPy's FFT methods. The complete details are included in a forthcoming manuscript. The Jupyter notebooks in the "notebooks" directory reproduce the computational examples from the manuscript.
format Software
author Aaron Stubblefield
spellingShingle Aaron Stubblefield
agstub/subglacial-inversion: First release of subglacial parameter inversion code
author_facet Aaron Stubblefield
author_sort Aaron Stubblefield
title agstub/subglacial-inversion: First release of subglacial parameter inversion code
title_short agstub/subglacial-inversion: First release of subglacial parameter inversion code
title_full agstub/subglacial-inversion: First release of subglacial parameter inversion code
title_fullStr agstub/subglacial-inversion: First release of subglacial parameter inversion code
title_full_unstemmed agstub/subglacial-inversion: First release of subglacial parameter inversion code
title_sort agstub/subglacial-inversion: first release of subglacial parameter inversion code
publishDate 2021
url https://zenodo.org/record/5775178
https://doi.org/10.5281/zenodo.5775178
genre Ice Sheet
genre_facet Ice Sheet
op_relation https://github.com/agstub/subglacial-inversion/tree/v1.0.0
doi:10.5281/zenodo.5775177
https://zenodo.org/record/5775178
https://doi.org/10.5281/zenodo.5775178
oai:zenodo.org:5775178
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.5281/zenodo.577517810.5281/zenodo.5775177
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