Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations
The basal interface of glaciers is generally not directly observable. Geophysical inverse methods are therefore used to infer basal parameters from surface observations. Such methods can also provide information about potential inadequacies of the forward model. Ideally an inverse problem can be reg...
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Cambridge University Press
2017
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ftdoajarticles:oai:doaj.org/article:a535d76128074176b5af29f0ffc7f7c1 2023-05-15T16:21:26+02:00 Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations MARIJKE HABERMANN MARTIN TRUFFER DAVID MAXWELL 2017-12-01T00:00:00Z https://doi.org/10.1017/jog.2017.61 https://doaj.org/article/a535d76128074176b5af29f0ffc7f7c1 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143017000612/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2017.61 0022-1430 1727-5652 https://doaj.org/article/a535d76128074176b5af29f0ffc7f7c1 Journal of Glaciology, Vol 63, Pp 999-1011 (2017) glacier modeling ice-sheet modeling subglacial processes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2017 ftdoajarticles https://doi.org/10.1017/jog.2017.61 2023-03-12T01:30:59Z The basal interface of glaciers is generally not directly observable. Geophysical inverse methods are therefore used to infer basal parameters from surface observations. Such methods can also provide information about potential inadequacies of the forward model. Ideally an inverse problem can be regularized so that the differences between modeled and observed surface velocities reflect observational errors. However, deficiencies in the forward model usually result in additional errors. Here we use the spatial pattern of velocity residuals to discuss the main error sources for basal stress inversions for Jakobshavn Isbræ, Greenland. Synthetic tests with prescribed patterns of basal yield stress with varying length scales are then used to investigate different weighting functions for the data-model misfit and for the ability of the inversion to resolve details in basal yield stress. We also test real-data inversions for their sensitivities to prior estimate, forward model parameters, data gaps, and temperature fields. We find that velocity errors are not sufficient to explain the residual patterns of real-data inversions. Conversely, ice-geometry errors and especially simulated errors in model simplifications are capable of reproducing similar error patterns and magnitudes. We suggest that residual patterns can provide useful guidance for forward model improvements. Article in Journal/Newspaper glacier Greenland Ice Sheet Jakobshavn Jakobshavn isbræ Journal of Glaciology Directory of Open Access Journals: DOAJ Articles Greenland Jakobshavn Isbræ ENVELOPE(-49.917,-49.917,69.167,69.167) Journal of Glaciology 63 242 999 1011 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
glacier modeling ice-sheet modeling subglacial processes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
glacier modeling ice-sheet modeling subglacial processes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 MARIJKE HABERMANN MARTIN TRUFFER DAVID MAXWELL Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations |
topic_facet |
glacier modeling ice-sheet modeling subglacial processes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
The basal interface of glaciers is generally not directly observable. Geophysical inverse methods are therefore used to infer basal parameters from surface observations. Such methods can also provide information about potential inadequacies of the forward model. Ideally an inverse problem can be regularized so that the differences between modeled and observed surface velocities reflect observational errors. However, deficiencies in the forward model usually result in additional errors. Here we use the spatial pattern of velocity residuals to discuss the main error sources for basal stress inversions for Jakobshavn Isbræ, Greenland. Synthetic tests with prescribed patterns of basal yield stress with varying length scales are then used to investigate different weighting functions for the data-model misfit and for the ability of the inversion to resolve details in basal yield stress. We also test real-data inversions for their sensitivities to prior estimate, forward model parameters, data gaps, and temperature fields. We find that velocity errors are not sufficient to explain the residual patterns of real-data inversions. Conversely, ice-geometry errors and especially simulated errors in model simplifications are capable of reproducing similar error patterns and magnitudes. We suggest that residual patterns can provide useful guidance for forward model improvements. |
format |
Article in Journal/Newspaper |
author |
MARIJKE HABERMANN MARTIN TRUFFER DAVID MAXWELL |
author_facet |
MARIJKE HABERMANN MARTIN TRUFFER DAVID MAXWELL |
author_sort |
MARIJKE HABERMANN |
title |
Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations |
title_short |
Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations |
title_full |
Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations |
title_fullStr |
Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations |
title_full_unstemmed |
Error sources in basal yield stress inversions for Jakobshavn Isbræ, Greenland, derived from residual patterns of misfit to observations |
title_sort |
error sources in basal yield stress inversions for jakobshavn isbræ, greenland, derived from residual patterns of misfit to observations |
publisher |
Cambridge University Press |
publishDate |
2017 |
url |
https://doi.org/10.1017/jog.2017.61 https://doaj.org/article/a535d76128074176b5af29f0ffc7f7c1 |
long_lat |
ENVELOPE(-49.917,-49.917,69.167,69.167) |
geographic |
Greenland Jakobshavn Isbræ |
geographic_facet |
Greenland Jakobshavn Isbræ |
genre |
glacier Greenland Ice Sheet Jakobshavn Jakobshavn isbræ Journal of Glaciology |
genre_facet |
glacier Greenland Ice Sheet Jakobshavn Jakobshavn isbræ Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 63, Pp 999-1011 (2017) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143017000612/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2017.61 0022-1430 1727-5652 https://doaj.org/article/a535d76128074176b5af29f0ffc7f7c1 |
op_doi |
https://doi.org/10.1017/jog.2017.61 |
container_title |
Journal of Glaciology |
container_volume |
63 |
container_issue |
242 |
container_start_page |
999 |
op_container_end_page |
1011 |
_version_ |
1766009443663740928 |