A note on digital elevation model smoothing and driving stresses

Ice-flow fields, including the driving stress, provide important information on the current state and evolution of Antarctic and Greenland ice-sheet dynamics. However, computation of flow fields from continent-scale DEMs requires the use of smoothing functions and scales, the choice of which can be...

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Published in:Polar Research
Main Authors: McCormack, Felicity S., Roberts, Jason L., Jong, Lenneke M., Young, Duncan A., Beem, Lucas H.
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2019
Subjects:
Online Access:https://polarresearch.net/index.php/polar/article/view/3498
https://doi.org/10.33265/polar.v38.3498
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spelling ftjpolarres:oai:journals.openacademia.net:article/3498 2024-06-23T07:47:11+00:00 A note on digital elevation model smoothing and driving stresses McCormack, Felicity S. Roberts, Jason L. Jong, Lenneke M. Young, Duncan A. Beem, Lucas H. 2019-03-28 application/pdf text/html application/epub+zip application/xml https://polarresearch.net/index.php/polar/article/view/3498 https://doi.org/10.33265/polar.v38.3498 eng eng Norwegian Polar Institute https://polarresearch.net/index.php/polar/article/view/3498/9172 https://polarresearch.net/index.php/polar/article/view/3498/9173 https://polarresearch.net/index.php/polar/article/view/3498/9174 https://polarresearch.net/index.php/polar/article/view/3498/9176 https://polarresearch.net/index.php/polar/article/view/3498 doi:10.33265/polar.v38.3498 Polar Research; Vol 38 (2019) 1751-8369 ice-flow direction smoothing filter Antarctic Ice Sheet ice-sheet dynamics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2019 ftjpolarres https://doi.org/10.33265/polar.v38.3498 2024-06-13T23:33:00Z Ice-flow fields, including the driving stress, provide important information on the current state and evolution of Antarctic and Greenland ice-sheet dynamics. However, computation of flow fields from continent-scale DEMs requires the use of smoothing functions and scales, the choice of which can be ad hoc. This study evaluates smoothing functions and scales for robust calculations of driving stress from Antarctic DEMs. Our approach compares a variety of filters and scales for their capacity to minimize the residual between predicted and observed flow direction fields. We find that a spatially varying triangular filter with a width of 8–10 ice thicknesses provides the closest match between the observed and predicted flow direction fields. We use the predicted flow direction fields to highlight artefacts in observed Antarctic velocities, demonstrating that comparison of multiple observational data sets has utility for quality control of continent-scale data sets. Article in Journal/Newspaper Antarc* Antarctic Greenland Ice Sheet Polar Research Polar Research Antarctic Greenland Polar Research 38 0
institution Open Polar
collection Polar Research
op_collection_id ftjpolarres
language English
topic ice-flow direction
smoothing filter
Antarctic Ice Sheet
ice-sheet dynamics
spellingShingle ice-flow direction
smoothing filter
Antarctic Ice Sheet
ice-sheet dynamics
McCormack, Felicity S.
Roberts, Jason L.
Jong, Lenneke M.
Young, Duncan A.
Beem, Lucas H.
A note on digital elevation model smoothing and driving stresses
topic_facet ice-flow direction
smoothing filter
Antarctic Ice Sheet
ice-sheet dynamics
description Ice-flow fields, including the driving stress, provide important information on the current state and evolution of Antarctic and Greenland ice-sheet dynamics. However, computation of flow fields from continent-scale DEMs requires the use of smoothing functions and scales, the choice of which can be ad hoc. This study evaluates smoothing functions and scales for robust calculations of driving stress from Antarctic DEMs. Our approach compares a variety of filters and scales for their capacity to minimize the residual between predicted and observed flow direction fields. We find that a spatially varying triangular filter with a width of 8–10 ice thicknesses provides the closest match between the observed and predicted flow direction fields. We use the predicted flow direction fields to highlight artefacts in observed Antarctic velocities, demonstrating that comparison of multiple observational data sets has utility for quality control of continent-scale data sets.
format Article in Journal/Newspaper
author McCormack, Felicity S.
Roberts, Jason L.
Jong, Lenneke M.
Young, Duncan A.
Beem, Lucas H.
author_facet McCormack, Felicity S.
Roberts, Jason L.
Jong, Lenneke M.
Young, Duncan A.
Beem, Lucas H.
author_sort McCormack, Felicity S.
title A note on digital elevation model smoothing and driving stresses
title_short A note on digital elevation model smoothing and driving stresses
title_full A note on digital elevation model smoothing and driving stresses
title_fullStr A note on digital elevation model smoothing and driving stresses
title_full_unstemmed A note on digital elevation model smoothing and driving stresses
title_sort note on digital elevation model smoothing and driving stresses
publisher Norwegian Polar Institute
publishDate 2019
url https://polarresearch.net/index.php/polar/article/view/3498
https://doi.org/10.33265/polar.v38.3498
geographic Antarctic
Greenland
geographic_facet Antarctic
Greenland
genre Antarc*
Antarctic
Greenland
Ice Sheet
Polar Research
genre_facet Antarc*
Antarctic
Greenland
Ice Sheet
Polar Research
op_source Polar Research; Vol 38 (2019)
1751-8369
op_relation https://polarresearch.net/index.php/polar/article/view/3498/9172
https://polarresearch.net/index.php/polar/article/view/3498/9173
https://polarresearch.net/index.php/polar/article/view/3498/9174
https://polarresearch.net/index.php/polar/article/view/3498/9176
https://polarresearch.net/index.php/polar/article/view/3498
doi:10.33265/polar.v38.3498
op_doi https://doi.org/10.33265/polar.v38.3498
container_title Polar Research
container_volume 38
container_issue 0
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