The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ...
Ice stream bed topography contains key evidence for the ways ice streams interact with, and are potentially controlled by, their beds. Here we present the first application of two-dimensional Fourier analysis to 22 marine and terrestrial topographies from 5 regions in Antarctica and Canada, with and...
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ftdatacite:10.17863/cam.12223 2024-02-27T08:35:19+00:00 The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ... Spagnolo, M Bartholomaus, TC Clark, CD Stokes, CR Atkinson, N Dowdeswell, JA Ely, JC Graham, AGC Hogan, KA King, EC Larter, RD Livingstone, SJ Pritchard, HD 2017 https://dx.doi.org/10.17863/cam.12223 https://www.repository.cam.ac.uk/handle/1810/267028 en eng AGU Publications open.access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 ice stream bed mega-scale glacial lineations period topography pattern topography Fourier article-journal ScholarlyArticle JournalArticle Article 2017 ftdatacite https://doi.org/10.17863/cam.12223 2024-02-01T14:57:25Z Ice stream bed topography contains key evidence for the ways ice streams interact with, and are potentially controlled by, their beds. Here we present the first application of two-dimensional Fourier analysis to 22 marine and terrestrial topographies from 5 regions in Antarctica and Canada, with and without mega-scale glacial lineations (MSGLs). We find that the topography of MSGL-rich ice stream sedimentary beds is characterized by multiple, periodic wavelengths between 300 and 1200 m and amplitudes from decimeters to a few meters. This periodic topography is consistent with the idea that instability is a key element to the formation of MSGL bedforms. Dominant wavelengths vary among locations and, on one paleo ice stream bed, increase along the direction of ice flow by 1.7 ± 0.52% km−1. We suggest that these changes are likely to reflect pattern evolution via downstream wavelength coarsening, even under potentially steady ice stream geometry and flow conditions. The amplitude of MSGLs is smaller than that ... Article in Journal/Newspaper Antarc* Antarctica DataCite Metadata Store (German National Library of Science and Technology) Canada |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
ice stream bed mega-scale glacial lineations period topography pattern topography Fourier |
spellingShingle |
ice stream bed mega-scale glacial lineations period topography pattern topography Fourier Spagnolo, M Bartholomaus, TC Clark, CD Stokes, CR Atkinson, N Dowdeswell, JA Ely, JC Graham, AGC Hogan, KA King, EC Larter, RD Livingstone, SJ Pritchard, HD The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ... |
topic_facet |
ice stream bed mega-scale glacial lineations period topography pattern topography Fourier |
description |
Ice stream bed topography contains key evidence for the ways ice streams interact with, and are potentially controlled by, their beds. Here we present the first application of two-dimensional Fourier analysis to 22 marine and terrestrial topographies from 5 regions in Antarctica and Canada, with and without mega-scale glacial lineations (MSGLs). We find that the topography of MSGL-rich ice stream sedimentary beds is characterized by multiple, periodic wavelengths between 300 and 1200 m and amplitudes from decimeters to a few meters. This periodic topography is consistent with the idea that instability is a key element to the formation of MSGL bedforms. Dominant wavelengths vary among locations and, on one paleo ice stream bed, increase along the direction of ice flow by 1.7 ± 0.52% km−1. We suggest that these changes are likely to reflect pattern evolution via downstream wavelength coarsening, even under potentially steady ice stream geometry and flow conditions. The amplitude of MSGLs is smaller than that ... |
format |
Article in Journal/Newspaper |
author |
Spagnolo, M Bartholomaus, TC Clark, CD Stokes, CR Atkinson, N Dowdeswell, JA Ely, JC Graham, AGC Hogan, KA King, EC Larter, RD Livingstone, SJ Pritchard, HD |
author_facet |
Spagnolo, M Bartholomaus, TC Clark, CD Stokes, CR Atkinson, N Dowdeswell, JA Ely, JC Graham, AGC Hogan, KA King, EC Larter, RD Livingstone, SJ Pritchard, HD |
author_sort |
Spagnolo, M |
title |
The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ... |
title_short |
The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ... |
title_full |
The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ... |
title_fullStr |
The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ... |
title_full_unstemmed |
The periodic topography of ice stream beds: Insights from the Fourier spectra of mega-scale glacial lineations ... |
title_sort |
periodic topography of ice stream beds: insights from the fourier spectra of mega-scale glacial lineations ... |
publisher |
AGU Publications |
publishDate |
2017 |
url |
https://dx.doi.org/10.17863/cam.12223 https://www.repository.cam.ac.uk/handle/1810/267028 |
geographic |
Canada |
geographic_facet |
Canada |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_rights |
open.access Creative Commons Attribution 4.0 International Creative Commons Attribution 4.0 International Attribution 4.0 International Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.12223 |
_version_ |
1792041811037913088 |