Basal Roughness at Upper Thwaites Glacier

The basal roughness of glaciers and ice sheets is an important parameter controlling ice flow. Ice will generally slide faster over a smoother bed than a rougher one, but the horizontal scale of roughness is as important as its amplitude. Studies of basal roughness to date have used airborne radar d...

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Main Author: Boon, Xiang Ying Rebecca
Other Authors: Sridhar Anandakrishnan
Format: Text
Language:English
Published: Penn State 2011
Subjects:
Online Access:http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-6516/index.html
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spelling ftpennstate:OAI:PSUETD:ETD-6516 2023-05-15T13:36:40+02:00 Basal Roughness at Upper Thwaites Glacier Boon, Xiang Ying Rebecca Sridhar Anandakrishnan 2011-08-13 application/pdf http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-6516/index.html en eng Penn State WorldWide Copyright information available at source archive http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-6516/index.html Geoscience text 2011 ftpennstate 2011-09-13T09:04:36Z The basal roughness of glaciers and ice sheets is an important parameter controlling ice flow. Ice will generally slide faster over a smoother bed than a rougher one, but the horizontal scale of roughness is as important as its amplitude. Studies of basal roughness to date have used airborne radar data, which capture kilometer-scale roughness well, but for which it is challenging to resolve the smaller-scale roughness that is likely more important to ice flow. Here we present the results of a ground-based radar survey to study basal roughness on the scale of 10s to 100s of meters, and relate these observations to basal conditions. The data are from Thwaites Glacier, West Antarctica, one of the largest and fastest-flowing outlet glaciers on the continent, as well as one that is thinning rapidly and contributing to sea-level rise. We assess the value of different methods for quantitatively characterizing roughness using radar data, including bed-echo intensities, along-track root-mean-square (RMS) deviation of the basal topography, and spectral and wavelet analysis of the basal topography. We find that roughness is greater across-flow than along-flow, and greater downstream than upstream in our study area. This spatial organization results from a combination of pre-existing topography and glacial erosion. The multi-method analysis allows us to robustly characterize basal roughness in our study area. We correlate our results with existing models of greater basal shear stress downstream, and infer the presence of subglacial water. Finally, we clarify the nature of the relationship between basal conditions and roughness and relate our findings to those of similar studies. Text Antarc* Antarctica Thwaites Glacier West Antarctica PennState: Electronic Theses and Dissertations (eTD) Thwaites Glacier ENVELOPE(-106.750,-106.750,-75.500,-75.500) West Antarctica
institution Open Polar
collection PennState: Electronic Theses and Dissertations (eTD)
op_collection_id ftpennstate
language English
topic Geoscience
spellingShingle Geoscience
Boon, Xiang Ying Rebecca
Basal Roughness at Upper Thwaites Glacier
topic_facet Geoscience
description The basal roughness of glaciers and ice sheets is an important parameter controlling ice flow. Ice will generally slide faster over a smoother bed than a rougher one, but the horizontal scale of roughness is as important as its amplitude. Studies of basal roughness to date have used airborne radar data, which capture kilometer-scale roughness well, but for which it is challenging to resolve the smaller-scale roughness that is likely more important to ice flow. Here we present the results of a ground-based radar survey to study basal roughness on the scale of 10s to 100s of meters, and relate these observations to basal conditions. The data are from Thwaites Glacier, West Antarctica, one of the largest and fastest-flowing outlet glaciers on the continent, as well as one that is thinning rapidly and contributing to sea-level rise. We assess the value of different methods for quantitatively characterizing roughness using radar data, including bed-echo intensities, along-track root-mean-square (RMS) deviation of the basal topography, and spectral and wavelet analysis of the basal topography. We find that roughness is greater across-flow than along-flow, and greater downstream than upstream in our study area. This spatial organization results from a combination of pre-existing topography and glacial erosion. The multi-method analysis allows us to robustly characterize basal roughness in our study area. We correlate our results with existing models of greater basal shear stress downstream, and infer the presence of subglacial water. Finally, we clarify the nature of the relationship between basal conditions and roughness and relate our findings to those of similar studies.
author2 Sridhar Anandakrishnan
format Text
author Boon, Xiang Ying Rebecca
author_facet Boon, Xiang Ying Rebecca
author_sort Boon, Xiang Ying Rebecca
title Basal Roughness at Upper Thwaites Glacier
title_short Basal Roughness at Upper Thwaites Glacier
title_full Basal Roughness at Upper Thwaites Glacier
title_fullStr Basal Roughness at Upper Thwaites Glacier
title_full_unstemmed Basal Roughness at Upper Thwaites Glacier
title_sort basal roughness at upper thwaites glacier
publisher Penn State
publishDate 2011
url http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-6516/index.html
long_lat ENVELOPE(-106.750,-106.750,-75.500,-75.500)
geographic Thwaites Glacier
West Antarctica
geographic_facet Thwaites Glacier
West Antarctica
genre Antarc*
Antarctica
Thwaites Glacier
West Antarctica
genre_facet Antarc*
Antarctica
Thwaites Glacier
West Antarctica
op_source http://etda.libraries.psu.edu/theses/approved/WorldWideIndex/ETD-6516/index.html
op_rights WorldWide
Copyright information available at source archive
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