A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica

The East Antarctic Ice Sheet (EAIS) is the largest source of potential sea-level rise, containing approximately 52 m of sea-level equivalent. To constrain estimates of sea-level rise into the future requires knowledge of ice-sheet properties and geometry and ice-penetrating radar offers a means to e...

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Main Authors: Abdul Salam, Syed, Roberts, Jason L., McCormack, Felicity S., Coleman, Richard, Halpin, Jacqueline A.
Format: Text
Language:English
Published: 2020
Subjects:
Online Access:https://doi.org/10.5194/essd-2020-146
https://essd.copernicus.org/preprints/essd-2020-146/
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spelling ftcopernicus:oai:publications.copernicus.org:essdd86199 2023-05-15T13:31:39+02:00 A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica Abdul Salam, Syed Roberts, Jason L. McCormack, Felicity S. Coleman, Richard Halpin, Jacqueline A. 2020-10-27 application/pdf https://doi.org/10.5194/essd-2020-146 https://essd.copernicus.org/preprints/essd-2020-146/ eng eng doi:10.5194/essd-2020-146 https://essd.copernicus.org/preprints/essd-2020-146/ eISSN: 1866-3516 Text 2020 ftcopernicus https://doi.org/10.5194/essd-2020-146 2020-11-02T17:22:14Z The East Antarctic Ice Sheet (EAIS) is the largest source of potential sea-level rise, containing approximately 52 m of sea-level equivalent. To constrain estimates of sea-level rise into the future requires knowledge of ice-sheet properties and geometry and ice-penetrating radar offers a means to estimate these properties (e.g. ice thickness, englacial temperatures). One of the regions that have been extensively surveyed using ice-penetrating radar from the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project in East Antarctica is Law Dome, a small independent ice cap situated to the west of Totten Ice Shelf. The ice cap is slow-moving, has a low melt-rate at the surface and moderate wind speeds, making it a useful study site for estimating the radar attenuation. A new method is proposed for the estimation of attenuation rate from radar data which is mathematically modelled as a constrained regularised l 2 minimisation problem. In the proposed method, only radar data is required and the englacial reflectors are automatically detected from the radar data itself. To validate our methodology, attenuation differences at flight crossover points are calculated and statistical analyses performed to assess the accuracy of the results. For spatial analyses, the errors are of the order 22.6 %, 15.2 %, and 32.8 % for mean absolute error, median absolute error, and root mean square error respectively. Also, for the depth analyses, up to the depth of 800 m, the errors are under 29.9 %, 24.2 %, and 38.8 % for mean absolute error, median absolute error, and root mean square error respectively. A final product of 3D attenuation rates and uncertainty estimates is provided. The generated dataset is publicly available at https://doi.org/10.25959/5e6851e266f4a (Abdul Salam, 2020). Text Antarc* Antarctic Antarctica East Antarctica Ice cap Ice Sheet Ice Shelf Totten Ice Shelf Copernicus Publications: E-Journals Antarctic East Antarctic Ice Sheet East Antarctica Law Dome ENVELOPE(112.833,112.833,-66.733,-66.733)
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description The East Antarctic Ice Sheet (EAIS) is the largest source of potential sea-level rise, containing approximately 52 m of sea-level equivalent. To constrain estimates of sea-level rise into the future requires knowledge of ice-sheet properties and geometry and ice-penetrating radar offers a means to estimate these properties (e.g. ice thickness, englacial temperatures). One of the regions that have been extensively surveyed using ice-penetrating radar from the Investigating the Cryospheric Evolution of the Central Antarctic Plate (ICECAP) project in East Antarctica is Law Dome, a small independent ice cap situated to the west of Totten Ice Shelf. The ice cap is slow-moving, has a low melt-rate at the surface and moderate wind speeds, making it a useful study site for estimating the radar attenuation. A new method is proposed for the estimation of attenuation rate from radar data which is mathematically modelled as a constrained regularised l 2 minimisation problem. In the proposed method, only radar data is required and the englacial reflectors are automatically detected from the radar data itself. To validate our methodology, attenuation differences at flight crossover points are calculated and statistical analyses performed to assess the accuracy of the results. For spatial analyses, the errors are of the order 22.6 %, 15.2 %, and 32.8 % for mean absolute error, median absolute error, and root mean square error respectively. Also, for the depth analyses, up to the depth of 800 m, the errors are under 29.9 %, 24.2 %, and 38.8 % for mean absolute error, median absolute error, and root mean square error respectively. A final product of 3D attenuation rates and uncertainty estimates is provided. The generated dataset is publicly available at https://doi.org/10.25959/5e6851e266f4a (Abdul Salam, 2020).
format Text
author Abdul Salam, Syed
Roberts, Jason L.
McCormack, Felicity S.
Coleman, Richard
Halpin, Jacqueline A.
spellingShingle Abdul Salam, Syed
Roberts, Jason L.
McCormack, Felicity S.
Coleman, Richard
Halpin, Jacqueline A.
A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica
author_facet Abdul Salam, Syed
Roberts, Jason L.
McCormack, Felicity S.
Coleman, Richard
Halpin, Jacqueline A.
author_sort Abdul Salam, Syed
title A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica
title_short A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica
title_full A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica
title_fullStr A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica
title_full_unstemmed A 3D map of englacial attenuation rate from radar reflections at Law Dome, East Antarctica
title_sort 3d map of englacial attenuation rate from radar reflections at law dome, east antarctica
publishDate 2020
url https://doi.org/10.5194/essd-2020-146
https://essd.copernicus.org/preprints/essd-2020-146/
long_lat ENVELOPE(112.833,112.833,-66.733,-66.733)
geographic Antarctic
East Antarctic Ice Sheet
East Antarctica
Law Dome
geographic_facet Antarctic
East Antarctic Ice Sheet
East Antarctica
Law Dome
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ice cap
Ice Sheet
Ice Shelf
Totten Ice Shelf
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ice cap
Ice Sheet
Ice Shelf
Totten Ice Shelf
op_source eISSN: 1866-3516
op_relation doi:10.5194/essd-2020-146
https://essd.copernicus.org/preprints/essd-2020-146/
op_doi https://doi.org/10.5194/essd-2020-146
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