GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice
Snow thickness on sea ice is not known on the regional scales and to the accuracy requiredfor climate analysis and to assess its significant role in the Earth's cryosphere mass balance.The thickness of snow on sea ice is a largely under-sampled, but crucially importantparameter when estimating...
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ftunivtasecite:oai:ecite.utas.edu.au:126032 2023-05-15T13:42:40+02:00 GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice Lieser, J Pfaffhuber, A Haas, C 2018 application/pdf http://ecite.utas.edu.au/126032 en eng . http://ecite.utas.edu.au/126032/1/Lieser_etal Polar 2018 - Abstract Submission System.pdf http://ecite.utas.edu.au/126032/2/Talk.pdf Lieser, J and Pfaffhuber, A and Haas, C, GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice, 35th SCAR Biennial Meetings, 19-23 June 2018, Davos, Switzerland, pp. 1. (2018) [Conference Extract] http://ecite.utas.edu.au/126032 Earth Sciences Physical geography and environmental geoscience Physical geography and environmental geoscience not elsewhere classified Conference Extract NonPeerReviewed 2018 ftunivtasecite 2022-11-07T23:17:14Z Snow thickness on sea ice is not known on the regional scales and to the accuracy requiredfor climate analysis and to assess its significant role in the Earth's cryosphere mass balance.The thickness of snow on sea ice is a largely under-sampled, but crucially importantparameter when estimating sea-ice thickness from space-borne sensors. Traditionalsampling methods comprise meter-stick measurements or snow probes, which yield highlyaccurate data but are sparse in space and time, whereas remote sensing data have thepotential to cover large areas but exhibit large uncertainties. To increase the local datavolume and to apply as an intermediate level for remote-sensing data validation, we presentnon-destructive ground-penetrating radar (GPR) snow-thickness data of remarkableaccuracy (millimetre to centimetre) when compared to in-situ data. The semi-regional datacollected during two Antarctic campaigns in late winter/early spring confirm theunderestimation of snow thickness on sea ice using remote-sensing methods by roughly30%. The radar wave propagation was found to be rather constant in snow (+/- 6%),supporting the applicability of GPR for regional snow thickness surveys of snow thicker than10cm, which was the detection limit of the off-the-shelf GPR setup used in this study. Conference Object Antarc* Antarctic Sea ice eCite UTAS (University of Tasmania) Antarctic |
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Earth Sciences Physical geography and environmental geoscience Physical geography and environmental geoscience not elsewhere classified |
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Earth Sciences Physical geography and environmental geoscience Physical geography and environmental geoscience not elsewhere classified Lieser, J Pfaffhuber, A Haas, C GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice |
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Earth Sciences Physical geography and environmental geoscience Physical geography and environmental geoscience not elsewhere classified |
description |
Snow thickness on sea ice is not known on the regional scales and to the accuracy requiredfor climate analysis and to assess its significant role in the Earth's cryosphere mass balance.The thickness of snow on sea ice is a largely under-sampled, but crucially importantparameter when estimating sea-ice thickness from space-borne sensors. Traditionalsampling methods comprise meter-stick measurements or snow probes, which yield highlyaccurate data but are sparse in space and time, whereas remote sensing data have thepotential to cover large areas but exhibit large uncertainties. To increase the local datavolume and to apply as an intermediate level for remote-sensing data validation, we presentnon-destructive ground-penetrating radar (GPR) snow-thickness data of remarkableaccuracy (millimetre to centimetre) when compared to in-situ data. The semi-regional datacollected during two Antarctic campaigns in late winter/early spring confirm theunderestimation of snow thickness on sea ice using remote-sensing methods by roughly30%. The radar wave propagation was found to be rather constant in snow (+/- 6%),supporting the applicability of GPR for regional snow thickness surveys of snow thicker than10cm, which was the detection limit of the off-the-shelf GPR setup used in this study. |
format |
Conference Object |
author |
Lieser, J Pfaffhuber, A Haas, C |
author_facet |
Lieser, J Pfaffhuber, A Haas, C |
author_sort |
Lieser, J |
title |
GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice |
title_short |
GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice |
title_full |
GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice |
title_fullStr |
GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice |
title_full_unstemmed |
GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice |
title_sort |
gpr for rapid and accurate snow-thickness measurements on antarctic sea ice |
publisher |
. |
publishDate |
2018 |
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http://ecite.utas.edu.au/126032 |
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Antarctic |
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Antarctic |
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Antarc* Antarctic Sea ice |
genre_facet |
Antarc* Antarctic Sea ice |
op_relation |
http://ecite.utas.edu.au/126032/1/Lieser_etal Polar 2018 - Abstract Submission System.pdf http://ecite.utas.edu.au/126032/2/Talk.pdf Lieser, J and Pfaffhuber, A and Haas, C, GPR for rapid and accurate snow-thickness measurements on Antarctic sea ice, 35th SCAR Biennial Meetings, 19-23 June 2018, Davos, Switzerland, pp. 1. (2018) [Conference Extract] http://ecite.utas.edu.au/126032 |
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