Measuring snow accumulation using ground-penetrating radar(GPR)
Ground-penetrating radar (GPR) is a non invasive geophysical method that uses radar pulses to image the subsurface. GPR can be used in a variety of media, including rock, soil, ice, fresh water, pavements and structures. In polar ice sheets, snow accumulation is transported by ice flow to outlet ice...
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University of Canterbury
2013
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ftunivcanter:oai:ir.canterbury.ac.nz:10092/13875 2023-05-15T16:40:53+02:00 Measuring snow accumulation using ground-penetrating radar(GPR) Hogarth, Kathy 2013 application/pdf http://hdl.handle.net/10092/13875 English en eng University of Canterbury http://hdl.handle.net/10092/13875 All Rights Reserved Theses / Dissertations 2013 ftunivcanter 2022-09-08T13:40:19Z Ground-penetrating radar (GPR) is a non invasive geophysical method that uses radar pulses to image the subsurface. GPR can be used in a variety of media, including rock, soil, ice, fresh water, pavements and structures. In polar ice sheets, snow accumulation is transported by ice flow to outlet ice streams and glaciers and/or ice shelves. Time scales for this transport can vary up to 105 years depending on the physical processes operating within the ice sheets. Therefore understanding of the internal physical processes, internal structure and flow regime is of great importance for understanding past, present, and future changes of the ice sheet. Radar is an established geophysical technique that has been and continues to be applied to investigate a variety of ice mass properties. This review presents the evolution of the technique from its early inception to the modern currently used Ground penetrating Radar (GPR) systems in the application of primarily measuring snow accumulation in Polar Regions. Other/Unknown Material Ice Sheet Ice Shelves University of Canterbury, Christchurch: UC Research Repository |
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Open Polar |
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University of Canterbury, Christchurch: UC Research Repository |
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ftunivcanter |
language |
English |
description |
Ground-penetrating radar (GPR) is a non invasive geophysical method that uses radar pulses to image the subsurface. GPR can be used in a variety of media, including rock, soil, ice, fresh water, pavements and structures. In polar ice sheets, snow accumulation is transported by ice flow to outlet ice streams and glaciers and/or ice shelves. Time scales for this transport can vary up to 105 years depending on the physical processes operating within the ice sheets. Therefore understanding of the internal physical processes, internal structure and flow regime is of great importance for understanding past, present, and future changes of the ice sheet. Radar is an established geophysical technique that has been and continues to be applied to investigate a variety of ice mass properties. This review presents the evolution of the technique from its early inception to the modern currently used Ground penetrating Radar (GPR) systems in the application of primarily measuring snow accumulation in Polar Regions. |
format |
Other/Unknown Material |
author |
Hogarth, Kathy |
spellingShingle |
Hogarth, Kathy Measuring snow accumulation using ground-penetrating radar(GPR) |
author_facet |
Hogarth, Kathy |
author_sort |
Hogarth, Kathy |
title |
Measuring snow accumulation using ground-penetrating radar(GPR) |
title_short |
Measuring snow accumulation using ground-penetrating radar(GPR) |
title_full |
Measuring snow accumulation using ground-penetrating radar(GPR) |
title_fullStr |
Measuring snow accumulation using ground-penetrating radar(GPR) |
title_full_unstemmed |
Measuring snow accumulation using ground-penetrating radar(GPR) |
title_sort |
measuring snow accumulation using ground-penetrating radar(gpr) |
publisher |
University of Canterbury |
publishDate |
2013 |
url |
http://hdl.handle.net/10092/13875 |
genre |
Ice Sheet Ice Shelves |
genre_facet |
Ice Sheet Ice Shelves |
op_relation |
http://hdl.handle.net/10092/13875 |
op_rights |
All Rights Reserved |
_version_ |
1766031313543888896 |