High frequency GPR measurements in comparison to detailed snow profiles
Snow stratigraphy in Antarctica is strongly influenced by wind. This results in a complex stratigraphy. Yearly accumulation is often masked by intermediate erosion and deposition events. Kohnen-Station has a higher accu- mulation than the very low accumulation areas of East Antarctica, and therefore...
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ftawi:oai:epic.awi.de:37204 2024-09-15T17:47:06+00:00 High frequency GPR measurements in comparison to detailed snow profiles Kreitmeier, Lisa Weißbach, Stefanie Schneebeli, Martin 2014-04-30 https://epic.awi.de/id/eprint/37204/ https://hdl.handle.net/10013/epic.44892 unknown Kreitmeier, L. , Weißbach, S. and Schneebeli, M. (2014) High frequency GPR measurements in comparison to detailed snow profiles , EGU General Assembly 2014, Vienna, Austria, 27 April 2014 - 2 May 2014 . hdl:10013/epic.44892 EPIC3EGU General Assembly 2014, Vienna, Austria, 2014-04-27-2014-05-02 Conference notRev 2014 ftawi 2024-06-24T04:11:05Z Snow stratigraphy in Antarctica is strongly influenced by wind. This results in a complex stratigraphy. Yearly accumulation is often masked by intermediate erosion and deposition events. Kohnen-Station has a higher accu- mulation than the very low accumulation areas of East Antarctica, and therefore is suited to investigate complex stratigraphy. Here we use very high frequency GPR at 1.6 GHz to resolve stratigraphy. We compared the GPR mea- surements with detailed snow profiles measured using near-infrared photography and translucent profiles. Detailed depositional features, as dunes and cross-bedding are visible. First results show very complex patterns, which are not easily correlated to other features, and not necessarily to yearly accumulation. Conference Object Antarc* Antarctica East Antarctica Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) |
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ftawi |
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unknown |
description |
Snow stratigraphy in Antarctica is strongly influenced by wind. This results in a complex stratigraphy. Yearly accumulation is often masked by intermediate erosion and deposition events. Kohnen-Station has a higher accu- mulation than the very low accumulation areas of East Antarctica, and therefore is suited to investigate complex stratigraphy. Here we use very high frequency GPR at 1.6 GHz to resolve stratigraphy. We compared the GPR mea- surements with detailed snow profiles measured using near-infrared photography and translucent profiles. Detailed depositional features, as dunes and cross-bedding are visible. First results show very complex patterns, which are not easily correlated to other features, and not necessarily to yearly accumulation. |
format |
Conference Object |
author |
Kreitmeier, Lisa Weißbach, Stefanie Schneebeli, Martin |
spellingShingle |
Kreitmeier, Lisa Weißbach, Stefanie Schneebeli, Martin High frequency GPR measurements in comparison to detailed snow profiles |
author_facet |
Kreitmeier, Lisa Weißbach, Stefanie Schneebeli, Martin |
author_sort |
Kreitmeier, Lisa |
title |
High frequency GPR measurements in comparison to detailed snow profiles |
title_short |
High frequency GPR measurements in comparison to detailed snow profiles |
title_full |
High frequency GPR measurements in comparison to detailed snow profiles |
title_fullStr |
High frequency GPR measurements in comparison to detailed snow profiles |
title_full_unstemmed |
High frequency GPR measurements in comparison to detailed snow profiles |
title_sort |
high frequency gpr measurements in comparison to detailed snow profiles |
publishDate |
2014 |
url |
https://epic.awi.de/id/eprint/37204/ https://hdl.handle.net/10013/epic.44892 |
genre |
Antarc* Antarctica East Antarctica |
genre_facet |
Antarc* Antarctica East Antarctica |
op_source |
EPIC3EGU General Assembly 2014, Vienna, Austria, 2014-04-27-2014-05-02 |
op_relation |
Kreitmeier, L. , Weißbach, S. and Schneebeli, M. (2014) High frequency GPR measurements in comparison to detailed snow profiles , EGU General Assembly 2014, Vienna, Austria, 27 April 2014 - 2 May 2014 . hdl:10013/epic.44892 |
_version_ |
1810495704781553664 |