GPR as an effective tool for safety and glacier characterization: experiences and future development

In recent times, the GPR technique has assumed an important role in glacial environment exploration. Ice thickness, bedrock description, internal water floods or underground channel, glacial structures (as snow layering and crevasses detection) form part of our experience in Antarctica and in high a...

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Published in:Proceedings of the XIII Internarional Conference on Ground Penetrating Radar
Main Authors: Urbini, S., Baskaradas, J. A.
Other Authors: Urbini, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Baskaradas, J. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Format: Article in Journal/Newspaper
Language:English
Published: IEEE 2010
Subjects:
GPR
snow layering
Antarctica
alpine glaciers
crevasses
water channels
02. Cryosphere::02.02. Glaciers::02.02.10. Instruments and techniques
Antarc*
Online Access:http://hdl.handle.net/2122/6244
https://doi.org/10.1109/ICGPR.2010.5550268
id ftingv:oai:www.earth-prints.org:2122/6244
record_format openpolar
spelling ftingv:oai:www.earth-prints.org:2122/6244 2023-05-15T14:01:36+02:00 GPR as an effective tool for safety and glacier characterization: experiences and future development Urbini, S. Baskaradas, J. A. Urbini, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Baskaradas, J. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia 2010-08 http://hdl.handle.net/2122/6244 https://doi.org/10.1109/ICGPR.2010.5550268 en eng IEEE IEEE Xplore / (2010) [1] S.A. Arcone, V.B. Spikes, G.S.Hamilton “Stratigraphic variation within polar firn caused by differential accumulation and ice flow: interpretation of a 400 MHz short-pulse radar profile from West Antarctica” J. Glaciol., Vol. 51, No. 174, pp. 407-422, 2005 [2] S. Fujita and 6 others “ Nature of radio-echo layering in the Antarctic ice sheet detected by a two-frequency experiment” J. Geophys. Res., 104 (B6), 13.013-13.024, 1999. [3] S. Urbini, L. Vittuari, S. Gandolfi “GPR and GPS data integration:examples of application in Antarctica”, Ann. Geofis., 44(4), pp. 687-702, 2001. [4] M. Frezzotti, S. Urbini, M. Proposito, C. Scarchilli, S. Gandolfi “Spatial and temporal variability of surface mass balance near Talos Dome, East Antarctica”, J. Geoph. Res.,112 (F02032), 2006, DOI:10.1029/2006JF000638. [5] S. Urbini, M. Frezzotti, S. Gandolfi, C. Vincent, C. Scarchilli, L. Vittuari, M. Fily “ Historical behaviour of Dome C and Talos Dome (East Antarctica) as investigated by snow accumulation and ice velocity measurements”, Global and Planetary Change, Vol. 60 (2008), pp. 576-588 [6] J. M Glover, and H. V. Rees, “Radar investigations of fim structures and crevasses,” in Geological Survey of Canada Paper 904, “Ground Penetrating Radar,” J.A. Pilon, Ed. Dept. of Energy, Mines and Resources, Ottawa, Ont., 1992, pp. 75-84. [7] A.J. Delaney, S.A. Arcone, A.O’Bannon and J. Wright, “Crevasse detection with GPR across the Ross Ice Shelf, Antarctica”, Tenth International Conference on Ground Penetrating Radar (2004), Delft, Netherlands [8] K. Eder, C. Reidler, C. Mayer and M. Leopold , “Crevasse Detection In Alpine Areas Using Ground Penetrating Radar As A Component For A Mountain Guide System”, The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B8. Beijing 2008 [9] A. Zirizzotti , J.A.Baskaradas , C. Bianchi ,U. Sciacca, I. E. Tabacco and E. Zuccheretti, “Glacio RADAR system and results”, IEEE Aerospace and Electronics Systems Society, (AESS), 26-May-2008 [10] D.J. Daniels, “Surface Penetrating Radar”, The Institution of Electrical Engineers,1996. [11] Kim, J.-H., Cho, S.-J. and Yi,M.-J. “,Removal of ringing noise in GPR data by signal processing”, Geosciences Journal,75-81, March 2007 http://hdl.handle.net/2122/6244 doi:10.1109/ICGPR.2010.5550268 restricted GPR snow layering Antarctica alpine glaciers crevasses water channels 02. Cryosphere::02.02. Glaciers::02.02.10. Instruments and techniques article 2010 ftingv https://doi.org/10.1109/ICGPR.2010.5550268 https://doi.org/10.1029/2006JF000638 2022-07-29T06:05:41Z In recent times, the GPR technique has assumed an important role in glacial environment exploration. Ice thickness, bedrock description, internal water floods or underground channel, glacial structures (as snow layering and crevasses detection) form part of our experience in Antarctica and in high alpine glacier ski areas. In this paper, we present some results of these investigations exploring the possibility of combining our technical expertise on Radio Echo Sounding (RES) instrumentation to develop a system for subglacial environment exploration. Published 1-6 1.8. Osservazioni di geofisica ambientale 3.8. Geofisica per l'ambiente N/A or not JCR restricted Article in Journal/Newspaper Antarc* Antarctica Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia) Proceedings of the XIII Internarional Conference on Ground Penetrating Radar 1 6
institution Open Polar
collection Earth-Prints (Istituto Nazionale di Geofisica e Vulcanologia)
op_collection_id ftingv
language English
topic GPR
snow layering
Antarctica
alpine glaciers
crevasses
water channels
02. Cryosphere::02.02. Glaciers::02.02.10. Instruments and techniques
spellingShingle GPR
snow layering
Antarctica
alpine glaciers
crevasses
water channels
02. Cryosphere::02.02. Glaciers::02.02.10. Instruments and techniques
Urbini, S.
Baskaradas, J. A.
GPR as an effective tool for safety and glacier characterization: experiences and future development
topic_facet GPR
snow layering
Antarctica
alpine glaciers
crevasses
water channels
02. Cryosphere::02.02. Glaciers::02.02.10. Instruments and techniques
description In recent times, the GPR technique has assumed an important role in glacial environment exploration. Ice thickness, bedrock description, internal water floods or underground channel, glacial structures (as snow layering and crevasses detection) form part of our experience in Antarctica and in high alpine glacier ski areas. In this paper, we present some results of these investigations exploring the possibility of combining our technical expertise on Radio Echo Sounding (RES) instrumentation to develop a system for subglacial environment exploration. Published 1-6 1.8. Osservazioni di geofisica ambientale 3.8. Geofisica per l'ambiente N/A or not JCR restricted
author2 Urbini, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Baskaradas, J. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia
format Article in Journal/Newspaper
author Urbini, S.
Baskaradas, J. A.
author_facet Urbini, S.
Baskaradas, J. A.
author_sort Urbini, S.
title GPR as an effective tool for safety and glacier characterization: experiences and future development
title_short GPR as an effective tool for safety and glacier characterization: experiences and future development
title_full GPR as an effective tool for safety and glacier characterization: experiences and future development
title_fullStr GPR as an effective tool for safety and glacier characterization: experiences and future development
title_full_unstemmed GPR as an effective tool for safety and glacier characterization: experiences and future development
title_sort gpr as an effective tool for safety and glacier characterization: experiences and future development
publisher IEEE
publishDate 2010
url http://hdl.handle.net/2122/6244
https://doi.org/10.1109/ICGPR.2010.5550268
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation IEEE Xplore
/ (2010)
[1] S.A. Arcone, V.B. Spikes, G.S.Hamilton “Stratigraphic variation within polar firn caused by differential accumulation and ice flow: interpretation of a 400 MHz short-pulse radar profile from West Antarctica” J. Glaciol., Vol. 51, No. 174, pp. 407-422, 2005 [2] S. Fujita and 6 others “ Nature of radio-echo layering in the Antarctic ice sheet detected by a two-frequency experiment” J. Geophys. Res., 104 (B6), 13.013-13.024, 1999. [3] S. Urbini, L. Vittuari, S. Gandolfi “GPR and GPS data integration:examples of application in Antarctica”, Ann. Geofis., 44(4), pp. 687-702, 2001. [4] M. Frezzotti, S. Urbini, M. Proposito, C. Scarchilli, S. Gandolfi “Spatial and temporal variability of surface mass balance near Talos Dome, East Antarctica”, J. Geoph. Res.,112 (F02032), 2006, DOI:10.1029/2006JF000638. [5] S. Urbini, M. Frezzotti, S. Gandolfi, C. Vincent, C. Scarchilli, L. Vittuari, M. Fily “ Historical behaviour of Dome C and Talos Dome (East Antarctica) as investigated by snow accumulation and ice velocity measurements”, Global and Planetary Change, Vol. 60 (2008), pp. 576-588 [6] J. M Glover, and H. V. Rees, “Radar investigations of fim structures and crevasses,” in Geological Survey of Canada Paper 904, “Ground Penetrating Radar,” J.A. Pilon, Ed. Dept. of Energy, Mines and Resources, Ottawa, Ont., 1992, pp. 75-84. [7] A.J. Delaney, S.A. Arcone, A.O’Bannon and J. Wright, “Crevasse detection with GPR across the Ross Ice Shelf, Antarctica”, Tenth International Conference on Ground Penetrating Radar (2004), Delft, Netherlands [8] K. Eder, C. Reidler, C. Mayer and M. Leopold , “Crevasse Detection In Alpine Areas Using Ground Penetrating Radar As A Component For A Mountain Guide System”, The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences. Vol. XXXVII. Part B8. Beijing 2008 [9] A. Zirizzotti , J.A.Baskaradas , C. Bianchi ,U. Sciacca, I. E. Tabacco and E. Zuccheretti, “Glacio RADAR system and results”, IEEE Aerospace and Electronics Systems Society, (AESS), 26-May-2008 [10] D.J. Daniels, “Surface Penetrating Radar”, The Institution of Electrical Engineers,1996. [11] Kim, J.-H., Cho, S.-J. and Yi,M.-J. “,Removal of ringing noise in GPR data by signal processing”, Geosciences Journal,75-81, March 2007
http://hdl.handle.net/2122/6244
doi:10.1109/ICGPR.2010.5550268
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