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Please use this identifier to cite or link to this item: http://hdl.handle.net/2122/6244
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dc.contributor.authorallUrbini, S.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.authorallBaskaradas, J. A.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.date.accessioned2010-11-16T10:54:27Zen
dc.date.available2010-11-16T10:54:27Zen
dc.date.issued2010-08en
dc.identifier.urihttp://hdl.handle.net/2122/6244en
dc.description.abstractIn 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.en
dc.language.isoEnglishen
dc.publisher.nameIEEEen
dc.relation.ispartofIEEE Xploreen
dc.relation.ispartofseries/ (2010)en
dc.subjectGPRen
dc.subjectsnow layeringen
dc.subjectAntarcticaen
dc.subjectalpine glaciersen
dc.subjectcrevassesen
dc.subjectwater channelsen
dc.titleGPR as an effective tool for safety and glacier characterization: experiences and future developmenten
dc.typearticleen
dc.description.statusPublisheden
dc.description.pagenumber1-6en
dc.subject.INGV02. Cryosphere::02.02. Glaciers::02.02.10. Instruments and techniquesen
dc.identifier.doi10.1109/ICGPR.2010.5550268en
dc.relation.references[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 2007en
dc.description.obiettivoSpecifico1.8. Osservazioni di geofisica ambientaleen
dc.description.obiettivoSpecifico3.8. Geofisica per l'ambienteen
dc.description.journalTypeN/A or not JCRen
dc.description.fulltextrestricteden
dc.contributor.authorUrbini, S.en
dc.contributor.authorBaskaradas, J. A.en
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
dc.contributor.departmentIstituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italiaen
item.openairetypearticle-
item.cerifentitytypePublications-
item.languageiso639-1en-
item.grantfulltextrestricted-
item.openairecristypehttp://purl.org/coar/resource_type/c_18cf-
item.fulltextWith Fulltext-
crisitem.author.deptIstituto Nazionale di Geofisica e Vulcanologia (INGV), Sezione Roma2, Roma, Italia-
crisitem.author.deptSAP, School of Electrical and Electronics Engineering-
crisitem.author.orcid0000-0002-8053-4197-
crisitem.author.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.classification.parent02. Cryosphere-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
crisitem.department.parentorgIstituto Nazionale di Geofisica e Vulcanologia-
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