Electromagnetic reflecting properties of sub ice surfaces

The power strength of the radio-echo signal coming from reflecting sub-ice surfaces is used to determine the nature of the reflecting surface, i.e. rock, water or sea water. Electromagnetic analysis shows that the amplitude variations detected by radio-echo sounding are mainly due to the nature of t...

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Bibliographic Details
Main Authors: C. Bianchi, A. Forieri, I. Tabacco
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2004
Subjects:
Online Access:http://hdl.handle.net/2434/11697
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author C. Bianchi
A. Forieri
I. Tabacco
author2 C. Bianchi
A. Forieri
I. Tabacco
author_facet C. Bianchi
A. Forieri
I. Tabacco
author_sort C. Bianchi
collection The University of Milan: Archivio Istituzionale della Ricerca (AIR)
description The power strength of the radio-echo signal coming from reflecting sub-ice surfaces is used to determine the nature of the reflecting surface, i.e. rock, water or sea water. Electromagnetic analysis shows that the amplitude variations detected by radio-echo sounding are mainly due to the nature of the interface as well as the concave or convex shape of the reflectors. In this paper, some relevant profiles showing the power variations due to the different nature of the interface and the shape of the reflectors are presented. These results are important both for surface shape determination and for subglacial lake detection.
format Article in Journal/Newspaper
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
id ftunivmilanoair:oai:air.unimi.it:2434/11697
institution Open Polar
language English
op_collection_id ftunivmilanoair
op_relation volume:39
firstpage:9
lastpage:12
journal:ANNALS OF GLACIOLOGY
http://hdl.handle.net/2434/11697
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-23844481430
publishDate 2004
publisher International Glaciological Society
record_format openpolar
spelling ftunivmilanoair:oai:air.unimi.it:2434/11697 2025-01-16T19:26:49+00:00 Electromagnetic reflecting properties of sub ice surfaces C. Bianchi A. Forieri I. Tabacco C. Bianchi A. Forieri I. Tabacco 2004 http://hdl.handle.net/2434/11697 eng eng International Glaciological Society volume:39 firstpage:9 lastpage:12 journal:ANNALS OF GLACIOLOGY http://hdl.handle.net/2434/11697 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-23844481430 radar instrumentation ice absorption Antarctica Settore GEO/11 - Geofisica Applicata info:eu-repo/semantics/article 2004 ftunivmilanoair 2024-01-09T23:19:58Z The power strength of the radio-echo signal coming from reflecting sub-ice surfaces is used to determine the nature of the reflecting surface, i.e. rock, water or sea water. Electromagnetic analysis shows that the amplitude variations detected by radio-echo sounding are mainly due to the nature of the interface as well as the concave or convex shape of the reflectors. In this paper, some relevant profiles showing the power variations due to the different nature of the interface and the shape of the reflectors are presented. These results are important both for surface shape determination and for subglacial lake detection. Article in Journal/Newspaper Antarc* Antarctica The University of Milan: Archivio Istituzionale della Ricerca (AIR)
spellingShingle radar instrumentation
ice absorption
Antarctica
Settore GEO/11 - Geofisica Applicata
C. Bianchi
A. Forieri
I. Tabacco
Electromagnetic reflecting properties of sub ice surfaces
title Electromagnetic reflecting properties of sub ice surfaces
title_full Electromagnetic reflecting properties of sub ice surfaces
title_fullStr Electromagnetic reflecting properties of sub ice surfaces
title_full_unstemmed Electromagnetic reflecting properties of sub ice surfaces
title_short Electromagnetic reflecting properties of sub ice surfaces
title_sort electromagnetic reflecting properties of sub ice surfaces
topic radar instrumentation
ice absorption
Antarctica
Settore GEO/11 - Geofisica Applicata
topic_facet radar instrumentation
ice absorption
Antarctica
Settore GEO/11 - Geofisica Applicata
url http://hdl.handle.net/2434/11697