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...
Main Authors: | , , |
---|---|
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
International Glaciological Society
2004
|
Subjects: | |
Online Access: | http://hdl.handle.net/2434/11697 |
_version_ | 1821758685867671552 |
---|---|
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 |