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...

Full description

Bibliographic Details
Main Authors: Bianchi, C., Forieri, A., Tabacco, I. E.
Other Authors: Bianchi, C.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Forieri, A.; Sezione Geofisica, Università di Milano, Via Cicognara 7, I-20129 Milan, Italy, Tabacco, I. E.; Sezione Geofisica, Università di Milano, Via Cicognara 7, I-20129 Milan, Italy, Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia, Sezione Geofisica, Università di Milano, Via Cicognara 7, I-20129 Milan, Italy
Format: Article in Journal/Newspaper
Language:English
Published: International Glaciological Society 2004
Subjects:
Online Access:http://hdl.handle.net/2122/4178
Description
Summary: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. Published 9-12 3.8. Geofisica per l'ambiente JCR Journal reserved