Glacier radar sounding using multiple-frequency bands

Svein-Erik Hamran; Jon Ove Hagen; Rune S. Odegard

doi:10.1117/12.383566

27 April 2000 Glacier radar sounding using multiple-frequency bands

Svein-Erik Hamran, Jon Ove Hagen, Rune S. Odegard

Proceedings Volume 4084, Eighth International Conference on Ground Penetrating Radar; (2000) https://doi.org/10.1117/12.383566
Event: 8th International Conference on Ground Penetrating Radar, 2000, Gold Coast, Australia

Abstract

A glacier consists of physical structures covering a large span of length scales. The different scales can be mapped using different radar frequencies. The bottom topography is mapped using HF frequencies (5 - 20 MHz). The internal structure is seen at UHF frequencies (100 - 500 MHz). The snow cover and firn layers can be mapped with frequencies around 1 GHz.

Citation Download Citation

Svein-Erik Hamran, Jon Ove Hagen, and Rune S. Odegard "Glacier radar sounding using multiple-frequency bands", Proc. SPIE 4084, Eighth International Conference on Ground Penetrating Radar, (27 April 2000); https://doi.org/10.1117/12.383566

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