Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn

Abstract Radio-echo signals travel faster in firn than in ice, which affects the analysis of ice-mass thickness. If this effect is neglected, then the calculated thickness of an ice mass may be in error by an amount of the order of one-tenth of the firn thickness. An exact formulation is derived for...

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Published in:Journal of Glaciology
Main Author: Rasmussen, L. A.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1986
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000015501
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015501
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spelling crcambridgeupr:10.1017/s0022143000015501 2024-03-03T08:46:09+00:00 Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn Rasmussen, L. A. 1986 http://dx.doi.org/10.1017/s0022143000015501 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015501 en eng Cambridge University Press (CUP) Journal of Glaciology volume 32, issue 111, page 192-194 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1986 crcambridgeupr https://doi.org/10.1017/s0022143000015501 2024-02-08T08:38:15Z Abstract Radio-echo signals travel faster in firn than in ice, which affects the analysis of ice-mass thickness. If this effect is neglected, then the calculated thickness of an ice mass may be in error by an amount of the order of one-tenth of the firn thickness. An exact formulation is derived for the path of the signal through the firn and the ice. Explicit solutions are given for constant, linear, and quadratic profiles of the refractive index in the firn layer. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 32 111 192 194
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Rasmussen, L. A.
Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn
topic_facet Earth-Surface Processes
description Abstract Radio-echo signals travel faster in firn than in ice, which affects the analysis of ice-mass thickness. If this effect is neglected, then the calculated thickness of an ice mass may be in error by an amount of the order of one-tenth of the firn thickness. An exact formulation is derived for the path of the signal through the firn and the ice. Explicit solutions are given for constant, linear, and quadratic profiles of the refractive index in the firn layer.
format Article in Journal/Newspaper
author Rasmussen, L. A.
author_facet Rasmussen, L. A.
author_sort Rasmussen, L. A.
title Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn
title_short Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn
title_full Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn
title_fullStr Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn
title_full_unstemmed Refraction Correction for Radio Echo-Sounding of Ice Overlain by Firn
title_sort refraction correction for radio echo-sounding of ice overlain by firn
publisher Cambridge University Press (CUP)
publishDate 1986
url http://dx.doi.org/10.1017/s0022143000015501
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000015501
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 32, issue 111, page 192-194
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000015501
container_title Journal of Glaciology
container_volume 32
container_issue 111
container_start_page 192
op_container_end_page 194
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