Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity
We present a technique that modifies and extends down-hole target methods to provide absolute measures of uncertainty in radar-reflector depth of origin. We use ice-core profiles to model wave propagation and reflection, and then cross-correlate the model results with radio-echo sounding (RES) data...
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ftunivbern:oai:boris.unibe.ch:158681 2023-08-20T04:00:31+02:00 Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity Eisen, Olaf Wilhelms, Frank Steinhage, Daniel Schwander, Jakob 2006 application/pdf https://boris.unibe.ch/158681/1/improved-method-to-determine-radio-echo-sounding-reflector-depths-from-ice-core-profiles-of-permittivity-and-conductivity.pdf https://boris.unibe.ch/158681/ eng eng International Glaciological Society https://boris.unibe.ch/158681/ info:eu-repo/semantics/restrictedAccess Eisen, Olaf; Wilhelms, Frank; Steinhage, Daniel; Schwander, Jakob (2006). Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity. Journal of glaciology, 52(177), pp. 299-310. International Glaciological Society 10.3189/172756506781828674 <http://dx.doi.org/10.3189/172756506781828674> 530 Physics info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion PeerReviewed 2006 ftunivbern https://doi.org/10.3189/172756506781828674 2023-07-31T22:08:15Z We present a technique that modifies and extends down-hole target methods to provide absolute measures of uncertainty in radar-reflector depth of origin. We use ice-core profiles to model wave propagation and reflection, and then cross-correlate the model results with radio-echo sounding (RES) data to identify the depth of reflector events. Stacked traces recorded with RES near the EPICA drill site in Dronning Maud Land, Antarctica, provide reference radargrams, and dielectric properties along the deep ice core form the input data to a forward model of wave propagation that produces synthetic radargrams. Cross-correlations between synthetic and RES radargrams identify differences in propagation wave speed. They are attributed to uncertainties in pure-ice permittivity and are used for calibration. Removing conductivity peaks results in the disappearance of related synthetic reflections and enables the unambiguous relation of electric signatures to RES features. We find that (i) density measurements with g-attenuation or dielectric profiling are too noisy below the firn–ice transition to allow clear identification of reflections, (ii) single conductivity peaks less than 0.5 m wide cause the majority of prominent reflections beyond a travel time of about 10 µs (~900m depth) and (iii) some closely spaced conductivity peaks within a range of 1–2m cannot be resolved within the RES or synthetic data. Our results provide a depth accuracy to allow synchronization of age–depth profiles of ice cores by RES, modeling of isochronous internal structures, and determination of wave speed and of pure-ice properties. The technique successfully operates with dielectric profiling and electrical conductivity measurements, suggesting that it can be applied at other ice cores and drill sites. Article in Journal/Newspaper Antarc* Antarctica Dronning Maud Land EPICA ice core Journal of Glaciology BORIS (Bern Open Repository and Information System, University of Bern) Dronning Maud Land Journal of Glaciology 52 177 299 310 |
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Open Polar |
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BORIS (Bern Open Repository and Information System, University of Bern) |
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ftunivbern |
language |
English |
topic |
530 Physics |
spellingShingle |
530 Physics Eisen, Olaf Wilhelms, Frank Steinhage, Daniel Schwander, Jakob Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity |
topic_facet |
530 Physics |
description |
We present a technique that modifies and extends down-hole target methods to provide absolute measures of uncertainty in radar-reflector depth of origin. We use ice-core profiles to model wave propagation and reflection, and then cross-correlate the model results with radio-echo sounding (RES) data to identify the depth of reflector events. Stacked traces recorded with RES near the EPICA drill site in Dronning Maud Land, Antarctica, provide reference radargrams, and dielectric properties along the deep ice core form the input data to a forward model of wave propagation that produces synthetic radargrams. Cross-correlations between synthetic and RES radargrams identify differences in propagation wave speed. They are attributed to uncertainties in pure-ice permittivity and are used for calibration. Removing conductivity peaks results in the disappearance of related synthetic reflections and enables the unambiguous relation of electric signatures to RES features. We find that (i) density measurements with g-attenuation or dielectric profiling are too noisy below the firn–ice transition to allow clear identification of reflections, (ii) single conductivity peaks less than 0.5 m wide cause the majority of prominent reflections beyond a travel time of about 10 µs (~900m depth) and (iii) some closely spaced conductivity peaks within a range of 1–2m cannot be resolved within the RES or synthetic data. Our results provide a depth accuracy to allow synchronization of age–depth profiles of ice cores by RES, modeling of isochronous internal structures, and determination of wave speed and of pure-ice properties. The technique successfully operates with dielectric profiling and electrical conductivity measurements, suggesting that it can be applied at other ice cores and drill sites. |
format |
Article in Journal/Newspaper |
author |
Eisen, Olaf Wilhelms, Frank Steinhage, Daniel Schwander, Jakob |
author_facet |
Eisen, Olaf Wilhelms, Frank Steinhage, Daniel Schwander, Jakob |
author_sort |
Eisen, Olaf |
title |
Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity |
title_short |
Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity |
title_full |
Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity |
title_fullStr |
Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity |
title_full_unstemmed |
Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity |
title_sort |
improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity |
publisher |
International Glaciological Society |
publishDate |
2006 |
url |
https://boris.unibe.ch/158681/1/improved-method-to-determine-radio-echo-sounding-reflector-depths-from-ice-core-profiles-of-permittivity-and-conductivity.pdf https://boris.unibe.ch/158681/ |
geographic |
Dronning Maud Land |
geographic_facet |
Dronning Maud Land |
genre |
Antarc* Antarctica Dronning Maud Land EPICA ice core Journal of Glaciology |
genre_facet |
Antarc* Antarctica Dronning Maud Land EPICA ice core Journal of Glaciology |
op_source |
Eisen, Olaf; Wilhelms, Frank; Steinhage, Daniel; Schwander, Jakob (2006). Improved method to determine radio-echo sounding reflector depths from ice-core profiles of permittivity and conductivity. Journal of glaciology, 52(177), pp. 299-310. International Glaciological Society 10.3189/172756506781828674 <http://dx.doi.org/10.3189/172756506781828674> |
op_relation |
https://boris.unibe.ch/158681/ |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.3189/172756506781828674 |
container_title |
Journal of Glaciology |
container_volume |
52 |
container_issue |
177 |
container_start_page |
299 |
op_container_end_page |
310 |
_version_ |
1774718647619551232 |