Radio-echo layering in polar ice sheets ...
This thesis is concerned with layered reflections observed in the Antarctic and Greenland ice sheets during radio-echo sounding. It describes in detail layering seen with 60 and 300 MHz equipment _in the Antarctic ice sheet during three field seasons betwe~n 1974 and 1979, and discusses the effects...
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1981
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Online Access: | https://dx.doi.org/10.17863/cam.14157 https://www.repository.cam.ac.uk/handle/1810/268045 |
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ftdatacite:10.17863/cam.14157 2024-09-15T17:44:26+00:00 Radio-echo layering in polar ice sheets ... Millar, David H M 1981 https://dx.doi.org/10.17863/cam.14157 https://www.repository.cam.ac.uk/handle/1810/268045 en eng Apollo - University of Cambridge Repository open.access All Rights Reserved https://www.rioxx.net/licenses/all-rights-reserved/ http://purl.org/coar/access_right/c_abf2 Dissertation thesis Thesis 1981 ftdatacite https://doi.org/10.17863/cam.14157 2024-07-03T13:13:19Z This thesis is concerned with layered reflections observed in the Antarctic and Greenland ice sheets during radio-echo sounding. It describes in detail layering seen with 60 and 300 MHz equipment _in the Antarctic ice sheet during three field seasons betwe~n 1974 and 1979, and discusses the effects of glaciological and equipment factors, particularly radio pulse length. The effects of changing pulse length and accumulation rate on layer echo separation are analysed, and the importance of closely spaced groups of reflectors assessed. Reflection coefficient vs depth profiles are presented for layering observed at nearly twenty sites in the Antarctic and Greenland, and are used to demonstrate the existence of two separate reflection mechanisms: changes in (a) ice density, and (b) loss tangent. Supporting density and conductivity data from ice cores are summarised. It is concluded that most layer echoes arise from layers of ice containing acidic impurities of volcanic origin~ Layer reflectivity variations_are ... Thesis Antarc* Antarctic Greenland Ice Sheet DataCite |
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ftdatacite |
language |
English |
description |
This thesis is concerned with layered reflections observed in the Antarctic and Greenland ice sheets during radio-echo sounding. It describes in detail layering seen with 60 and 300 MHz equipment _in the Antarctic ice sheet during three field seasons betwe~n 1974 and 1979, and discusses the effects of glaciological and equipment factors, particularly radio pulse length. The effects of changing pulse length and accumulation rate on layer echo separation are analysed, and the importance of closely spaced groups of reflectors assessed. Reflection coefficient vs depth profiles are presented for layering observed at nearly twenty sites in the Antarctic and Greenland, and are used to demonstrate the existence of two separate reflection mechanisms: changes in (a) ice density, and (b) loss tangent. Supporting density and conductivity data from ice cores are summarised. It is concluded that most layer echoes arise from layers of ice containing acidic impurities of volcanic origin~ Layer reflectivity variations_are ... |
format |
Thesis |
author |
Millar, David H M |
spellingShingle |
Millar, David H M Radio-echo layering in polar ice sheets ... |
author_facet |
Millar, David H M |
author_sort |
Millar, David H M |
title |
Radio-echo layering in polar ice sheets ... |
title_short |
Radio-echo layering in polar ice sheets ... |
title_full |
Radio-echo layering in polar ice sheets ... |
title_fullStr |
Radio-echo layering in polar ice sheets ... |
title_full_unstemmed |
Radio-echo layering in polar ice sheets ... |
title_sort |
radio-echo layering in polar ice sheets ... |
publisher |
Apollo - University of Cambridge Repository |
publishDate |
1981 |
url |
https://dx.doi.org/10.17863/cam.14157 https://www.repository.cam.ac.uk/handle/1810/268045 |
genre |
Antarc* Antarctic Greenland Ice Sheet |
genre_facet |
Antarc* Antarctic Greenland Ice Sheet |
op_rights |
open.access All Rights Reserved https://www.rioxx.net/licenses/all-rights-reserved/ http://purl.org/coar/access_right/c_abf2 |
op_doi |
https://doi.org/10.17863/cam.14157 |
_version_ |
1810492015988703232 |