Electrical Resistivity Measurements on Ice Sheets

The electrical resistivity of firn and ice of ice sheets is a function of the “base” resistivity, the contact resistance between the grains, and the temperature. At greater depths temperature is the predominant influence, and observed resistivity curves can be explained by temperature variations whi...

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Bibliographic Details
Published in:Journal of Glaciology
Main Author: Hochstein, M.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1967
Subjects:
Earth-Surface Processes
Journal of Glaciology
Online Access:http://dx.doi.org/10.1017/s0022143000019894
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019894
id crcambridgeupr:10.1017/s0022143000019894
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spelling crcambridgeupr:10.1017/s0022143000019894 2024-04-07T07:53:42+00:00 Electrical Resistivity Measurements on Ice Sheets Hochstein, M. 1967 http://dx.doi.org/10.1017/s0022143000019894 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019894 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 47, page 623-633 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1967 crcambridgeupr https://doi.org/10.1017/s0022143000019894 2024-03-08T00:35:19Z The electrical resistivity of firn and ice of ice sheets is a function of the “base” resistivity, the contact resistance between the grains, and the temperature. At greater depths temperature is the predominant influence, and observed resistivity curves can be explained by temperature variations which agree partly with the theories of heat conduction in ice sheets. Article in Journal/Newspaper Journal of Glaciology Cambridge University Press Journal of Glaciology 6 47 623 633
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Earth-Surface Processes
spellingShingle Earth-Surface Processes
Hochstein, M.
Electrical Resistivity Measurements on Ice Sheets
topic_facet Earth-Surface Processes
description The electrical resistivity of firn and ice of ice sheets is a function of the “base” resistivity, the contact resistance between the grains, and the temperature. At greater depths temperature is the predominant influence, and observed resistivity curves can be explained by temperature variations which agree partly with the theories of heat conduction in ice sheets.
format Article in Journal/Newspaper
author Hochstein, M.
author_facet Hochstein, M.
author_sort Hochstein, M.
title Electrical Resistivity Measurements on Ice Sheets
title_short Electrical Resistivity Measurements on Ice Sheets
title_full Electrical Resistivity Measurements on Ice Sheets
title_fullStr Electrical Resistivity Measurements on Ice Sheets
title_full_unstemmed Electrical Resistivity Measurements on Ice Sheets
title_sort electrical resistivity measurements on ice sheets
publisher Cambridge University Press (CUP)
publishDate 1967
url http://dx.doi.org/10.1017/s0022143000019894
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000019894
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source Journal of Glaciology
volume 6, issue 47, page 623-633
ISSN 0022-1430 1727-5652
op_doi https://doi.org/10.1017/s0022143000019894
container_title Journal of Glaciology
container_volume 6
container_issue 47
container_start_page 623
op_container_end_page 633
_version_ 1795669796574986240

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