Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice
Abstract A model for the isotopic composition in δ D and δ 18 O of ice formed by refreezing at the glacier sole is developed. This model predicts relatively well the distribution of points representing samples from basal layers of an Arctic and an Alpine glacier on a δ D– δ 18 O diagram. The frozen...
Published in: | Journal of Glaciology |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Cambridge University Press (CUP)
1982
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Subjects: | |
Online Access: | http://dx.doi.org/10.1017/s0022143000011771 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011771 |
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author | Jouzel, J. Souchez, R. A. |
author_facet | Jouzel, J. Souchez, R. A. |
author_sort | Jouzel, J. |
collection | Cambridge University Press |
container_issue | 98 |
container_start_page | 35 |
container_title | Journal of Glaciology |
container_volume | 28 |
description | Abstract A model for the isotopic composition in δ D and δ 18 O of ice formed by refreezing at the glacier sole is developed. This model predicts relatively well the distribution of points representing samples from basal layers of an Arctic and an Alpine glacier on a δ D– δ 18 O diagram. The frozen fraction which is the part of the liquid that refreezes can be determined for each basal ice layer. This may have implications on the study of the ice–water system at the ice–rock interface. |
format | Article in Journal/Newspaper |
genre | Arctic Journal of Glaciology |
genre_facet | Arctic Journal of Glaciology |
geographic | Arctic |
geographic_facet | Arctic |
id | crcambridgeupr:10.1017/s0022143000011771 |
institution | Open Polar |
language | English |
op_collection_id | crcambridgeupr |
op_container_end_page | 42 |
op_doi | https://doi.org/10.1017/s0022143000011771 |
op_source | Journal of Glaciology volume 28, issue 98, page 35-42 ISSN 0022-1430 1727-5652 |
publishDate | 1982 |
publisher | Cambridge University Press (CUP) |
record_format | openpolar |
spelling | crcambridgeupr:10.1017/s0022143000011771 2025-01-16T20:30:09+00:00 Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice Jouzel, J. Souchez, R. A. 1982 http://dx.doi.org/10.1017/s0022143000011771 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011771 en eng Cambridge University Press (CUP) Journal of Glaciology volume 28, issue 98, page 35-42 ISSN 0022-1430 1727-5652 journal-article 1982 crcambridgeupr https://doi.org/10.1017/s0022143000011771 2024-07-31T04:04:19Z Abstract A model for the isotopic composition in δ D and δ 18 O of ice formed by refreezing at the glacier sole is developed. This model predicts relatively well the distribution of points representing samples from basal layers of an Arctic and an Alpine glacier on a δ D– δ 18 O diagram. The frozen fraction which is the part of the liquid that refreezes can be determined for each basal ice layer. This may have implications on the study of the ice–water system at the ice–rock interface. Article in Journal/Newspaper Arctic Journal of Glaciology Cambridge University Press Arctic Journal of Glaciology 28 98 35 42 |
spellingShingle | Jouzel, J. Souchez, R. A. Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice |
title | Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice |
title_full | Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice |
title_fullStr | Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice |
title_full_unstemmed | Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice |
title_short | Melting–Refreezing at the Glacier Sole and the Isotopic Composition of the Ice |
title_sort | melting–refreezing at the glacier sole and the isotopic composition of the ice |
url | http://dx.doi.org/10.1017/s0022143000011771 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000011771 |