Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica
Measurements of the concentrations of Na + K + , Mg 2+ , and Ca 2+ were made on 28 samples from the 255 m deep ice core from Little America V. All concentrations decrease sharply with depth from the firn–ice transition at 52 m to somewhere between 125 m and 150 m. From 150 m to 250 m the cationic co...
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Language: | English |
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Cambridge University Press (CUP)
1974
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Online Access: | http://dx.doi.org/10.1017/s0022143000023200 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023200 |
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crcambridgeupr:10.1017/s0022143000023200 2024-09-15T17:48:40+00:00 Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica Langway, C. C. Herron, M. Cragin, J. H. 1974 http://dx.doi.org/10.1017/s0022143000023200 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023200 en eng Cambridge University Press (CUP) Journal of Glaciology volume 13, issue 69, page 431-435 ISSN 0022-1430 1727-5652 journal-article 1974 crcambridgeupr https://doi.org/10.1017/s0022143000023200 2024-07-31T04:04:11Z Measurements of the concentrations of Na + K + , Mg 2+ , and Ca 2+ were made on 28 samples from the 255 m deep ice core from Little America V. All concentrations decrease sharply with depth from the firn–ice transition at 52 m to somewhere between 125 m and 150 m. From 150 m to 250 m the cationic concentrations are relatively constant. This is interpreted to indicate that the ice above 125 m fell as snow on the Ross Ice Shelf and that ice below 150 m originated inland on Marie Byrd Land. Article in Journal/Newspaper Antarc* Antarctica ice core Ice Shelf Journal of Glaciology Marie Byrd Land Ross Ice Shelf Cambridge University Press Journal of Glaciology 13 69 431 435 |
institution |
Open Polar |
collection |
Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
description |
Measurements of the concentrations of Na + K + , Mg 2+ , and Ca 2+ were made on 28 samples from the 255 m deep ice core from Little America V. All concentrations decrease sharply with depth from the firn–ice transition at 52 m to somewhere between 125 m and 150 m. From 150 m to 250 m the cationic concentrations are relatively constant. This is interpreted to indicate that the ice above 125 m fell as snow on the Ross Ice Shelf and that ice below 150 m originated inland on Marie Byrd Land. |
format |
Article in Journal/Newspaper |
author |
Langway, C. C. Herron, M. Cragin, J. H. |
spellingShingle |
Langway, C. C. Herron, M. Cragin, J. H. Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica |
author_facet |
Langway, C. C. Herron, M. Cragin, J. H. |
author_sort |
Langway, C. C. |
title |
Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica |
title_short |
Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica |
title_full |
Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica |
title_fullStr |
Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica |
title_full_unstemmed |
Chemical Profile of the Ross Ice Shelf at Little America V, Antarctica |
title_sort |
chemical profile of the ross ice shelf at little america v, antarctica |
publisher |
Cambridge University Press (CUP) |
publishDate |
1974 |
url |
http://dx.doi.org/10.1017/s0022143000023200 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000023200 |
genre |
Antarc* Antarctica ice core Ice Shelf Journal of Glaciology Marie Byrd Land Ross Ice Shelf |
genre_facet |
Antarc* Antarctica ice core Ice Shelf Journal of Glaciology Marie Byrd Land Ross Ice Shelf |
op_source |
Journal of Glaciology volume 13, issue 69, page 431-435 ISSN 0022-1430 1727-5652 |
op_doi |
https://doi.org/10.1017/s0022143000023200 |
container_title |
Journal of Glaciology |
container_volume |
13 |
container_issue |
69 |
container_start_page |
431 |
op_container_end_page |
435 |
_version_ |
1810290150372016128 |