3. On the Distribution of Temperature in the Antarctic Ocean
Abstract In the regions of the Antarctic Ocean where icebergs are numerous, and where in winter the sea-water freezes, the distribution of temperature in the deeper layers of water is peculiar. The facts are detailed in the Challenger Narrative (vol. i.). The general result of her observations went...
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crcambridgeupr:10.1017/s0370164600003679 2024-03-03T08:37:45+00:00 3. On the Distribution of Temperature in the Antarctic Ocean Buchanan, J. Y. 1888 http://dx.doi.org/10.1017/s0370164600003679 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0370164600003679 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Proceedings of the Royal Society of Edinburgh volume 14, page 147-149 ISSN 0370-1646 General Engineering journal-article 1888 crcambridgeupr https://doi.org/10.1017/s0370164600003679 2024-02-08T08:30:50Z Abstract In the regions of the Antarctic Ocean where icebergs are numerous, and where in winter the sea-water freezes, the distribution of temperature in the deeper layers of water is peculiar. The facts are detailed in the Challenger Narrative (vol. i.). The general result of her observations went to show that, from the edge of the ice-pack, a wedge of cold water stretches northwards for more than 12° of latitude, underlying and overlying strata at a higher temperature than itself (p. 418). Article in Journal/Newspaper Antarc* Antarctic Antarctic Ocean ice pack Iceberg* Cambridge University Press Antarctic The Antarctic Antarctic Ocean Proceedings of the Royal Society of Edinburgh 14 147 149 |
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Open Polar |
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Cambridge University Press |
op_collection_id |
crcambridgeupr |
language |
English |
topic |
General Engineering |
spellingShingle |
General Engineering Buchanan, J. Y. 3. On the Distribution of Temperature in the Antarctic Ocean |
topic_facet |
General Engineering |
description |
Abstract In the regions of the Antarctic Ocean where icebergs are numerous, and where in winter the sea-water freezes, the distribution of temperature in the deeper layers of water is peculiar. The facts are detailed in the Challenger Narrative (vol. i.). The general result of her observations went to show that, from the edge of the ice-pack, a wedge of cold water stretches northwards for more than 12° of latitude, underlying and overlying strata at a higher temperature than itself (p. 418). |
format |
Article in Journal/Newspaper |
author |
Buchanan, J. Y. |
author_facet |
Buchanan, J. Y. |
author_sort |
Buchanan, J. Y. |
title |
3. On the Distribution of Temperature in the Antarctic Ocean |
title_short |
3. On the Distribution of Temperature in the Antarctic Ocean |
title_full |
3. On the Distribution of Temperature in the Antarctic Ocean |
title_fullStr |
3. On the Distribution of Temperature in the Antarctic Ocean |
title_full_unstemmed |
3. On the Distribution of Temperature in the Antarctic Ocean |
title_sort |
3. on the distribution of temperature in the antarctic ocean |
publisher |
Cambridge University Press (CUP) |
publishDate |
1888 |
url |
http://dx.doi.org/10.1017/s0370164600003679 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0370164600003679 |
geographic |
Antarctic The Antarctic Antarctic Ocean |
geographic_facet |
Antarctic The Antarctic Antarctic Ocean |
genre |
Antarc* Antarctic Antarctic Ocean ice pack Iceberg* |
genre_facet |
Antarc* Antarctic Antarctic Ocean ice pack Iceberg* |
op_source |
Proceedings of the Royal Society of Edinburgh volume 14, page 147-149 ISSN 0370-1646 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0370164600003679 |
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Proceedings of the Royal Society of Edinburgh |
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14 |
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147 |
op_container_end_page |
149 |
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1792501317604737024 |