Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C.
Brine volume of sea ice is a function of the salinity and temperature of the ice, and it is related to its strength. This paper gives three equations which can be used to compute the brine volume for three temperature ranges from −0.5° to −22.9°C. A less accurate equation covering the total range is...
| Published in: | Journal of Glaciology |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
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Cambridge University Press (CUP)
1967
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/s0022143000020244 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020244 |
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crcambridgeupr:10.1017/s0022143000020244 |
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openpolar |
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crcambridgeupr:10.1017/s0022143000020244 2024-03-03T08:46:03+00:00 Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. Frankenstein, Guenther Garner, Robert 1967 http://dx.doi.org/10.1017/s0022143000020244 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020244 en eng Cambridge University Press (CUP) Journal of Glaciology volume 6, issue 48, page 943-944 ISSN 0022-1430 1727-5652 Earth-Surface Processes journal-article 1967 crcambridgeupr https://doi.org/10.1017/s0022143000020244 2024-02-08T08:36:15Z Brine volume of sea ice is a function of the salinity and temperature of the ice, and it is related to its strength. This paper gives three equations which can be used to compute the brine volume for three temperature ranges from −0.5° to −22.9°C. A less accurate equation covering the total range is also presented. Article in Journal/Newspaper Journal of Glaciology Sea ice Cambridge University Press Journal of Glaciology 6 48 943 944 |
| institution |
Open Polar |
| collection |
Cambridge University Press |
| op_collection_id |
crcambridgeupr |
| language |
English |
| topic |
Earth-Surface Processes |
| spellingShingle |
Earth-Surface Processes Frankenstein, Guenther Garner, Robert Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. |
| topic_facet |
Earth-Surface Processes |
| description |
Brine volume of sea ice is a function of the salinity and temperature of the ice, and it is related to its strength. This paper gives three equations which can be used to compute the brine volume for three temperature ranges from −0.5° to −22.9°C. A less accurate equation covering the total range is also presented. |
| format |
Article in Journal/Newspaper |
| author |
Frankenstein, Guenther Garner, Robert |
| author_facet |
Frankenstein, Guenther Garner, Robert |
| author_sort |
Frankenstein, Guenther |
| title |
Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. |
| title_short |
Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. |
| title_full |
Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. |
| title_fullStr |
Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. |
| title_full_unstemmed |
Equations for Determining the Brine Volume of Sea Ice from −0.5° to −22.9°C. |
| title_sort |
equations for determining the brine volume of sea ice from −0.5° to −22.9°c. |
| publisher |
Cambridge University Press (CUP) |
| publishDate |
1967 |
| url |
http://dx.doi.org/10.1017/s0022143000020244 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000020244 |
| genre |
Journal of Glaciology Sea ice |
| genre_facet |
Journal of Glaciology Sea ice |
| op_source |
Journal of Glaciology volume 6, issue 48, page 943-944 ISSN 0022-1430 1727-5652 |
| op_doi |
https://doi.org/10.1017/s0022143000020244 |
| container_title |
Journal of Glaciology |
| container_volume |
6 |
| container_issue |
48 |
| container_start_page |
943 |
| op_container_end_page |
944 |
| _version_ |
1792501896111456256 |