Liquid brine in ice shelves
Holes drilled into thin areas of the Brunt Ice Shelf encounter a layer of liquid brine less than 1 m thick approximately at sea-level. Assuming the brine to be moving horizontally, analysis of its effects on thermal equilibrium gives an estimate of steady-state annual brine flow that is in good agre...
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International Glaciological Society
1975
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Online Access: | http://nora.nerc.ac.uk/id/eprint/525872/ https://doi.org/10.3189/S0022143000013459 |
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ftnerc:oai:nora.nerc.ac.uk:525872 2023-05-15T15:47:02+02:00 Liquid brine in ice shelves Thomas, R.H. 1975 http://nora.nerc.ac.uk/id/eprint/525872/ https://doi.org/10.3189/S0022143000013459 unknown International Glaciological Society Thomas, R.H. 1975 Liquid brine in ice shelves. Journal of Glaciology, 14 (70). 125-136. https://doi.org/10.3189/S0022143000013459 <https://doi.org/10.3189/S0022143000013459> Publication - Article PeerReviewed 1975 ftnerc https://doi.org/10.3189/S0022143000013459 2023-02-04T19:49:39Z Holes drilled into thin areas of the Brunt Ice Shelf encounter a layer of liquid brine less than 1 m thick approximately at sea-level. Assuming the brine to be moving horizontally, analysis of its effects on thermal equilibrium gives an estimate of steady-state annual brine flow that is in good agreement with the value deduced from a percolation model. The effect of firn density on percolation rates is such that the slope of an active brine layer increases rapidly as ice thickness increases. However, the heat transport model predicts that brine layers are unlikely to be active in both very thick and very thin ice shelves. Article in Journal/Newspaper Brunt Ice Shelf Ice Shelf Ice Shelves Journal of Glaciology Natural Environment Research Council: NERC Open Research Archive Brunt Ice Shelf ENVELOPE(-22.500,-22.500,-74.750,-74.750) Journal of Glaciology 14 70 125 136 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
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ftnerc |
language |
unknown |
description |
Holes drilled into thin areas of the Brunt Ice Shelf encounter a layer of liquid brine less than 1 m thick approximately at sea-level. Assuming the brine to be moving horizontally, analysis of its effects on thermal equilibrium gives an estimate of steady-state annual brine flow that is in good agreement with the value deduced from a percolation model. The effect of firn density on percolation rates is such that the slope of an active brine layer increases rapidly as ice thickness increases. However, the heat transport model predicts that brine layers are unlikely to be active in both very thick and very thin ice shelves. |
format |
Article in Journal/Newspaper |
author |
Thomas, R.H. |
spellingShingle |
Thomas, R.H. Liquid brine in ice shelves |
author_facet |
Thomas, R.H. |
author_sort |
Thomas, R.H. |
title |
Liquid brine in ice shelves |
title_short |
Liquid brine in ice shelves |
title_full |
Liquid brine in ice shelves |
title_fullStr |
Liquid brine in ice shelves |
title_full_unstemmed |
Liquid brine in ice shelves |
title_sort |
liquid brine in ice shelves |
publisher |
International Glaciological Society |
publishDate |
1975 |
url |
http://nora.nerc.ac.uk/id/eprint/525872/ https://doi.org/10.3189/S0022143000013459 |
long_lat |
ENVELOPE(-22.500,-22.500,-74.750,-74.750) |
geographic |
Brunt Ice Shelf |
geographic_facet |
Brunt Ice Shelf |
genre |
Brunt Ice Shelf Ice Shelf Ice Shelves Journal of Glaciology |
genre_facet |
Brunt Ice Shelf Ice Shelf Ice Shelves Journal of Glaciology |
op_relation |
Thomas, R.H. 1975 Liquid brine in ice shelves. Journal of Glaciology, 14 (70). 125-136. https://doi.org/10.3189/S0022143000013459 <https://doi.org/10.3189/S0022143000013459> |
op_doi |
https://doi.org/10.3189/S0022143000013459 |
container_title |
Journal of Glaciology |
container_volume |
14 |
container_issue |
70 |
container_start_page |
125 |
op_container_end_page |
136 |
_version_ |
1766381851002273792 |