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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Published in:Journal of Glaciology
Main Author: Thomas, R.H.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 1975
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/525872/
https://doi.org/10.3189/S0022143000013459
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spelling 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
op_collection_id 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
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