Circulation and Melting Beneath the Ross Ice Shelf

Thermohaline observations in the water column beneath the Ross Ice Shelf and along its terminal face show significant vertical stratification, active horizontal circulation, and net melting at the ice shelf base. Heat is supplied by seawater that moves southward beneath the ice shelf from a central...

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Published in:Science
Main Authors: Jacobs, Stanley S., Gordon, Arnold L., Ardai, J. L.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1979
Subjects:
Online Access:http://dx.doi.org/10.1126/science.203.4379.439
https://www.science.org/doi/pdf/10.1126/science.203.4379.439
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spelling craaas:10.1126/science.203.4379.439 2024-06-09T07:46:51+00:00 Circulation and Melting Beneath the Ross Ice Shelf Jacobs, Stanley S. Gordon, Arnold L. Ardai, J. L. 1979 http://dx.doi.org/10.1126/science.203.4379.439 https://www.science.org/doi/pdf/10.1126/science.203.4379.439 en eng American Association for the Advancement of Science (AAAS) Science volume 203, issue 4379, page 439-443 ISSN 0036-8075 1095-9203 journal-article 1979 craaas https://doi.org/10.1126/science.203.4379.439 2024-05-16T12:55:07Z Thermohaline observations in the water column beneath the Ross Ice Shelf and along its terminal face show significant vertical stratification, active horizontal circulation, and net melting at the ice shelf base. Heat is supplied by seawater that moves southward beneath the ice shelf from a central warm core and from a western region of high salinity. The near-freezing Ice Shelf Water produced flows northward into the Ross Sea. Article in Journal/Newspaper Ice Shelf Ross Ice Shelf Ross Sea AAAS Resource Center (American Association for the Advancement of Science) Ross Ice Shelf Ross Sea Science 203 4379 439 443
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Thermohaline observations in the water column beneath the Ross Ice Shelf and along its terminal face show significant vertical stratification, active horizontal circulation, and net melting at the ice shelf base. Heat is supplied by seawater that moves southward beneath the ice shelf from a central warm core and from a western region of high salinity. The near-freezing Ice Shelf Water produced flows northward into the Ross Sea.
format Article in Journal/Newspaper
author Jacobs, Stanley S.
Gordon, Arnold L.
Ardai, J. L.
spellingShingle Jacobs, Stanley S.
Gordon, Arnold L.
Ardai, J. L.
Circulation and Melting Beneath the Ross Ice Shelf
author_facet Jacobs, Stanley S.
Gordon, Arnold L.
Ardai, J. L.
author_sort Jacobs, Stanley S.
title Circulation and Melting Beneath the Ross Ice Shelf
title_short Circulation and Melting Beneath the Ross Ice Shelf
title_full Circulation and Melting Beneath the Ross Ice Shelf
title_fullStr Circulation and Melting Beneath the Ross Ice Shelf
title_full_unstemmed Circulation and Melting Beneath the Ross Ice Shelf
title_sort circulation and melting beneath the ross ice shelf
publisher American Association for the Advancement of Science (AAAS)
publishDate 1979
url http://dx.doi.org/10.1126/science.203.4379.439
https://www.science.org/doi/pdf/10.1126/science.203.4379.439
geographic Ross Ice Shelf
Ross Sea
geographic_facet Ross Ice Shelf
Ross Sea
genre Ice Shelf
Ross Ice Shelf
Ross Sea
genre_facet Ice Shelf
Ross Ice Shelf
Ross Sea
op_source Science
volume 203, issue 4379, page 439-443
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.203.4379.439
container_title Science
container_volume 203
container_issue 4379
container_start_page 439
op_container_end_page 443
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