A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation

Chlorofluorocarbon-11 inventories for the deep Southern Ocean appear to confirm physical oceanographic and geochemical studies in the Southern Ocean, which suggest that no more than 5 × 10 6 cubic meters per second of ventilated deep water is currently being produced. This result conflicts with conc...

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Published in:Science
Main Authors: Broecker, Wallace S., Sutherland, Stewart, Peng, Tsung-Hung
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1999
Subjects:
Online Access:http://dx.doi.org/10.1126/science.286.5442.1132
https://www.science.org/doi/pdf/10.1126/science.286.5442.1132
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author Broecker, Wallace S.
Sutherland, Stewart
Peng, Tsung-Hung
author_facet Broecker, Wallace S.
Sutherland, Stewart
Peng, Tsung-Hung
author_sort Broecker, Wallace S.
collection AAAS Resource Center (American Association for the Advancement of Science)
container_issue 5442
container_start_page 1132
container_title Science
container_volume 286
description Chlorofluorocarbon-11 inventories for the deep Southern Ocean appear to confirm physical oceanographic and geochemical studies in the Southern Ocean, which suggest that no more than 5 × 10 6 cubic meters per second of ventilated deep water is currently being produced. This result conflicts with conclusions based on the distributions of the carbon-14/carbon ratio and a quasi-conservative property, PO 4 * , in the deep sea, which seem to require an average of about 15 × 10 6 cubic meters per second of Southern Ocean deep ventilation over about the past 800 years. A major reduction in Southern Ocean deep water production during the 20th century (from high rates during the Little Ice Age) may explain this apparent discordance. If this is true, a seesawing of deep water production between the northern Atlantic and Southern oceans may lie at the heart of the 1500-year ice-rafting cycle.
format Article in Journal/Newspaper
genre Southern Ocean
genre_facet Southern Ocean
geographic Southern Ocean
geographic_facet Southern Ocean
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op_doi https://doi.org/10.1126/science.286.5442.1132
op_source Science
volume 286, issue 5442, page 1132-1135
ISSN 0036-8075 1095-9203
publishDate 1999
publisher American Association for the Advancement of Science (AAAS)
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spelling craaas:10.1126/science.286.5442.1132 2025-01-17T00:53:38+00:00 A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation Broecker, Wallace S. Sutherland, Stewart Peng, Tsung-Hung 1999 http://dx.doi.org/10.1126/science.286.5442.1132 https://www.science.org/doi/pdf/10.1126/science.286.5442.1132 en eng American Association for the Advancement of Science (AAAS) Science volume 286, issue 5442, page 1132-1135 ISSN 0036-8075 1095-9203 journal-article 1999 craaas https://doi.org/10.1126/science.286.5442.1132 2024-09-27T04:00:49Z Chlorofluorocarbon-11 inventories for the deep Southern Ocean appear to confirm physical oceanographic and geochemical studies in the Southern Ocean, which suggest that no more than 5 × 10 6 cubic meters per second of ventilated deep water is currently being produced. This result conflicts with conclusions based on the distributions of the carbon-14/carbon ratio and a quasi-conservative property, PO 4 * , in the deep sea, which seem to require an average of about 15 × 10 6 cubic meters per second of Southern Ocean deep ventilation over about the past 800 years. A major reduction in Southern Ocean deep water production during the 20th century (from high rates during the Little Ice Age) may explain this apparent discordance. If this is true, a seesawing of deep water production between the northern Atlantic and Southern oceans may lie at the heart of the 1500-year ice-rafting cycle. Article in Journal/Newspaper Southern Ocean AAAS Resource Center (American Association for the Advancement of Science) Southern Ocean Science 286 5442 1132 1135
spellingShingle Broecker, Wallace S.
Sutherland, Stewart
Peng, Tsung-Hung
A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation
title A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation
title_full A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation
title_fullStr A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation
title_full_unstemmed A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation
title_short A Possible 20th-Century Slowdown of Southern Ocean Deep Water Formation
title_sort possible 20th-century slowdown of southern ocean deep water formation
url http://dx.doi.org/10.1126/science.286.5442.1132
https://www.science.org/doi/pdf/10.1126/science.286.5442.1132