Two centuries of limited variability in subtropical North Atlantic thermocline ventilation
Ventilation and mixing of oceanic gyres is important to ocean-atmosphere heat and gas transfer, and to mid-latitude nutrient supply. The rates of mode water formation are believed to impact climate and carbon exchange between the surface and mid-depth water over decadal periods. Here, a record of 14...
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ftunivhongkonghu:oai:hub.hku.hk:10722/151373 2023-05-15T17:29:29+02:00 Two centuries of limited variability in subtropical North Atlantic thermocline ventilation Druffel, ERM Goodkin, NF Hughen, KA Doney, SC 2012 https://doi.org/10.1038/ncomms1811 http://hdl.handle.net/10722/151373 eng eng Nature Communications http://www.scopus.com/mlt/select.url?eid=2-s2.0-84860478007&selection=ref&src=s&origin=recordpage Nature Communications, 2012, v. 3 doi:10.1038/ncomms1811 WOS:000304611400003 2041-1723 eid_2-s2.0-84860478007 http://hdl.handle.net/10722/151373 3 Article 2012 ftunivhongkonghu https://doi.org/10.1038/ncomms1811 2023-01-14T15:43:34Z Ventilation and mixing of oceanic gyres is important to ocean-atmosphere heat and gas transfer, and to mid-latitude nutrient supply. The rates of mode water formation are believed to impact climate and carbon exchange between the surface and mid-depth water over decadal periods. Here, a record of 14 C/ 12 C (1780-1940), which is a proxy for vertical ocean mixing, from an annually banded coral from Bermuda, shows limited inter-annual variability and a substantial Suess Effect (the decrease in 14 C/12 C since 1900). The Sargasso Sea mixing rates between the surface and thermocline varied minimally over the past two centuries, despite changes to mean-hemispheric climate, including the Little Ice Age and variability in the North Atlantic Oscillation. This result indicates that regional formation rates of sub-tropical mode water are stable over decades, and that anthropogenic carbon absorbed by the ocean does not return to the surface at a variable rate. © 2012 Macmillan Publishers Limited. All rights reserved. link_to_subscribed_fulltext Article in Journal/Newspaper North Atlantic North Atlantic oscillation University of Hong Kong: HKU Scholars Hub Nature Communications 3 1 |
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Open Polar |
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University of Hong Kong: HKU Scholars Hub |
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ftunivhongkonghu |
language |
English |
description |
Ventilation and mixing of oceanic gyres is important to ocean-atmosphere heat and gas transfer, and to mid-latitude nutrient supply. The rates of mode water formation are believed to impact climate and carbon exchange between the surface and mid-depth water over decadal periods. Here, a record of 14 C/ 12 C (1780-1940), which is a proxy for vertical ocean mixing, from an annually banded coral from Bermuda, shows limited inter-annual variability and a substantial Suess Effect (the decrease in 14 C/12 C since 1900). The Sargasso Sea mixing rates between the surface and thermocline varied minimally over the past two centuries, despite changes to mean-hemispheric climate, including the Little Ice Age and variability in the North Atlantic Oscillation. This result indicates that regional formation rates of sub-tropical mode water are stable over decades, and that anthropogenic carbon absorbed by the ocean does not return to the surface at a variable rate. © 2012 Macmillan Publishers Limited. All rights reserved. link_to_subscribed_fulltext |
format |
Article in Journal/Newspaper |
author |
Druffel, ERM Goodkin, NF Hughen, KA Doney, SC |
spellingShingle |
Druffel, ERM Goodkin, NF Hughen, KA Doney, SC Two centuries of limited variability in subtropical North Atlantic thermocline ventilation |
author_facet |
Druffel, ERM Goodkin, NF Hughen, KA Doney, SC |
author_sort |
Druffel, ERM |
title |
Two centuries of limited variability in subtropical North Atlantic thermocline ventilation |
title_short |
Two centuries of limited variability in subtropical North Atlantic thermocline ventilation |
title_full |
Two centuries of limited variability in subtropical North Atlantic thermocline ventilation |
title_fullStr |
Two centuries of limited variability in subtropical North Atlantic thermocline ventilation |
title_full_unstemmed |
Two centuries of limited variability in subtropical North Atlantic thermocline ventilation |
title_sort |
two centuries of limited variability in subtropical north atlantic thermocline ventilation |
publishDate |
2012 |
url |
https://doi.org/10.1038/ncomms1811 http://hdl.handle.net/10722/151373 |
genre |
North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic North Atlantic oscillation |
op_relation |
Nature Communications http://www.scopus.com/mlt/select.url?eid=2-s2.0-84860478007&selection=ref&src=s&origin=recordpage Nature Communications, 2012, v. 3 doi:10.1038/ncomms1811 WOS:000304611400003 2041-1723 eid_2-s2.0-84860478007 http://hdl.handle.net/10722/151373 3 |
op_doi |
https://doi.org/10.1038/ncomms1811 |
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Nature Communications |
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3 |
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1766123616283394048 |