The passage of the bomb radiocarbon pulse into the Pacific Ocean
Author Posting. © Arizona Board of Regents on behalf of the University of Arizona, 2010. This article is posted here by permission of Dept. of Geosciences, University of Arizona for personal use, not for redistribution. The definitive version was published in Radiocarbon 52 (2010): 1182-1190. We rep...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/4376 2023-05-15T13:53:14+02:00 The passage of the bomb radiocarbon pulse into the Pacific Ocean Jenkins, William J. Elder, Kathryn L. McNichol, Ann P. von Reden, Karl F. 2010-08 application/pdf https://hdl.handle.net/1912/4376 en_US eng Dept. of Geosciences, University of Arizona https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/3615 Radiocarbon 52 (2010): 1182-1190 https://hdl.handle.net/1912/4376 Radiocarbon 52 (2010): 1182-1190 Article 2010 ftwhoas 2022-05-28T22:58:18Z Author Posting. © Arizona Board of Regents on behalf of the University of Arizona, 2010. This article is posted here by permission of Dept. of Geosciences, University of Arizona for personal use, not for redistribution. The definitive version was published in Radiocarbon 52 (2010): 1182-1190. We report and compare radiocarbon observations made on 2 meridional oceanographic sections along 150°W in the South Pacific in 1991 and 2005. The distributions reflect the progressive penetration of nuclear weapons-produced 14C into the oceanic thermocline. The changes over the 14 yr between occupations are demonstrably large relative to any possible drift in our analytical standardization. The computed difference field based on the gridded data in the upper 1600 m of the section exhibits a significant decrease over time (approaching 40 to 50‰ in Δ14C) in the upper 200–300 m, consistent with the decadal post-bomb decline in atmospheric 14C levels. A strong positive anomaly (increase with time), centered on the low salinity core of the Antarctic Intermediate Water (AAIW), approaches 50–60‰ in Δ14C, a clear signature of the downstream evolution of the 14C transient in this water mass. We use this observation to estimate the transit time of AAIW from its “source region” in the southeast South Pacific and to compute the effective reservoir age of this water mass. The 2 sections show small but significant changes in the abyssal 14C distributions. Between 1991 and 2005, Δ14C has increased by 9‰ below 2000 m north of 55°S. This change is accompanied overall by a modest increase in salinity and dissolved oxygen, as well as a slight decrease in dissolved silica. Such changes are indicative of greater ventilation. Calculation of “phosphate star” also indicates that this may be due to a shift from the Southern Ocean toward North Atlantic Deep Water as the ventilation source of the abyssal South Pacific. This work was performed under National Science Foundation Grant number OCE-0223434 as well as a cooperative agreement with NSF ... Article in Journal/Newspaper Antarc* Antarctic North Atlantic Deep Water North Atlantic Southern Ocean Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Antarctic Pacific Southern Ocean The Antarctic |
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Open Polar |
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Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
description |
Author Posting. © Arizona Board of Regents on behalf of the University of Arizona, 2010. This article is posted here by permission of Dept. of Geosciences, University of Arizona for personal use, not for redistribution. The definitive version was published in Radiocarbon 52 (2010): 1182-1190. We report and compare radiocarbon observations made on 2 meridional oceanographic sections along 150°W in the South Pacific in 1991 and 2005. The distributions reflect the progressive penetration of nuclear weapons-produced 14C into the oceanic thermocline. The changes over the 14 yr between occupations are demonstrably large relative to any possible drift in our analytical standardization. The computed difference field based on the gridded data in the upper 1600 m of the section exhibits a significant decrease over time (approaching 40 to 50‰ in Δ14C) in the upper 200–300 m, consistent with the decadal post-bomb decline in atmospheric 14C levels. A strong positive anomaly (increase with time), centered on the low salinity core of the Antarctic Intermediate Water (AAIW), approaches 50–60‰ in Δ14C, a clear signature of the downstream evolution of the 14C transient in this water mass. We use this observation to estimate the transit time of AAIW from its “source region” in the southeast South Pacific and to compute the effective reservoir age of this water mass. The 2 sections show small but significant changes in the abyssal 14C distributions. Between 1991 and 2005, Δ14C has increased by 9‰ below 2000 m north of 55°S. This change is accompanied overall by a modest increase in salinity and dissolved oxygen, as well as a slight decrease in dissolved silica. Such changes are indicative of greater ventilation. Calculation of “phosphate star” also indicates that this may be due to a shift from the Southern Ocean toward North Atlantic Deep Water as the ventilation source of the abyssal South Pacific. This work was performed under National Science Foundation Grant number OCE-0223434 as well as a cooperative agreement with NSF ... |
format |
Article in Journal/Newspaper |
author |
Jenkins, William J. Elder, Kathryn L. McNichol, Ann P. von Reden, Karl F. |
spellingShingle |
Jenkins, William J. Elder, Kathryn L. McNichol, Ann P. von Reden, Karl F. The passage of the bomb radiocarbon pulse into the Pacific Ocean |
author_facet |
Jenkins, William J. Elder, Kathryn L. McNichol, Ann P. von Reden, Karl F. |
author_sort |
Jenkins, William J. |
title |
The passage of the bomb radiocarbon pulse into the Pacific Ocean |
title_short |
The passage of the bomb radiocarbon pulse into the Pacific Ocean |
title_full |
The passage of the bomb radiocarbon pulse into the Pacific Ocean |
title_fullStr |
The passage of the bomb radiocarbon pulse into the Pacific Ocean |
title_full_unstemmed |
The passage of the bomb radiocarbon pulse into the Pacific Ocean |
title_sort |
passage of the bomb radiocarbon pulse into the pacific ocean |
publisher |
Dept. of Geosciences, University of Arizona |
publishDate |
2010 |
url |
https://hdl.handle.net/1912/4376 |
geographic |
Antarctic Pacific Southern Ocean The Antarctic |
geographic_facet |
Antarctic Pacific Southern Ocean The Antarctic |
genre |
Antarc* Antarctic North Atlantic Deep Water North Atlantic Southern Ocean |
genre_facet |
Antarc* Antarctic North Atlantic Deep Water North Atlantic Southern Ocean |
op_source |
Radiocarbon 52 (2010): 1182-1190 |
op_relation |
https://journals.uair.arizona.edu/index.php/radiocarbon/article/view/3615 Radiocarbon 52 (2010): 1182-1190 https://hdl.handle.net/1912/4376 |
_version_ |
1766258232013094912 |