Radiocarbon as a thermocline proxy for the eastern equatorial Pacific
An ocean model is used to test the idea that sea surface Δ14C behaves as a thermocline proxy in the eastern equatorial Pacific. The ORCA2 model, which includes Δ14C as a passive tracer, has been forced with reanalysis fluxes over 1948–1999, and the output is compared with a previously reported Galap...
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ftnerc:oai:nora.nerc.ac.uk:164807 2023-05-15T13:48:07+02:00 Radiocarbon as a thermocline proxy for the eastern equatorial Pacific Rodgers, Keith B. Aumont, Olivier Madec, Gurvan Menkes, Christophe Blanke, Bruno Monfray, Patrick Orr, James C. Schrag, Daniel P. 2004-07-30 http://nora.nerc.ac.uk/id/eprint/164807/ http://www.agu.org/pubs/crossref/2004/2004GL019764.shtml https://doi.org/10.1029/2004GL019764 unknown Rodgers, Keith B.; Aumont, Olivier; Madec, Gurvan; Menkes, Christophe; Blanke, Bruno; Monfray, Patrick; Orr, James C.; Schrag, Daniel P. 2004 Radiocarbon as a thermocline proxy for the eastern equatorial Pacific. Geophysical Research Letters, 31. L14314. https://doi.org/10.1029/2004GL019764 <https://doi.org/10.1029/2004GL019764> Publication - Article PeerReviewed 2004 ftnerc https://doi.org/10.1029/2004GL019764 2023-02-04T19:35:25Z An ocean model is used to test the idea that sea surface Δ14C behaves as a thermocline proxy in the eastern equatorial Pacific. The ORCA2 model, which includes Δ14C as a passive tracer, has been forced with reanalysis fluxes over 1948–1999, and the output is compared with a previously reported Galapagos Δ14C record. The model reproduces the abrupt increase in the seasonally minimum Δ14C in 1976/77 found in the data. This increase is associated with neither a shift of thermocline depth over the NINO3 region, nor a change in the relative proportion of Northern/Southern source waters. Rather, it is due to a decrease in the Sub-Antarctic Mode Water (SAMW) component of the upwelling water, thereby representing a decrease in entrainment of water from below the base of the directly ventilated thermocline. Article in Journal/Newspaper Antarc* Antarctic Natural Environment Research Council: NERC Open Research Archive Antarctic Galapagos Pacific Geophysical Research Letters 31 14 |
institution |
Open Polar |
collection |
Natural Environment Research Council: NERC Open Research Archive |
op_collection_id |
ftnerc |
language |
unknown |
description |
An ocean model is used to test the idea that sea surface Δ14C behaves as a thermocline proxy in the eastern equatorial Pacific. The ORCA2 model, which includes Δ14C as a passive tracer, has been forced with reanalysis fluxes over 1948–1999, and the output is compared with a previously reported Galapagos Δ14C record. The model reproduces the abrupt increase in the seasonally minimum Δ14C in 1976/77 found in the data. This increase is associated with neither a shift of thermocline depth over the NINO3 region, nor a change in the relative proportion of Northern/Southern source waters. Rather, it is due to a decrease in the Sub-Antarctic Mode Water (SAMW) component of the upwelling water, thereby representing a decrease in entrainment of water from below the base of the directly ventilated thermocline. |
format |
Article in Journal/Newspaper |
author |
Rodgers, Keith B. Aumont, Olivier Madec, Gurvan Menkes, Christophe Blanke, Bruno Monfray, Patrick Orr, James C. Schrag, Daniel P. |
spellingShingle |
Rodgers, Keith B. Aumont, Olivier Madec, Gurvan Menkes, Christophe Blanke, Bruno Monfray, Patrick Orr, James C. Schrag, Daniel P. Radiocarbon as a thermocline proxy for the eastern equatorial Pacific |
author_facet |
Rodgers, Keith B. Aumont, Olivier Madec, Gurvan Menkes, Christophe Blanke, Bruno Monfray, Patrick Orr, James C. Schrag, Daniel P. |
author_sort |
Rodgers, Keith B. |
title |
Radiocarbon as a thermocline proxy for the eastern equatorial Pacific |
title_short |
Radiocarbon as a thermocline proxy for the eastern equatorial Pacific |
title_full |
Radiocarbon as a thermocline proxy for the eastern equatorial Pacific |
title_fullStr |
Radiocarbon as a thermocline proxy for the eastern equatorial Pacific |
title_full_unstemmed |
Radiocarbon as a thermocline proxy for the eastern equatorial Pacific |
title_sort |
radiocarbon as a thermocline proxy for the eastern equatorial pacific |
publishDate |
2004 |
url |
http://nora.nerc.ac.uk/id/eprint/164807/ http://www.agu.org/pubs/crossref/2004/2004GL019764.shtml https://doi.org/10.1029/2004GL019764 |
geographic |
Antarctic Galapagos Pacific |
geographic_facet |
Antarctic Galapagos Pacific |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
Rodgers, Keith B.; Aumont, Olivier; Madec, Gurvan; Menkes, Christophe; Blanke, Bruno; Monfray, Patrick; Orr, James C.; Schrag, Daniel P. 2004 Radiocarbon as a thermocline proxy for the eastern equatorial Pacific. Geophysical Research Letters, 31. L14314. https://doi.org/10.1029/2004GL019764 <https://doi.org/10.1029/2004GL019764> |
op_doi |
https://doi.org/10.1029/2004GL019764 |
container_title |
Geophysical Research Letters |
container_volume |
31 |
container_issue |
14 |
_version_ |
1766248618752212992 |