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From the subtropics to the equator in the Southwest Pacific: Continental material fluxes quantified using neodymium data along modeled thermocline water pathways
Citation
Grenier, M and Jeandel, C and Cravatte, S, From the subtropics to the equator in the Southwest Pacific: Continental material fluxes quantified using neodymium data along modeled thermocline water pathways, Journal of Geophysical Research: Oceans, 119, (6) pp. 3948-3966. ISSN 2169-9275 (2014) [Refereed Article]
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Copyright Statement
Copyright 2014 American Geophysical Union
Abstract
The southwestern tropical Pacific, part of a major pathway for waters feeding the Equatorial Undercurrent, is a region of important geochemical enrichment through land-ocean boundary exchange. Here we develop an original method based on the coupling between dynamical modeling and geochemical tracer data to identify regions of enrichment along the water pathways from the subtropics to the equator, and to allow a refined quantification of continental material fluxes. Neodymium data are interpreted with the help of modeled Lagrangian trajectories of an Ocean General Circulation Model. We reveal that upper and lower thermocline waters have different pathways together with different geochemical evolutions. The upper thermocline waters entering the Solomon Sea mainly originate from the central subtropical gyre, enter the Coral Sea in the North Vanuatu Jet and likely receive radiogenic neodymium from the basaltic island margins encountered along their route. The lower thermocline waters entering the Solomon Sea mainly originate from northeast of New Zealand and enter the Coral Sea in the North Caledonian Jet. Depletion of their neodymium content likely occurs when flowing along the Australian and Papua coasts. Downstream from the Solomon Sea, waters flowing along the Papua New Guinea margins near the Sepik river mouth become surprisingly depleted in their neodymium content in the upper thermocline while enriched in the lower thermocline. This coupled approach is proposed as strong support to interpret the origin of the equatorial Pacific natural fertilization through a better understanding of the circulation, important objectives of the international GEOTRACES and SPICE programs, respectively.
Item Details
| Item Type: | Refereed Article |
|---|---|
| Keywords: | continental material flux, neodumium data, thermocline water pathways, equatorial undercurrent, tropical Pacific |
| Research Division: | Earth Sciences |
| Research Group: | Oceanography |
| Research Field: | Physical oceanography |
| Objective Division: | Expanding Knowledge |
| Objective Group: | Expanding knowledge |
| Objective Field: | Expanding knowledge in the earth sciences |
| UTAS Author: | Grenier, M (Dr Melanie Grenier) |
| ID Code: | 118231 |
| Year Published: | 2014 |
| Web of Science® Times Cited: | 21 |
| Deposited By: | CRC-Antarctic Climate & Ecosystems |
| Deposited On: | 2017-07-07 |
| Last Modified: | 2018-04-17 |
| Downloads: | 143 View Download Statistics |
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