Southern Ocean nutrient trapping and the efficiency of the biological pump
We present a data-assimilated model of the ocean's phosphorus cycle that is constrained by climatological phosphate, temperature, salinity, sea-surface height, surface heat and freshwater fluxes, as well as chlorofluorocarbon- 11(CFC-11) and natural Δ14C. Export production is estimated to be 5....
Published in: | Journal of Geophysical Research: Oceans |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
American Geophysical Union
2013
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Subjects: | |
Online Access: | http://hdl.handle.net/1959.4/unsworks_37744 https://unsworks.unsw.edu.au/bitstreams/c406ee55-0b86-48db-9844-163a0a635ddd/download https://doi.org/10.1002/jgrc.20181 |
_version_ | 1829943413260156928 |
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author | Primeau, FW Holzer, M DeVries, T |
author_facet | Primeau, FW Holzer, M DeVries, T |
author_sort | Primeau, FW |
collection | UNSW Sydney (The University of New South Wales): UNSWorks |
container_issue | 5 |
container_start_page | 2547 |
container_title | Journal of Geophysical Research: Oceans |
container_volume | 118 |
description | We present a data-assimilated model of the ocean's phosphorus cycle that is constrained by climatological phosphate, temperature, salinity, sea-surface height, surface heat and freshwater fluxes, as well as chlorofluorocarbon- 11(CFC-11) and natural Δ14C. Export production is estimated to be 5.8±2.0×1012 mol P/yr of which (26±6)% originates in the Southern Ocean (SO) south of 40°S. The biological pump efficiency, defined as the proportion of the ocean's phosphate inventory that is regenerated, is (39±7)%. Dividing the SO south of 40°S into a sub-Antarctic zone (SANTZ) and an Antarctic zone (ANTZ) separated by the latitude of maximum Ekman divergence, we estimate that the SANTZ and ANTZ account, respectively, for (23±5)% and (3±1)% of global export production, (17±4)% and (3±1)% of the regenerated nutrient inventory, and (31±1)% and (43±5)% of the preformed nutrient inventory. Idealized SO nutrient depletion experiments reveal a large-scale transfer of nutrients into circumpolar and deep waters and from the preformed to the regenerated pool. In accord with the concept of the biogeochemical divide, we find that nutrient drawdown in the ANTZ is more effective than in the SANTZ for increasing the efficiency of the biological pump, while having a smaller impact on production in regions north of 40°S. Complete SO nutrient drawdown would allow the biological pump to operate at 94% efficiency by short circuiting the transport of nutrients in northward Ekman currents, leading to a trapping of nutrients in circumpolar and deep waters that would decrease production outside the SO by approximately 44% while increasing it in the SO by more than 725%. ©2013. American Geophysical Union. All Rights Reserved. |
format | Article in Journal/Newspaper |
genre | Antarc* Antarctic Southern Ocean |
genre_facet | Antarc* Antarctic Southern Ocean |
geographic | Antarctic Southern Ocean |
geographic_facet | Antarctic Southern Ocean |
id | ftunswworks:oai:unsworks.library.unsw.edu.au:1959.4/unsworks_37744 |
institution | Open Polar |
language | unknown |
op_collection_id | ftunswworks |
op_container_end_page | 2564 |
op_doi | https://doi.org/10.1002/jgrc.20181 |
op_relation | http://purl.org/au-research/grants/arc/DP120100674 http://hdl.handle.net/1959.4/unsworks_37744 https://doi.org/10.1002/jgrc.20181 |
op_rights | open access https://purl.org/coar/access_right/c_abf2 CC-BY-NC-ND https://creativecommons.org/licenses/by-nc-nd/4.0/ free_to_read |
op_source | urn:ISSN:0148-0227 urn:ISSN:2169-9291 Journal of Geophysical Research, 118, 5, 2547-2564 |
publishDate | 2013 |
publisher | American Geophysical Union |
record_format | openpolar |
spelling | ftunswworks:oai:unsworks.library.unsw.edu.au:1959.4/unsworks_37744 2025-04-20T14:25:53+00:00 Southern Ocean nutrient trapping and the efficiency of the biological pump Primeau, FW Holzer, M DeVries, T 2013 application/pdf http://hdl.handle.net/1959.4/unsworks_37744 https://unsworks.unsw.edu.au/bitstreams/c406ee55-0b86-48db-9844-163a0a635ddd/download https://doi.org/10.1002/jgrc.20181 unknown American Geophysical Union http://purl.org/au-research/grants/arc/DP120100674 http://hdl.handle.net/1959.4/unsworks_37744 https://doi.org/10.1002/jgrc.20181 open access https://purl.org/coar/access_right/c_abf2 CC-BY-NC-ND https://creativecommons.org/licenses/by-nc-nd/4.0/ free_to_read urn:ISSN:0148-0227 urn:ISSN:2169-9291 Journal of Geophysical Research, 118, 5, 2547-2564 37 Earth Sciences 3708 Oceanography anzsrc-for: 37 Earth Sciences anzsrc-for: 3708 Oceanography anzsrc-for: 040503 Physical Oceanography anzsrc-for: 040502 Chemical Oceanography journal article http://purl.org/coar/resource_type/c_6501 2013 ftunswworks https://doi.org/10.1002/jgrc.20181 2025-04-01T00:02:14Z We present a data-assimilated model of the ocean's phosphorus cycle that is constrained by climatological phosphate, temperature, salinity, sea-surface height, surface heat and freshwater fluxes, as well as chlorofluorocarbon- 11(CFC-11) and natural Δ14C. Export production is estimated to be 5.8±2.0×1012 mol P/yr of which (26±6)% originates in the Southern Ocean (SO) south of 40°S. The biological pump efficiency, defined as the proportion of the ocean's phosphate inventory that is regenerated, is (39±7)%. Dividing the SO south of 40°S into a sub-Antarctic zone (SANTZ) and an Antarctic zone (ANTZ) separated by the latitude of maximum Ekman divergence, we estimate that the SANTZ and ANTZ account, respectively, for (23±5)% and (3±1)% of global export production, (17±4)% and (3±1)% of the regenerated nutrient inventory, and (31±1)% and (43±5)% of the preformed nutrient inventory. Idealized SO nutrient depletion experiments reveal a large-scale transfer of nutrients into circumpolar and deep waters and from the preformed to the regenerated pool. In accord with the concept of the biogeochemical divide, we find that nutrient drawdown in the ANTZ is more effective than in the SANTZ for increasing the efficiency of the biological pump, while having a smaller impact on production in regions north of 40°S. Complete SO nutrient drawdown would allow the biological pump to operate at 94% efficiency by short circuiting the transport of nutrients in northward Ekman currents, leading to a trapping of nutrients in circumpolar and deep waters that would decrease production outside the SO by approximately 44% while increasing it in the SO by more than 725%. ©2013. American Geophysical Union. All Rights Reserved. Article in Journal/Newspaper Antarc* Antarctic Southern Ocean UNSW Sydney (The University of New South Wales): UNSWorks Antarctic Southern Ocean Journal of Geophysical Research: Oceans 118 5 2547 2564 |
spellingShingle | 37 Earth Sciences 3708 Oceanography anzsrc-for: 37 Earth Sciences anzsrc-for: 3708 Oceanography anzsrc-for: 040503 Physical Oceanography anzsrc-for: 040502 Chemical Oceanography Primeau, FW Holzer, M DeVries, T Southern Ocean nutrient trapping and the efficiency of the biological pump |
title | Southern Ocean nutrient trapping and the efficiency of the biological pump |
title_full | Southern Ocean nutrient trapping and the efficiency of the biological pump |
title_fullStr | Southern Ocean nutrient trapping and the efficiency of the biological pump |
title_full_unstemmed | Southern Ocean nutrient trapping and the efficiency of the biological pump |
title_short | Southern Ocean nutrient trapping and the efficiency of the biological pump |
title_sort | southern ocean nutrient trapping and the efficiency of the biological pump |
topic | 37 Earth Sciences 3708 Oceanography anzsrc-for: 37 Earth Sciences anzsrc-for: 3708 Oceanography anzsrc-for: 040503 Physical Oceanography anzsrc-for: 040502 Chemical Oceanography |
topic_facet | 37 Earth Sciences 3708 Oceanography anzsrc-for: 37 Earth Sciences anzsrc-for: 3708 Oceanography anzsrc-for: 040503 Physical Oceanography anzsrc-for: 040502 Chemical Oceanography |
url | http://hdl.handle.net/1959.4/unsworks_37744 https://unsworks.unsw.edu.au/bitstreams/c406ee55-0b86-48db-9844-163a0a635ddd/download https://doi.org/10.1002/jgrc.20181 |