Zinc and silicon biogeochemical decoupling in the North Pacific Ocean
Zinc (Zn) in the ocean is a trace metal and the distribution is controlled by the biological processes, and therefore it is considered a biogeochemically important element. The distribution of dissolved Zn in the global ocean is similar to that of silica (Si). Previous model-based experiments propos...
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ftgfzpotsdam:oai:gfzpublic.gfz-potsdam.de:item_5018189 2023-08-20T04:05:36+02:00 Zinc and silicon biogeochemical decoupling in the North Pacific Ocean Sugino, K. Oka, A. 2023 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018189 eng eng info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1043 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018189 XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) info:eu-repo/semantics/conferenceObject 2023 ftgfzpotsdam https://doi.org/10.57757/IUGG23-1043 2023-07-30T23:40:44Z Zinc (Zn) in the ocean is a trace metal and the distribution is controlled by the biological processes, and therefore it is considered a biogeochemically important element. The distribution of dissolved Zn in the global ocean is similar to that of silica (Si). Previous model-based experiments proposed the Southern Ocean hypothesis: the similarity of Zn and Si distribution spreads from the Southern Ocean surface to the global ocean. The hypothesis is based on the diatom Zn uptake characteristics and the water mass formation process in the Southern Ocean. However, observational data from the North Pacific showed that there is decoupling of Zn and Si: the correlation between Zn and Si breaks down in the North Pacific. The objective of this study is to understand the Zn cycle processes in the North Pacific with an ocean general circulation model, focusing on Zn-Si decoupling. We conducted the model experiment with various Zn uptake speeds in the surface ocean, but it was not easy to reproduce Zn concentrations in the North Pacific. By considering additional Zn sources from the continental shelves of the Sea of Okhotsk and the Bering Sea, we found that high Zn concentration and the Zn–Si decoupling in the North Pacific were reproduced, consistent with observational data. Our result suggests the Zn supply from the coastal regions in the North Pacific. Conference Object Bering Sea Southern Ocean GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) Bering Sea Okhotsk Pacific Southern Ocean |
institution |
Open Polar |
collection |
GFZpublic (German Research Centre for Geosciences, Helmholtz-Zentrum Potsdam) |
op_collection_id |
ftgfzpotsdam |
language |
English |
description |
Zinc (Zn) in the ocean is a trace metal and the distribution is controlled by the biological processes, and therefore it is considered a biogeochemically important element. The distribution of dissolved Zn in the global ocean is similar to that of silica (Si). Previous model-based experiments proposed the Southern Ocean hypothesis: the similarity of Zn and Si distribution spreads from the Southern Ocean surface to the global ocean. The hypothesis is based on the diatom Zn uptake characteristics and the water mass formation process in the Southern Ocean. However, observational data from the North Pacific showed that there is decoupling of Zn and Si: the correlation between Zn and Si breaks down in the North Pacific. The objective of this study is to understand the Zn cycle processes in the North Pacific with an ocean general circulation model, focusing on Zn-Si decoupling. We conducted the model experiment with various Zn uptake speeds in the surface ocean, but it was not easy to reproduce Zn concentrations in the North Pacific. By considering additional Zn sources from the continental shelves of the Sea of Okhotsk and the Bering Sea, we found that high Zn concentration and the Zn–Si decoupling in the North Pacific were reproduced, consistent with observational data. Our result suggests the Zn supply from the coastal regions in the North Pacific. |
format |
Conference Object |
author |
Sugino, K. Oka, A. |
spellingShingle |
Sugino, K. Oka, A. Zinc and silicon biogeochemical decoupling in the North Pacific Ocean |
author_facet |
Sugino, K. Oka, A. |
author_sort |
Sugino, K. |
title |
Zinc and silicon biogeochemical decoupling in the North Pacific Ocean |
title_short |
Zinc and silicon biogeochemical decoupling in the North Pacific Ocean |
title_full |
Zinc and silicon biogeochemical decoupling in the North Pacific Ocean |
title_fullStr |
Zinc and silicon biogeochemical decoupling in the North Pacific Ocean |
title_full_unstemmed |
Zinc and silicon biogeochemical decoupling in the North Pacific Ocean |
title_sort |
zinc and silicon biogeochemical decoupling in the north pacific ocean |
publishDate |
2023 |
url |
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018189 |
geographic |
Bering Sea Okhotsk Pacific Southern Ocean |
geographic_facet |
Bering Sea Okhotsk Pacific Southern Ocean |
genre |
Bering Sea Southern Ocean |
genre_facet |
Bering Sea Southern Ocean |
op_source |
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG) |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.57757/IUGG23-1043 https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018189 |
op_doi |
https://doi.org/10.57757/IUGG23-1043 |
_version_ |
1774716172586975232 |