Iron supply to the Amundsen Sea, Antarctica is dominated by circumpolar deepwater and continental subglacial sources
Abstract Glacial melting in West Antarctica has intensified with the increased intrusion of warm ocean water beneath ice shelves, but the processes controlling the export of meltwater-associated micronutrient iron (Fe) to Southern Ocean surface waters remain unclear. Here, we report Fe concentration...
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| Asıl Yazarlar: | , , , , , , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Nature Portfolio
2026-02-01
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| Seri Bilgileri: | Communications Earth & Environment |
| Online Erişim: | https://doi.org/10.1038/s43247-026-03264-x |
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