Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late‐Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas

Over the Ross Sea shelf, annual primary production is limited by dissolved iron (DFe) supply. Here, a major source of DFe to surface waters is thought to be vertical resupply from the benthos, which is assumed most prevalent during winter months when katabatic winds drive sea ice formation and conve...

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Detalles Bibliográficos
Autores principales: Sedwick, P. N., Sohst, B. M., O’Hara, C., Stammerjohn, S. E., Loose, B., Dinniman, M. S., Buck, N. J., Resing, J. A., Ackley, S. F.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2022
Materias:
Research Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9788290/
https://www.ncbi.nlm.nih.gov/pubmed/36590600
http://dx.doi.org/10.1029/2022JC018999

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9788290/
https://www.ncbi.nlm.nih.gov/pubmed/36590600
http://dx.doi.org/10.1029/2022JC018999

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