The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf

Approximately half of the freshwater discharged from the Greenland and Antarctic Ice Sheets enters the ocean subsurface as a result of basal ice melt, or runoff draining via the grounding line of a deep ice shelf or marine-terminating glacier. Around Antarctica and parts of northern Greenland, this...

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Detalles Bibliográficos
Autores principales: Krisch, Stephan, Hopwood, Mark James, Schaffer, Janin, Al-Hashem, Ali, Höfer, Juan, Rutgers van der Loeff, Michiel M., Conway, Tim M., Summers, Brent A., Lodeiro, Pablo, Ardiningsih, Indah, Steffens, Tim, Achterberg, Eric Pieter
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8144390/
https://www.ncbi.nlm.nih.gov/pubmed/34031401
http://dx.doi.org/10.1038/s41467-021-23093-0

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8144390/
https://www.ncbi.nlm.nih.gov/pubmed/34031401
http://dx.doi.org/10.1038/s41467-021-23093-0

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