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

A large fraction of ice sheet discharge enters the ocean subsurface from underneath large floating ice-tongues. Here the authors show that associated nutrient export may be governed by shelf circulation and, especially for Fe, particle-dissolved phase exchanges, which is largely independent from fre...

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Autores principales: Stephan Krisch, Mark James Hopwood, Janin Schaffer, Ali Al-Hashem, Juan Höfer, Michiel M. Rutgers van der Loeff, Tim M. Conway, Brent A. Summers, Pablo Lodeiro, Indah Ardiningsih, Tim Steffens, Eric Pieter Achterberg
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Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/04e85f35f35b4a54b08471f477bacf1f
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spelling oai:doaj.org-article:04e85f35f35b4a54b08471f477bacf1f2021-12-02T14:47:28ZThe 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf10.1038/s41467-021-23093-02041-1723https://doaj.org/article/04e85f35f35b4a54b08471f477bacf1f2021-05-01T00:00:00Zhttps://doi.org/10.1038/s41467-021-23093-0https://doaj.org/toc/2041-1723A large fraction of ice sheet discharge enters the ocean subsurface from underneath large floating ice-tongues. Here the authors show that associated nutrient export may be governed by shelf circulation and, especially for Fe, particle-dissolved phase exchanges, which is largely independent from freshwater Fe content.Stephan KrischMark James HopwoodJanin SchafferAli Al-HashemJuan HöferMichiel M. Rutgers van der LoeffTim M. ConwayBrent A. SummersPablo LodeiroIndah ArdiningsihTim SteffensEric Pieter AchterbergNature PortfolioarticleScienceQENNature Communications, Vol 12, Iss 1, Pp 1-13 (2021)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Stephan Krisch
Mark James Hopwood
Janin Schaffer
Ali Al-Hashem
Juan Höfer
Michiel M. Rutgers van der Loeff
Tim M. Conway
Brent A. Summers
Pablo Lodeiro
Indah Ardiningsih
Tim Steffens
Eric Pieter Achterberg
The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf
description A large fraction of ice sheet discharge enters the ocean subsurface from underneath large floating ice-tongues. Here the authors show that associated nutrient export may be governed by shelf circulation and, especially for Fe, particle-dissolved phase exchanges, which is largely independent from freshwater Fe content.
format article
author Stephan Krisch
Mark James Hopwood
Janin Schaffer
Ali Al-Hashem
Juan Höfer
Michiel M. Rutgers van der Loeff
Tim M. Conway
Brent A. Summers
Pablo Lodeiro
Indah Ardiningsih
Tim Steffens
Eric Pieter Achterberg
author_facet Stephan Krisch
Mark James Hopwood
Janin Schaffer
Ali Al-Hashem
Juan Höfer
Michiel M. Rutgers van der Loeff
Tim M. Conway
Brent A. Summers
Pablo Lodeiro
Indah Ardiningsih
Tim Steffens
Eric Pieter Achterberg
author_sort Stephan Krisch
title The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf
title_short The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf
title_full The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf
title_fullStr The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf
title_full_unstemmed The 79°N Glacier cavity modulates subglacial iron export to the NE Greenland Shelf
title_sort 79°n glacier cavity modulates subglacial iron export to the ne greenland shelf
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/04e85f35f35b4a54b08471f477bacf1f
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