Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms
Dissolved iron (DFe) plays an immeasurable role in shaping the biogeochemical processes of the open-ocean Southern Ocean. However, due to observational constraints iron supply pathways remain poorly understood. Using an idealized eddy-resolving physical-biogeochemical model representing a turbulent...
Main Authors: | , , , , , |
---|---|
Format: | Text |
Language: | English |
Published: |
2019
|
Subjects: | |
Online Access: | https://www.documentation.ird.fr/hor/fdi:010077431 |
id |
ftird:oai:ird.fr:fdi:010077431 |
---|---|
record_format |
openpolar |
spelling |
ftird:oai:ird.fr:fdi:010077431 2024-09-09T20:09:28+00:00 Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms Nicholson, S. A. /Levy, Marina /Jouanno, Julien /Capet, Xavier Swart, S. Monteiro, P. M. S. 2019 https://www.documentation.ird.fr/hor/fdi:010077431 EN eng https://www.documentation.ird.fr/hor/fdi:010077431 oai:ird.fr:fdi:010077431 Nicholson S. A., Levy Marina, Jouanno Julien, Capet Xavier, Swart S., Monteiro P. M. S. Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms. 2019, 46 (24), 14567-14575 storms seasonal iron supply winter entrainment eddy advection fronts Southern Ocean text 2019 ftird 2024-08-15T05:57:41Z Dissolved iron (DFe) plays an immeasurable role in shaping the biogeochemical processes of the open-ocean Southern Ocean. However, due to observational constraints iron supply pathways remain poorly understood. Using an idealized eddy-resolving physical-biogeochemical model representing a turbulent sector of the Southern Ocean with seasonal buoyancy forcing and zonal winds overlaid by storms, we quantify the importance of a range of subsurface and surface iron supply mechanisms. The main physical supply pathways to the surface layer are via eddy advection and winter convective mixing in equal proportions. The associated subsurface loss of DFe is restocked via net remineralization (75%) and eddy advection (25%). Summer storms resulted in weak DFe supplies relative to the seasonal supplies (<7.6%). However, in situations of deep summer mixed layers and when interacting with underlying ocean fronts, summer storms resulted in enhanced diffusive and advective DFe supplies and raised summer primary production by 20% for several days. Text Southern Ocean IRD (Institute de recherche pour le développement): Horizon Southern Ocean |
institution |
Open Polar |
collection |
IRD (Institute de recherche pour le développement): Horizon |
op_collection_id |
ftird |
language |
English |
topic |
storms seasonal iron supply winter entrainment eddy advection fronts Southern Ocean |
spellingShingle |
storms seasonal iron supply winter entrainment eddy advection fronts Southern Ocean Nicholson, S. A. /Levy, Marina /Jouanno, Julien /Capet, Xavier Swart, S. Monteiro, P. M. S. Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms |
topic_facet |
storms seasonal iron supply winter entrainment eddy advection fronts Southern Ocean |
description |
Dissolved iron (DFe) plays an immeasurable role in shaping the biogeochemical processes of the open-ocean Southern Ocean. However, due to observational constraints iron supply pathways remain poorly understood. Using an idealized eddy-resolving physical-biogeochemical model representing a turbulent sector of the Southern Ocean with seasonal buoyancy forcing and zonal winds overlaid by storms, we quantify the importance of a range of subsurface and surface iron supply mechanisms. The main physical supply pathways to the surface layer are via eddy advection and winter convective mixing in equal proportions. The associated subsurface loss of DFe is restocked via net remineralization (75%) and eddy advection (25%). Summer storms resulted in weak DFe supplies relative to the seasonal supplies (<7.6%). However, in situations of deep summer mixed layers and when interacting with underlying ocean fronts, summer storms resulted in enhanced diffusive and advective DFe supplies and raised summer primary production by 20% for several days. |
format |
Text |
author |
Nicholson, S. A. /Levy, Marina /Jouanno, Julien /Capet, Xavier Swart, S. Monteiro, P. M. S. |
author_facet |
Nicholson, S. A. /Levy, Marina /Jouanno, Julien /Capet, Xavier Swart, S. Monteiro, P. M. S. |
author_sort |
Nicholson, S. A. |
title |
Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms |
title_short |
Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms |
title_full |
Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms |
title_fullStr |
Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms |
title_full_unstemmed |
Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms |
title_sort |
iron supply pathways between the surface and subsurface waters of the southern ocean : from winter entrainment to summer storms |
publishDate |
2019 |
url |
https://www.documentation.ird.fr/hor/fdi:010077431 |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_relation |
https://www.documentation.ird.fr/hor/fdi:010077431 oai:ird.fr:fdi:010077431 Nicholson S. A., Levy Marina, Jouanno Julien, Capet Xavier, Swart S., Monteiro P. M. S. Iron supply pathways between the surface and subsurface waters of the Southern Ocean : from winter entrainment to summer storms. 2019, 46 (24), 14567-14575 |
_version_ |
1809943631281258496 |