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...
Published in: | Journal of Geophysical Research: Oceans |
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Format: | Article in Journal/Newspaper |
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ODU Digital Commons
2022
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Online Access: | https://digitalcommons.odu.edu/oeas_fac_pubs/465 https://doi.org/10.1029/2022JC018999 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1476/viewcontent/Sedwick_2022_SeasonalDynamicsofDissolvedIronOCR.pdf |
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ftolddominionuni:oai:digitalcommons.odu.edu:oeas_fac_pubs-1476 2023-06-11T04:07:05+02:00 Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas 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. 2022-01-01T08:00:00Z application/pdf https://digitalcommons.odu.edu/oeas_fac_pubs/465 https://doi.org/10.1029/2022JC018999 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1476/viewcontent/Sedwick_2022_SeasonalDynamicsofDissolvedIronOCR.pdf unknown ODU Digital Commons https://digitalcommons.odu.edu/oeas_fac_pubs/465 doi:10.1029/2022JC018999 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1476/viewcontent/Sedwick_2022_SeasonalDynamicsofDissolvedIronOCR.pdf © 2022. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License , which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. OES Faculty Publications Aluminium Aluminum Antarctic shelf Bays Benthos Continental shelves Convective mixing Deep water Heavy metals Hydrographic data Ice formation Ice shelves Iron Katabatic winds Land ice Local winds Manganese Mixed layer Mixed layer depth Ocean floor Offshore Overturn Polar environments Polynya Polynyas Primary production Remineralization Ross Sea Sea ice Sea ice formation Sea surface Seasonal variations Seawater Shelf dynamics Shelf water Summer Surface mixed layer surface water Trace metals Vertical mixing Water circulation Water column Wind Wind speed Winter Zinc Glaciology Hydrology Oceanography article 2022 ftolddominionuni https://doi.org/10.1029/2022JC018999 2023-05-08T18:02:42Z 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 convective overturn in coastal polynyas, although the impact of these processes on water-column DFe distributions has not been previously documented. We collected hydrographic data and water-column samples for trace metals analysis in the Terra Nova Bay and Ross Ice Shelf polynyas during April-May 2017 (late austral fall). In the Terra Nova Bay polynya, we observed intense katabatic wind events, and surface mixed layer depths varied from similar to 250 to similar to 600 m over lateral distances <10 km; there vertical mixing was just starting to excavate the dense, iron-rich Shelf Waters, and there was also evidence of DFe inputs at shallower depths in the water column. In the Ross Ice Shelf polynya, wind speeds were lower, mixed layers were <300 m deep, and DFe distributions were similar to previous, late-summer observations, with concentrations elevated near the seafloor. Corresponding measurements of dissolved manganese and zinc, and particulate iron, manganese, and aluminum, suggest that deep DFe maxima and some mid-depth DFe maxima primarily reflect sedimentary inputs, rather than remineralization. Our data and model simulations imply that vertical resupply of DFe in the Ross Sea occurs mainly during mid-late winter, and may be particularly sensitive to changes in the timing and extent of sea ice production. Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Ice Shelves Ross Ice Shelf Ross Sea Sea ice Old Dominion University: ODU Digital Commons Antarctic The Antarctic Austral Ross Sea Terra Nova Bay Ross Ice Shelf Journal of Geophysical Research: Oceans 127 10 |
institution |
Open Polar |
collection |
Old Dominion University: ODU Digital Commons |
op_collection_id |
ftolddominionuni |
language |
unknown |
topic |
Aluminium Aluminum Antarctic shelf Bays Benthos Continental shelves Convective mixing Deep water Heavy metals Hydrographic data Ice formation Ice shelves Iron Katabatic winds Land ice Local winds Manganese Mixed layer Mixed layer depth Ocean floor Offshore Overturn Polar environments Polynya Polynyas Primary production Remineralization Ross Sea Sea ice Sea ice formation Sea surface Seasonal variations Seawater Shelf dynamics Shelf water Summer Surface mixed layer surface water Trace metals Vertical mixing Water circulation Water column Wind Wind speed Winter Zinc Glaciology Hydrology Oceanography |
spellingShingle |
Aluminium Aluminum Antarctic shelf Bays Benthos Continental shelves Convective mixing Deep water Heavy metals Hydrographic data Ice formation Ice shelves Iron Katabatic winds Land ice Local winds Manganese Mixed layer Mixed layer depth Ocean floor Offshore Overturn Polar environments Polynya Polynyas Primary production Remineralization Ross Sea Sea ice Sea ice formation Sea surface Seasonal variations Seawater Shelf dynamics Shelf water Summer Surface mixed layer surface water Trace metals Vertical mixing Water circulation Water column Wind Wind speed Winter Zinc Glaciology Hydrology Oceanography 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. Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas |
topic_facet |
Aluminium Aluminum Antarctic shelf Bays Benthos Continental shelves Convective mixing Deep water Heavy metals Hydrographic data Ice formation Ice shelves Iron Katabatic winds Land ice Local winds Manganese Mixed layer Mixed layer depth Ocean floor Offshore Overturn Polar environments Polynya Polynyas Primary production Remineralization Ross Sea Sea ice Sea ice formation Sea surface Seasonal variations Seawater Shelf dynamics Shelf water Summer Surface mixed layer surface water Trace metals Vertical mixing Water circulation Water column Wind Wind speed Winter Zinc Glaciology Hydrology Oceanography |
description |
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 convective overturn in coastal polynyas, although the impact of these processes on water-column DFe distributions has not been previously documented. We collected hydrographic data and water-column samples for trace metals analysis in the Terra Nova Bay and Ross Ice Shelf polynyas during April-May 2017 (late austral fall). In the Terra Nova Bay polynya, we observed intense katabatic wind events, and surface mixed layer depths varied from similar to 250 to similar to 600 m over lateral distances <10 km; there vertical mixing was just starting to excavate the dense, iron-rich Shelf Waters, and there was also evidence of DFe inputs at shallower depths in the water column. In the Ross Ice Shelf polynya, wind speeds were lower, mixed layers were <300 m deep, and DFe distributions were similar to previous, late-summer observations, with concentrations elevated near the seafloor. Corresponding measurements of dissolved manganese and zinc, and particulate iron, manganese, and aluminum, suggest that deep DFe maxima and some mid-depth DFe maxima primarily reflect sedimentary inputs, rather than remineralization. Our data and model simulations imply that vertical resupply of DFe in the Ross Sea occurs mainly during mid-late winter, and may be particularly sensitive to changes in the timing and extent of sea ice production. |
format |
Article in Journal/Newspaper |
author |
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. |
author_facet |
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. |
author_sort |
Sedwick, P. N. |
title |
Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas |
title_short |
Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas |
title_full |
Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas |
title_fullStr |
Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas |
title_full_unstemmed |
Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas |
title_sort |
seasonal dynamics of dissolved iron on the antarctic continental shelf: late-fall observations from the terra nova bay and ross ice shelf polynyas |
publisher |
ODU Digital Commons |
publishDate |
2022 |
url |
https://digitalcommons.odu.edu/oeas_fac_pubs/465 https://doi.org/10.1029/2022JC018999 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1476/viewcontent/Sedwick_2022_SeasonalDynamicsofDissolvedIronOCR.pdf |
geographic |
Antarctic The Antarctic Austral Ross Sea Terra Nova Bay Ross Ice Shelf |
geographic_facet |
Antarctic The Antarctic Austral Ross Sea Terra Nova Bay Ross Ice Shelf |
genre |
Antarc* Antarctic Ice Shelf Ice Shelves Ross Ice Shelf Ross Sea Sea ice |
genre_facet |
Antarc* Antarctic Ice Shelf Ice Shelves Ross Ice Shelf Ross Sea Sea ice |
op_source |
OES Faculty Publications |
op_relation |
https://digitalcommons.odu.edu/oeas_fac_pubs/465 doi:10.1029/2022JC018999 https://digitalcommons.odu.edu/context/oeas_fac_pubs/article/1476/viewcontent/Sedwick_2022_SeasonalDynamicsofDissolvedIronOCR.pdf |
op_rights |
© 2022. The Authors. This is an open access article under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License , which permits use and distribution in any medium, provided the original work is properly cited, the use is non-commercial and no modifications or adaptations are made. |
op_doi |
https://doi.org/10.1029/2022JC018999 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
127 |
container_issue |
10 |
_version_ |
1768379681125433344 |