Increased fluxes of shelf-derived materials to the central Arctic Ocean

© The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Science Advances 4 (2018): eaao1302, doi:10.1126/sciadv.aao1302. Rising temperatures in the Arctic Ocean region are responsible for changes such as...

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Published in:Science Advances
Main Authors: Kipp, Lauren, Charette, Matthew A., Moore, Willard S., Henderson, Paul B., Rigor, Ignatius
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science 2018
Subjects:
Ice
Online Access:https://hdl.handle.net/1912/9483
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spelling ftwhoas:oai:darchive.mblwhoilibrary.org:1912/9483 2023-05-15T14:36:55+02:00 Increased fluxes of shelf-derived materials to the central Arctic Ocean Kipp, Lauren Charette, Matthew A. Moore, Willard S. Henderson, Paul B. Rigor, Ignatius 2018-01-03 https://hdl.handle.net/1912/9483 en_US eng American Association for the Advancement of Science https://doi.org/10.1126/sciadv.aao1302 Science Advances 4 (2018): eaao1302 https://hdl.handle.net/1912/9483 doi:10.1126/sciadv.aao1302 Attribution-NonCommercial 4.0 International http://creativecommons.org/licenses/by-nc/4.0/ CC-BY-NC Science Advances 4 (2018): eaao1302 doi:10.1126/sciadv.aao1302 Article 2018 ftwhoas https://doi.org/10.1126/sciadv.aao1302 2022-05-28T23:00:06Z © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Science Advances 4 (2018): eaao1302, doi:10.1126/sciadv.aao1302. Rising temperatures in the Arctic Ocean region are responsible for changes such as reduced ice cover, permafrost thawing, and increased river discharge, which, together, alter nutrient and carbon cycles over the vast Arctic continental shelf. We show that the concentration of radium-228, sourced to seawater through sediment-water exchange processes, has increased substantially in surface waters of the central Arctic Ocean over the past decade. A mass balance model for 228Ra suggests that this increase is due to an intensification of shelf-derived material inputs to the central basin, a source that would also carry elevated concentrations of dissolved organic carbon and nutrients. Therefore, we suggest that significant changes in the nutrient, carbon, and trace metal balances of the Arctic Ocean are underway, with the potential to affect biological productivity and species assemblages in Arctic surface waters. This work was funded by NSF awards OCE-1458305 to M.A.C. and OCE-1458424 to W.S.M. The Mackenzie River sampling was supported by a Graduate Student Research Award from the North Pacific Research Board to L.E.K. L.E.K. also acknowledges support from a National Defense Science and Engineering Graduate Fellowship. I.G.R. acknowledges funding by the contributors to the U.S. Interagency Arctic Buoy Program, which include the U.S. Coast Guard, the Department of Energy, NASA, the U.S. Navy, the National Oceanic and Atmospheric Administration, and NSF. Article in Journal/Newspaper Arctic Arctic Ocean Ice Mackenzie river permafrost Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Arctic Arctic Ocean Central Basin ENVELOPE(43.000,43.000,73.500,73.500) Mackenzie River Pacific Science Advances 4 1 eaao1302
institution Open Polar
collection Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server)
op_collection_id ftwhoas
language English
description © The Author(s), 2018. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Science Advances 4 (2018): eaao1302, doi:10.1126/sciadv.aao1302. Rising temperatures in the Arctic Ocean region are responsible for changes such as reduced ice cover, permafrost thawing, and increased river discharge, which, together, alter nutrient and carbon cycles over the vast Arctic continental shelf. We show that the concentration of radium-228, sourced to seawater through sediment-water exchange processes, has increased substantially in surface waters of the central Arctic Ocean over the past decade. A mass balance model for 228Ra suggests that this increase is due to an intensification of shelf-derived material inputs to the central basin, a source that would also carry elevated concentrations of dissolved organic carbon and nutrients. Therefore, we suggest that significant changes in the nutrient, carbon, and trace metal balances of the Arctic Ocean are underway, with the potential to affect biological productivity and species assemblages in Arctic surface waters. This work was funded by NSF awards OCE-1458305 to M.A.C. and OCE-1458424 to W.S.M. The Mackenzie River sampling was supported by a Graduate Student Research Award from the North Pacific Research Board to L.E.K. L.E.K. also acknowledges support from a National Defense Science and Engineering Graduate Fellowship. I.G.R. acknowledges funding by the contributors to the U.S. Interagency Arctic Buoy Program, which include the U.S. Coast Guard, the Department of Energy, NASA, the U.S. Navy, the National Oceanic and Atmospheric Administration, and NSF.
format Article in Journal/Newspaper
author Kipp, Lauren
Charette, Matthew A.
Moore, Willard S.
Henderson, Paul B.
Rigor, Ignatius
spellingShingle Kipp, Lauren
Charette, Matthew A.
Moore, Willard S.
Henderson, Paul B.
Rigor, Ignatius
Increased fluxes of shelf-derived materials to the central Arctic Ocean
author_facet Kipp, Lauren
Charette, Matthew A.
Moore, Willard S.
Henderson, Paul B.
Rigor, Ignatius
author_sort Kipp, Lauren
title Increased fluxes of shelf-derived materials to the central Arctic Ocean
title_short Increased fluxes of shelf-derived materials to the central Arctic Ocean
title_full Increased fluxes of shelf-derived materials to the central Arctic Ocean
title_fullStr Increased fluxes of shelf-derived materials to the central Arctic Ocean
title_full_unstemmed Increased fluxes of shelf-derived materials to the central Arctic Ocean
title_sort increased fluxes of shelf-derived materials to the central arctic ocean
publisher American Association for the Advancement of Science
publishDate 2018
url https://hdl.handle.net/1912/9483
long_lat ENVELOPE(43.000,43.000,73.500,73.500)
geographic Arctic
Arctic Ocean
Central Basin
Mackenzie River
Pacific
geographic_facet Arctic
Arctic Ocean
Central Basin
Mackenzie River
Pacific
genre Arctic
Arctic Ocean
Ice
Mackenzie river
permafrost
genre_facet Arctic
Arctic Ocean
Ice
Mackenzie river
permafrost
op_source Science Advances 4 (2018): eaao1302
doi:10.1126/sciadv.aao1302
op_relation https://doi.org/10.1126/sciadv.aao1302
Science Advances 4 (2018): eaao1302
https://hdl.handle.net/1912/9483
doi:10.1126/sciadv.aao1302
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