Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water

Large amounts of atmospheric carbon can be exported and retained in the deep sea on millennial time scales, buffering global warming. However, while the Barents Sea is one of the most biologically productive areas of the Arctic Ocean, carbon retention times were thought to be short. Here we present...

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Published in:Nature Geoscience
Main Authors: Rogge, Andreas, Janout, Markus, Loginova, Nadezhda, Trudnowska, Emilia, Horstmann, Cora, Wekerle, Claudia, Oziel, Laurent, Schourup-Kristensen, Vibe, Ruiz-Castillo, Eugenio, Schulz, Kirstin, V. Povazhnyy, Vasily, Iversen, Morten, Waite, Anya M.
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://pure.au.dk/portal/da/publications/carbon-dioxide-sink-in-the-arctic-ocean-from-crossshelf-transport-of-dense-barents-sea-water(df025c1d-2755-4caa-bdf0-c1dcfa8c281c).html
https://doi.org/10.1038/s41561-022-01069-z
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spelling ftuniaarhuspubl:oai:pure.atira.dk:publications/df025c1d-2755-4caa-bdf0-c1dcfa8c281c 2023-12-31T10:01:57+01:00 Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water Rogge, Andreas Janout, Markus Loginova, Nadezhda Trudnowska, Emilia Horstmann, Cora Wekerle, Claudia Oziel, Laurent Schourup-Kristensen, Vibe Ruiz-Castillo, Eugenio Schulz, Kirstin V. Povazhnyy, Vasily Iversen, Morten Waite, Anya M. 2023-01 https://pure.au.dk/portal/da/publications/carbon-dioxide-sink-in-the-arctic-ocean-from-crossshelf-transport-of-dense-barents-sea-water(df025c1d-2755-4caa-bdf0-c1dcfa8c281c).html https://doi.org/10.1038/s41561-022-01069-z eng eng https://pure.au.dk/portal/da/publications/carbon-dioxide-sink-in-the-arctic-ocean-from-crossshelf-transport-of-dense-barents-sea-water(df025c1d-2755-4caa-bdf0-c1dcfa8c281c).html info:eu-repo/semantics/openAccess Rogge , A , Janout , M , Loginova , N , Trudnowska , E , Horstmann , C , Wekerle , C , Oziel , L , Schourup-Kristensen , V , Ruiz-Castillo , E , Schulz , K , V. Povazhnyy , V , Iversen , M & Waite , A M 2023 , ' Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water ' , Nature Geoscience , vol. 16 , no. 1 , pp. 82-88 . https://doi.org/10.1038/s41561-022-01069-z article 2023 ftuniaarhuspubl https://doi.org/10.1038/s41561-022-01069-z 2023-12-07T00:05:44Z Large amounts of atmospheric carbon can be exported and retained in the deep sea on millennial time scales, buffering global warming. However, while the Barents Sea is one of the most biologically productive areas of the Arctic Ocean, carbon retention times were thought to be short. Here we present observations, complemented by numerical model simulations, that revealed a deep and widespread lateral injection of approximately 2.33 kt C d −1 from the Barents Sea shelf to some 1,200 m of the Nansen Basin, driven by Barents Sea Bottom Water transport. With increasing distance from the outflow region, the plume expanded and penetrated into even deeper waters and the sediment. The seasonally fluctuating but continuous injection increases the carbon sequestration of the Barents Sea by 1/3 and feeds the deep sea community of the Nansen Basin. Our findings combined with those from other outflow regions of carbon-rich polar dense waters highlight the importance of lateral injection as a global carbon sink. Resolving uncertainties around negative feedbacks of global warming due to sea ice decline will necessitate observation of changes in bottom water formation and biological productivity at a resolution high enough to quantify future deep carbon injection. Article in Journal/Newspaper Arctic Arctic Arctic Ocean Barents Sea Global warming Nansen Basin Sea ice Aarhus University: Research Nature Geoscience 16 1 82 88
institution Open Polar
collection Aarhus University: Research
op_collection_id ftuniaarhuspubl
language English
description Large amounts of atmospheric carbon can be exported and retained in the deep sea on millennial time scales, buffering global warming. However, while the Barents Sea is one of the most biologically productive areas of the Arctic Ocean, carbon retention times were thought to be short. Here we present observations, complemented by numerical model simulations, that revealed a deep and widespread lateral injection of approximately 2.33 kt C d −1 from the Barents Sea shelf to some 1,200 m of the Nansen Basin, driven by Barents Sea Bottom Water transport. With increasing distance from the outflow region, the plume expanded and penetrated into even deeper waters and the sediment. The seasonally fluctuating but continuous injection increases the carbon sequestration of the Barents Sea by 1/3 and feeds the deep sea community of the Nansen Basin. Our findings combined with those from other outflow regions of carbon-rich polar dense waters highlight the importance of lateral injection as a global carbon sink. Resolving uncertainties around negative feedbacks of global warming due to sea ice decline will necessitate observation of changes in bottom water formation and biological productivity at a resolution high enough to quantify future deep carbon injection.
format Article in Journal/Newspaper
author Rogge, Andreas
Janout, Markus
Loginova, Nadezhda
Trudnowska, Emilia
Horstmann, Cora
Wekerle, Claudia
Oziel, Laurent
Schourup-Kristensen, Vibe
Ruiz-Castillo, Eugenio
Schulz, Kirstin
V. Povazhnyy, Vasily
Iversen, Morten
Waite, Anya M.
spellingShingle Rogge, Andreas
Janout, Markus
Loginova, Nadezhda
Trudnowska, Emilia
Horstmann, Cora
Wekerle, Claudia
Oziel, Laurent
Schourup-Kristensen, Vibe
Ruiz-Castillo, Eugenio
Schulz, Kirstin
V. Povazhnyy, Vasily
Iversen, Morten
Waite, Anya M.
Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water
author_facet Rogge, Andreas
Janout, Markus
Loginova, Nadezhda
Trudnowska, Emilia
Horstmann, Cora
Wekerle, Claudia
Oziel, Laurent
Schourup-Kristensen, Vibe
Ruiz-Castillo, Eugenio
Schulz, Kirstin
V. Povazhnyy, Vasily
Iversen, Morten
Waite, Anya M.
author_sort Rogge, Andreas
title Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water
title_short Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water
title_full Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water
title_fullStr Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water
title_full_unstemmed Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water
title_sort carbon dioxide sink in the arctic ocean from cross-shelf transport of dense barents sea water
publishDate 2023
url https://pure.au.dk/portal/da/publications/carbon-dioxide-sink-in-the-arctic-ocean-from-crossshelf-transport-of-dense-barents-sea-water(df025c1d-2755-4caa-bdf0-c1dcfa8c281c).html
https://doi.org/10.1038/s41561-022-01069-z
genre Arctic
Arctic
Arctic Ocean
Barents Sea
Global warming
Nansen Basin
Sea ice
genre_facet Arctic
Arctic
Arctic Ocean
Barents Sea
Global warming
Nansen Basin
Sea ice
op_source Rogge , A , Janout , M , Loginova , N , Trudnowska , E , Horstmann , C , Wekerle , C , Oziel , L , Schourup-Kristensen , V , Ruiz-Castillo , E , Schulz , K , V. Povazhnyy , V , Iversen , M & Waite , A M 2023 , ' Carbon dioxide sink in the Arctic Ocean from cross-shelf transport of dense Barents Sea water ' , Nature Geoscience , vol. 16 , no. 1 , pp. 82-88 . https://doi.org/10.1038/s41561-022-01069-z
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