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...
Published in: | Nature Geoscience |
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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 |
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Open Polar |
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Aarhus University: Research |
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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 |
op_relation |
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op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1038/s41561-022-01069-z |
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Nature Geoscience |
container_volume |
16 |
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1 |
container_start_page |
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op_container_end_page |
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