The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide
Abstract Dimethyl sulphide (DMS) and carbon monoxide (CO) are climate-relevant trace gases that play key roles in the radiative budget of the Arctic atmosphere. Under global warming, Arctic sea ice retreats at an unprecedented rate, altering light penetration and biological communities, and potentia...
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Springer Science and Business Media LLC
2021
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crspringernat:10.1007/s13280-021-01612-z 2023-05-15T14:35:31+02:00 The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide Campen, Hanna I. Arévalo-Martínez, Damian L. Artioli, Yuri Brown, Ian J. Kitidis, Vassilis Lessin, Gennadi Rees, Andrew P. Bange, Hermann W. Natural Environment Research Council Bundesministerium für Bildung und Forschung GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel 2021 http://dx.doi.org/10.1007/s13280-021-01612-z https://link.springer.com/content/pdf/10.1007/s13280-021-01612-z.pdf https://link.springer.com/article/10.1007/s13280-021-01612-z/fulltext.html en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Ambio volume 51, issue 2, page 411-422 ISSN 0044-7447 1654-7209 Ecology Environmental Chemistry Geography, Planning and Development General Medicine journal-article 2021 crspringernat https://doi.org/10.1007/s13280-021-01612-z 2022-01-04T14:23:32Z Abstract Dimethyl sulphide (DMS) and carbon monoxide (CO) are climate-relevant trace gases that play key roles in the radiative budget of the Arctic atmosphere. Under global warming, Arctic sea ice retreats at an unprecedented rate, altering light penetration and biological communities, and potentially affect DMS and CO cycling in the Arctic Ocean. This could have socio-economic implications in and beyond the Arctic region. However, little is known about CO production pathways and emissions in this region and the future development of DMS and CO cycling. Here we summarize the current understanding and assess potential future changes of DMS and CO cycling in relation to changes in sea ice coverage, light penetration, bacterial and microalgal communities, pH and physical properties. We suggest that production of DMS and CO might increase with ice melting, increasing light availability and shifting phytoplankton community. Among others, policy measures should facilitate large-scale process studies, coordinated long term observations and modelling efforts to improve our current understanding of the cycling and emissions of DMS and CO in the Arctic Ocean and of global consequences. Article in Journal/Newspaper Arctic Arctic Ocean Global warming Phytoplankton Sea ice Springer Nature (via Crossref) Arctic Arctic Ocean Ambio 51 2 411 422 |
institution |
Open Polar |
collection |
Springer Nature (via Crossref) |
op_collection_id |
crspringernat |
language |
English |
topic |
Ecology Environmental Chemistry Geography, Planning and Development General Medicine |
spellingShingle |
Ecology Environmental Chemistry Geography, Planning and Development General Medicine Campen, Hanna I. Arévalo-Martínez, Damian L. Artioli, Yuri Brown, Ian J. Kitidis, Vassilis Lessin, Gennadi Rees, Andrew P. Bange, Hermann W. The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide |
topic_facet |
Ecology Environmental Chemistry Geography, Planning and Development General Medicine |
description |
Abstract Dimethyl sulphide (DMS) and carbon monoxide (CO) are climate-relevant trace gases that play key roles in the radiative budget of the Arctic atmosphere. Under global warming, Arctic sea ice retreats at an unprecedented rate, altering light penetration and biological communities, and potentially affect DMS and CO cycling in the Arctic Ocean. This could have socio-economic implications in and beyond the Arctic region. However, little is known about CO production pathways and emissions in this region and the future development of DMS and CO cycling. Here we summarize the current understanding and assess potential future changes of DMS and CO cycling in relation to changes in sea ice coverage, light penetration, bacterial and microalgal communities, pH and physical properties. We suggest that production of DMS and CO might increase with ice melting, increasing light availability and shifting phytoplankton community. Among others, policy measures should facilitate large-scale process studies, coordinated long term observations and modelling efforts to improve our current understanding of the cycling and emissions of DMS and CO in the Arctic Ocean and of global consequences. |
author2 |
Natural Environment Research Council Bundesministerium für Bildung und Forschung GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel |
format |
Article in Journal/Newspaper |
author |
Campen, Hanna I. Arévalo-Martínez, Damian L. Artioli, Yuri Brown, Ian J. Kitidis, Vassilis Lessin, Gennadi Rees, Andrew P. Bange, Hermann W. |
author_facet |
Campen, Hanna I. Arévalo-Martínez, Damian L. Artioli, Yuri Brown, Ian J. Kitidis, Vassilis Lessin, Gennadi Rees, Andrew P. Bange, Hermann W. |
author_sort |
Campen, Hanna I. |
title |
The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide |
title_short |
The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide |
title_full |
The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide |
title_fullStr |
The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide |
title_full_unstemmed |
The role of a changing Arctic Ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide |
title_sort |
role of a changing arctic ocean and climate for the biogeochemical cycling of dimethyl sulphide and carbon monoxide |
publisher |
Springer Science and Business Media LLC |
publishDate |
2021 |
url |
http://dx.doi.org/10.1007/s13280-021-01612-z https://link.springer.com/content/pdf/10.1007/s13280-021-01612-z.pdf https://link.springer.com/article/10.1007/s13280-021-01612-z/fulltext.html |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean Global warming Phytoplankton Sea ice |
genre_facet |
Arctic Arctic Ocean Global warming Phytoplankton Sea ice |
op_source |
Ambio volume 51, issue 2, page 411-422 ISSN 0044-7447 1654-7209 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1007/s13280-021-01612-z |
container_title |
Ambio |
container_volume |
51 |
container_issue |
2 |
container_start_page |
411 |
op_container_end_page |
422 |
_version_ |
1766308328074379264 |