Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions
Which vapors are responsible for new particle formation in the Arctic is largely unknown. Here, the authors show that the formation of new particles at the central Arctic Ocean is mainly driven by iodic acid and that particles smaller than 30 nm in diameter can activate as cloud condensation nuclei.
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ftdoajarticles:oai:doaj.org/article:3f299475080246db8915ca16a290b70f 2023-05-15T14:33:40+02:00 Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions Andrea Baccarini Linn Karlsson Josef Dommen Patrick Duplessis Jutta Vüllers Ian M. Brooks Alfonso Saiz-Lopez Matthew Salter Michael Tjernström Urs Baltensperger Paul Zieger Julia Schmale 2020-10-01T00:00:00Z https://doi.org/10.1038/s41467-020-18551-0 https://doaj.org/article/3f299475080246db8915ca16a290b70f EN eng Nature Portfolio https://doi.org/10.1038/s41467-020-18551-0 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-020-18551-0 2041-1723 https://doaj.org/article/3f299475080246db8915ca16a290b70f Nature Communications, Vol 11, Iss 1, Pp 1-11 (2020) Science Q article 2020 ftdoajarticles https://doi.org/10.1038/s41467-020-18551-0 2022-12-31T11:18:28Z Which vapors are responsible for new particle formation in the Arctic is largely unknown. Here, the authors show that the formation of new particles at the central Arctic Ocean is mainly driven by iodic acid and that particles smaller than 30 nm in diameter can activate as cloud condensation nuclei. Article in Journal/Newspaper Arctic Arctic Ocean Directory of Open Access Journals: DOAJ Articles Arctic Arctic Ocean Nature Communications 11 1 |
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Open Polar |
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Directory of Open Access Journals: DOAJ Articles |
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ftdoajarticles |
language |
English |
topic |
Science Q |
spellingShingle |
Science Q Andrea Baccarini Linn Karlsson Josef Dommen Patrick Duplessis Jutta Vüllers Ian M. Brooks Alfonso Saiz-Lopez Matthew Salter Michael Tjernström Urs Baltensperger Paul Zieger Julia Schmale Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions |
topic_facet |
Science Q |
description |
Which vapors are responsible for new particle formation in the Arctic is largely unknown. Here, the authors show that the formation of new particles at the central Arctic Ocean is mainly driven by iodic acid and that particles smaller than 30 nm in diameter can activate as cloud condensation nuclei. |
format |
Article in Journal/Newspaper |
author |
Andrea Baccarini Linn Karlsson Josef Dommen Patrick Duplessis Jutta Vüllers Ian M. Brooks Alfonso Saiz-Lopez Matthew Salter Michael Tjernström Urs Baltensperger Paul Zieger Julia Schmale |
author_facet |
Andrea Baccarini Linn Karlsson Josef Dommen Patrick Duplessis Jutta Vüllers Ian M. Brooks Alfonso Saiz-Lopez Matthew Salter Michael Tjernström Urs Baltensperger Paul Zieger Julia Schmale |
author_sort |
Andrea Baccarini |
title |
Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions |
title_short |
Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions |
title_full |
Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions |
title_fullStr |
Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions |
title_full_unstemmed |
Frequent new particle formation over the high Arctic pack ice by enhanced iodine emissions |
title_sort |
frequent new particle formation over the high arctic pack ice by enhanced iodine emissions |
publisher |
Nature Portfolio |
publishDate |
2020 |
url |
https://doi.org/10.1038/s41467-020-18551-0 https://doaj.org/article/3f299475080246db8915ca16a290b70f |
geographic |
Arctic Arctic Ocean |
geographic_facet |
Arctic Arctic Ocean |
genre |
Arctic Arctic Ocean |
genre_facet |
Arctic Arctic Ocean |
op_source |
Nature Communications, Vol 11, Iss 1, Pp 1-11 (2020) |
op_relation |
https://doi.org/10.1038/s41467-020-18551-0 https://doaj.org/toc/2041-1723 doi:10.1038/s41467-020-18551-0 2041-1723 https://doaj.org/article/3f299475080246db8915ca16a290b70f |
op_doi |
https://doi.org/10.1038/s41467-020-18551-0 |
container_title |
Nature Communications |
container_volume |
11 |
container_issue |
1 |
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1766306879806373888 |