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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Autores principales: 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
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Lenguaje:EN
Publicado: Nature Portfolio 2020
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Acceso en línea:https://doaj.org/article/3f299475080246db8915ca16a290b70f
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spelling oai:doaj.org-article:3f299475080246db8915ca16a290b70f2021-12-02T19:16:55ZFrequent new particle formation over the high Arctic pack ice by enhanced iodine emissions10.1038/s41467-020-18551-02041-1723https://doaj.org/article/3f299475080246db8915ca16a290b70f2020-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-18551-0https://doaj.org/toc/2041-1723Which 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.Andrea BaccariniLinn KarlssonJosef DommenPatrick DuplessisJutta VüllersIan M. BrooksAlfonso Saiz-LopezMatthew SalterMichael TjernströmUrs BaltenspergerPaul ZiegerJulia SchmaleNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-11 (2020)
institution DOAJ
collection DOAJ
language EN
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
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
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://doaj.org/article/3f299475080246db8915ca16a290b70f
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