Infrequent new particle formation over the remote boreal forest of Siberia
Aerosol particle number size distributions (PNSD) were investigated to verify, if extremely low-volatility organic vapors (ELVOC) from natural sources alone could induce new particle formation and growth events over the remote boreal forest region of Siberia, hundreds of kilometers away from signifi...
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2018
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Online Access: | https://dx.doi.org/10.34657/6032 https://oa.tib.eu/renate/handle/123456789/6985 |
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ftdatacite:10.34657/6032 2023-05-15T18:30:45+02:00 Infrequent new particle formation over the remote boreal forest of Siberia Wiedensohler, A. Ma, N. Birmili, W. Heintzenberg, J. Ditas, F. Andreae, M.O. Panov, A. 2018 https://dx.doi.org/10.34657/6032 https://oa.tib.eu/renate/handle/123456789/6985 unknown Amsterdam [u.a.] : Elsevier Science Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Boundary layers Nucleation Observatories Aerosol particles Anthropogenic sources Condensational growth Homogeneous nucleation Natural sources New particle formation Particle number concentration Planetary boundary layers Forestry aerosol anthropogenic source boreal forest boundary layer forest cover nucleation observatory size distribution article concentration parameters height Russian Federation taiga Siberia 550 690 CreativeWork article 2018 ftdatacite https://doi.org/10.34657/6032 2022-03-10T12:43:22Z Aerosol particle number size distributions (PNSD) were investigated to verify, if extremely low-volatility organic vapors (ELVOC) from natural sources alone could induce new particle formation and growth events over the remote boreal forest region of Siberia, hundreds of kilometers away from significant anthropogenic sources. We re-evaluated observations determined at a height of 300 m of the remote observatory ZOTTO (Zotino Tall Tower Observatory, http://www.zottoproject.org). We found that new particle formation events occurred only on 11 days in a 3-year period, suggesting that homogeneous nucleation with a subsequent condensational growth could not be the major process, maintaining the particle number concentration in the planetary boundary layer of the remote boreal forest area of Siberia. © 2018 Elsevier Ltd Article in Journal/Newspaper taiga Siberia DataCite Metadata Store (German National Library of Science and Technology) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Boundary layers Nucleation Observatories Aerosol particles Anthropogenic sources Condensational growth Homogeneous nucleation Natural sources New particle formation Particle number concentration Planetary boundary layers Forestry aerosol anthropogenic source boreal forest boundary layer forest cover nucleation observatory size distribution article concentration parameters height Russian Federation taiga Siberia 550 690 |
spellingShingle |
Boundary layers Nucleation Observatories Aerosol particles Anthropogenic sources Condensational growth Homogeneous nucleation Natural sources New particle formation Particle number concentration Planetary boundary layers Forestry aerosol anthropogenic source boreal forest boundary layer forest cover nucleation observatory size distribution article concentration parameters height Russian Federation taiga Siberia 550 690 Wiedensohler, A. Ma, N. Birmili, W. Heintzenberg, J. Ditas, F. Andreae, M.O. Panov, A. Infrequent new particle formation over the remote boreal forest of Siberia |
topic_facet |
Boundary layers Nucleation Observatories Aerosol particles Anthropogenic sources Condensational growth Homogeneous nucleation Natural sources New particle formation Particle number concentration Planetary boundary layers Forestry aerosol anthropogenic source boreal forest boundary layer forest cover nucleation observatory size distribution article concentration parameters height Russian Federation taiga Siberia 550 690 |
description |
Aerosol particle number size distributions (PNSD) were investigated to verify, if extremely low-volatility organic vapors (ELVOC) from natural sources alone could induce new particle formation and growth events over the remote boreal forest region of Siberia, hundreds of kilometers away from significant anthropogenic sources. We re-evaluated observations determined at a height of 300 m of the remote observatory ZOTTO (Zotino Tall Tower Observatory, http://www.zottoproject.org). We found that new particle formation events occurred only on 11 days in a 3-year period, suggesting that homogeneous nucleation with a subsequent condensational growth could not be the major process, maintaining the particle number concentration in the planetary boundary layer of the remote boreal forest area of Siberia. © 2018 Elsevier Ltd |
format |
Article in Journal/Newspaper |
author |
Wiedensohler, A. Ma, N. Birmili, W. Heintzenberg, J. Ditas, F. Andreae, M.O. Panov, A. |
author_facet |
Wiedensohler, A. Ma, N. Birmili, W. Heintzenberg, J. Ditas, F. Andreae, M.O. Panov, A. |
author_sort |
Wiedensohler, A. |
title |
Infrequent new particle formation over the remote boreal forest of Siberia |
title_short |
Infrequent new particle formation over the remote boreal forest of Siberia |
title_full |
Infrequent new particle formation over the remote boreal forest of Siberia |
title_fullStr |
Infrequent new particle formation over the remote boreal forest of Siberia |
title_full_unstemmed |
Infrequent new particle formation over the remote boreal forest of Siberia |
title_sort |
infrequent new particle formation over the remote boreal forest of siberia |
publisher |
Amsterdam [u.a.] : Elsevier Science |
publishDate |
2018 |
url |
https://dx.doi.org/10.34657/6032 https://oa.tib.eu/renate/handle/123456789/6985 |
genre |
taiga Siberia |
genre_facet |
taiga Siberia |
op_rights |
Creative Commons Attribution 4.0 International CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.34657/6032 |
_version_ |
1766214331414872064 |