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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Main Authors: Wiedensohler, A., Ma, N., Birmili, W., Heintzenberg, J., Ditas, F., Andreae, M.O., Panov, A.
Format: Article in Journal/Newspaper
Language:English
Published: Amsterdam [u.a.] : Elsevier Science 2018
Subjects:
550
690
Online Access:https://oa.tib.eu/renate/handle/123456789/6985
https://doi.org/10.34657/6032
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spelling ftleibnizopen:oai:oai.leibnizopen.de:3zA974cBdbrxVwz6WckA 2023-06-11T04:17:14+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 application/pdf https://oa.tib.eu/renate/handle/123456789/6985 https://doi.org/10.34657/6032 eng eng Amsterdam [u.a.] : Elsevier Science CC BY 4.0 Unported https://creativecommons.org/licenses/by/4.0/ Atmospheric environment 200 (2019) 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 observatory size distribution article concentration (parameters) height Russian Federation taiga Siberia 550 690 article Text 2018 ftleibnizopen https://doi.org/10.34657/6032 2023-05-07T23:28:24Z 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 publishedVersion Article in Journal/Newspaper taiga Siberia LeibnizOpen (The Leibniz Association)
institution Open Polar
collection LeibnizOpen (The Leibniz Association)
op_collection_id ftleibnizopen
language English
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
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
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
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 publishedVersion
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://oa.tib.eu/renate/handle/123456789/6985
https://doi.org/10.34657/6032
genre taiga
Siberia
genre_facet taiga
Siberia
op_source Atmospheric environment 200 (2019)
op_rights CC BY 4.0 Unported
https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.34657/6032
_version_ 1768376193870987264