New particle formation in the Svalbard region 2006-2015 ...
Events of new particle formation (NPF) were analyzed in a 10-year data set of hourly particle size distributions recorded on Mt. Zeppelin, Spitsbergen, Svalbard. Three different types of NPF events were identified through objective search algorithms. The first and simplest algorithm utilizes short-t...
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2017
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Online Access: | https://dx.doi.org/10.34657/11099 https://oa.tib.eu/renate/handle/123456789/12065 |
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ftdatacite:10.34657/11099 2023-06-11T04:09:02+02:00 New particle formation in the Svalbard region 2006-2015 ... Heintzenberg, Jost Tunved, Peter Galí, Martí Leck, Caroline 2017 https://dx.doi.org/10.34657/11099 https://oa.tib.eu/renate/handle/123456789/12065 en eng Katlenburg-Lindau : EGU Creative Commons Attribution 3.0 Unported CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 aerosol formation algorithm concentration composition haze particle size seasonal variation size distribution Arctic Greenland Spitsbergen Svalbard Svalbard and Jan Mayen Mink enteritis virus 550 CreativeWork article 2017 ftdatacite https://doi.org/10.34657/11099 2023-05-02T11:06:30Z Events of new particle formation (NPF) were analyzed in a 10-year data set of hourly particle size distributions recorded on Mt. Zeppelin, Spitsbergen, Svalbard. Three different types of NPF events were identified through objective search algorithms. The first and simplest algorithm utilizes short-term increases in particle concentrations below 25 nm (PCT (percentiles) events). The second one builds on the growth of the sub-50 nm diameter median (DGR (diameter growth) events) and is most closely related to the classical "banana type" of event. The third and most complex, multiple-size approach to identifying NPF events builds on a hypothesis suggesting the concurrent production of polymer gel particles at several sizes below ca. 60 nm (MEV (multisize growth) events). As a first and general conclusion, we can state that NPF events are a summer phenomenon and not related to Arctic haze, which is a late winter to early spring feature. The occurrence of NPF events appears to be somewhat sensitive to the ... Article in Journal/Newspaper Arctic Greenland Jan Mayen Svalbard Spitsbergen DataCite Metadata Store (German National Library of Science and Technology) Arctic Svalbard Greenland Jan Mayen Svalbard ENVELOPE(20.000,20.000,78.000,78.000) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
aerosol formation algorithm concentration composition haze particle size seasonal variation size distribution Arctic Greenland Spitsbergen Svalbard Svalbard and Jan Mayen Mink enteritis virus 550 |
spellingShingle |
aerosol formation algorithm concentration composition haze particle size seasonal variation size distribution Arctic Greenland Spitsbergen Svalbard Svalbard and Jan Mayen Mink enteritis virus 550 Heintzenberg, Jost Tunved, Peter Galí, Martí Leck, Caroline New particle formation in the Svalbard region 2006-2015 ... |
topic_facet |
aerosol formation algorithm concentration composition haze particle size seasonal variation size distribution Arctic Greenland Spitsbergen Svalbard Svalbard and Jan Mayen Mink enteritis virus 550 |
description |
Events of new particle formation (NPF) were analyzed in a 10-year data set of hourly particle size distributions recorded on Mt. Zeppelin, Spitsbergen, Svalbard. Three different types of NPF events were identified through objective search algorithms. The first and simplest algorithm utilizes short-term increases in particle concentrations below 25 nm (PCT (percentiles) events). The second one builds on the growth of the sub-50 nm diameter median (DGR (diameter growth) events) and is most closely related to the classical "banana type" of event. The third and most complex, multiple-size approach to identifying NPF events builds on a hypothesis suggesting the concurrent production of polymer gel particles at several sizes below ca. 60 nm (MEV (multisize growth) events). As a first and general conclusion, we can state that NPF events are a summer phenomenon and not related to Arctic haze, which is a late winter to early spring feature. The occurrence of NPF events appears to be somewhat sensitive to the ... |
format |
Article in Journal/Newspaper |
author |
Heintzenberg, Jost Tunved, Peter Galí, Martí Leck, Caroline |
author_facet |
Heintzenberg, Jost Tunved, Peter Galí, Martí Leck, Caroline |
author_sort |
Heintzenberg, Jost |
title |
New particle formation in the Svalbard region 2006-2015 ... |
title_short |
New particle formation in the Svalbard region 2006-2015 ... |
title_full |
New particle formation in the Svalbard region 2006-2015 ... |
title_fullStr |
New particle formation in the Svalbard region 2006-2015 ... |
title_full_unstemmed |
New particle formation in the Svalbard region 2006-2015 ... |
title_sort |
new particle formation in the svalbard region 2006-2015 ... |
publisher |
Katlenburg-Lindau : EGU |
publishDate |
2017 |
url |
https://dx.doi.org/10.34657/11099 https://oa.tib.eu/renate/handle/123456789/12065 |
long_lat |
ENVELOPE(20.000,20.000,78.000,78.000) |
geographic |
Arctic Svalbard Greenland Jan Mayen Svalbard |
geographic_facet |
Arctic Svalbard Greenland Jan Mayen Svalbard |
genre |
Arctic Greenland Jan Mayen Svalbard Spitsbergen |
genre_facet |
Arctic Greenland Jan Mayen Svalbard Spitsbergen |
op_rights |
Creative Commons Attribution 3.0 Unported CC BY 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_doi |
https://doi.org/10.34657/11099 |
_version_ |
1768382736560553984 |