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New particle formation and sub-10 nm size distribution measurements during the A-LIFE field experiment in Paphos, Cyprus
Atmospheric particle size distributions were measured in Paphos, Cyprus, during the A-LIFE (absorbing aerosol layers in a changing climate: ageing, lifetime and dynamics) field experiment from 3 to 30 April 2017. The newly developed differential mobility analyser train (DMA-train) was deployed for t...
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Published in: | Atmospheric chemistry and physics 2020-05, Vol.20 (9), p.5645-5656 |
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creator | Brilke, Sophia Fölker, Nikolaus Müller, Thomas Kandler, Konrad Gong, Xianda Peischl, Jeff Weinzierl, Bernadett Winkler, Paul M |
description | Atmospheric particle size distributions were measured in
Paphos, Cyprus, during the A-LIFE (absorbing aerosol layers in a
changing climate: ageing, lifetime and dynamics) field experiment
from 3 to 30 April 2017. The newly developed differential
mobility analyser train (DMA-train) was deployed for the
first time in an atmospheric environment for the direct measurement of the
nucleation mode size range between 1.8 and 10 nm diameter. The DMA-train
set-up consists of seven size channels, of which five are set to fixed
particle mobility diameters and two additional diameters are obtained by
alternating voltage settings in one DMA every 10 s. In combination with a
conventional mobility particle size spectrometer (MPSS) and an aerodynamic
particle sizer (APS) the complete atmospheric aerosol size distribution from
1.8 nm to 10 µm was covered. The focus of the A-LIFE study was to
characterize new particle formation (NPF) in the eastern Mediterranean
region at a measurement site with strong local pollution sources. The nearby
Paphos airport was found to be a large emission source for nucleation mode
particles, and we analysed the size distribution of the airport emission
plumes at approximately 500 m from the main runway. The analysis yielded nine
NPF events in 27 measurement days from the combined analysis of the
DMA-train, MPSS and trace gas monitors. Growth rate calculations were
performed, and a size dependency of the initial growth rate ( |
doi_str_mv | 10.5194/acp-20-5645-2020 |
format | article |
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Paphos, Cyprus, during the A-LIFE (absorbing aerosol layers in a
changing climate: ageing, lifetime and dynamics) field experiment
from 3 to 30 April 2017. The newly developed differential
mobility analyser train (DMA-train) was deployed for the
first time in an atmospheric environment for the direct measurement of the
nucleation mode size range between 1.8 and 10 nm diameter. The DMA-train
set-up consists of seven size channels, of which five are set to fixed
particle mobility diameters and two additional diameters are obtained by
alternating voltage settings in one DMA every 10 s. In combination with a
conventional mobility particle size spectrometer (MPSS) and an aerodynamic
particle sizer (APS) the complete atmospheric aerosol size distribution from
1.8 nm to 10 µm was covered. The focus of the A-LIFE study was to
characterize new particle formation (NPF) in the eastern Mediterranean
region at a measurement site with strong local pollution sources. The nearby
Paphos airport was found to be a large emission source for nucleation mode
particles, and we analysed the size distribution of the airport emission
plumes at approximately 500 m from the main runway. The analysis yielded nine
NPF events in 27 measurement days from the combined analysis of the
DMA-train, MPSS and trace gas monitors. Growth rate calculations were
performed, and a size dependency of the initial growth rate (<10 nm)
was observed for one event case. Fast changes of the sub-10 nm size
distribution on a timescale of a few minutes were captured by the
DMA-train measurement during early particle growth and are discussed in a
second event case. In two cases, particle formation and growth were detected
in the nucleation mode size range which did not exceed the 10 nm threshold.
This finding implies that NPF likely occurs more frequently than estimated
from studies where the lower nanometre size regime is not covered by the
size distribution measurements.</description><identifier>ISSN: 1680-7324</identifier><identifier>ISSN: 1680-7316</identifier><identifier>EISSN: 1680-7324</identifier><identifier>DOI: 10.5194/acp-20-5645-2020</identifier><language>eng</language><publisher>Katlenburg-Lindau: Copernicus GmbH</publisher><subject>Aerosol layers ; Aerosol size distribution ; Aerosols ; Ageing ; Aging ; Airports ; Atmospheric physics ; Charged particles ; Climate change ; Diameters ; Emission analysis ; Emissions ; Growth rate ; Humidity ; Measurement ; Mobility ; Nucleation ; Particle formation ; Particle size ; Particle size distribution ; Plumes ; Pollution ; Pollution sources ; Runways ; Sensors ; Setting (Literature) ; Size distribution ; Time ; Trace gases</subject><ispartof>Atmospheric chemistry and physics, 2020-05, Vol.20 (9), p.5645-5656</ispartof><rights>COPYRIGHT 2020 Copernicus GmbH</rights><rights>2020. This work is published under https://creativecommons.org/licenses/by/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c410t-dc9d7c26310e37162650cd4219e4f198fd9cc11ffe26cda91b5c5b0049b89e103</citedby><cites>FETCH-LOGICAL-c410t-dc9d7c26310e37162650cd4219e4f198fd9cc11ffe26cda91b5c5b0049b89e103</cites><orcidid>0000-0003-3133-249X ; 0000-0002-9320-7101 ; 0000-0001-7274-0639 ; 0000-0003-4555-5686</orcidid></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.proquest.com/docview/2414756733/fulltextPDF?pq-origsite=primo$$EPDF$$P50$$Gproquest$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.proquest.com/docview/2414756733?pq-origsite=primo$$EHTML$$P50$$Gproquest$$Hfree_for_read</linktohtml><link.rule.ids>314,776,780,860,2095,25732,27903,27904,36991,44569,74873</link.rule.ids></links><search><creatorcontrib>Brilke, Sophia</creatorcontrib><creatorcontrib>Fölker, Nikolaus</creatorcontrib><creatorcontrib>Müller, Thomas</creatorcontrib><creatorcontrib>Kandler, Konrad</creatorcontrib><creatorcontrib>Gong, Xianda</creatorcontrib><creatorcontrib>Peischl, Jeff</creatorcontrib><creatorcontrib>Weinzierl, Bernadett</creatorcontrib><creatorcontrib>Winkler, Paul M</creatorcontrib><title>New particle formation and sub-10 nm size distribution measurements during the A-LIFE field experiment in Paphos, Cyprus</title><title>Atmospheric chemistry and physics</title><description>Atmospheric particle size distributions were measured in
Paphos, Cyprus, during the A-LIFE (absorbing aerosol layers in a
changing climate: ageing, lifetime and dynamics) field experiment
from 3 to 30 April 2017. The newly developed differential
mobility analyser train (DMA-train) was deployed for the
first time in an atmospheric environment for the direct measurement of the
nucleation mode size range between 1.8 and 10 nm diameter. The DMA-train
set-up consists of seven size channels, of which five are set to fixed
particle mobility diameters and two additional diameters are obtained by
alternating voltage settings in one DMA every 10 s. In combination with a
conventional mobility particle size spectrometer (MPSS) and an aerodynamic
particle sizer (APS) the complete atmospheric aerosol size distribution from
1.8 nm to 10 µm was covered. The focus of the A-LIFE study was to
characterize new particle formation (NPF) in the eastern Mediterranean
region at a measurement site with strong local pollution sources. The nearby
Paphos airport was found to be a large emission source for nucleation mode
particles, and we analysed the size distribution of the airport emission
plumes at approximately 500 m from the main runway. The analysis yielded nine
NPF events in 27 measurement days from the combined analysis of the
DMA-train, MPSS and trace gas monitors. Growth rate calculations were
performed, and a size dependency of the initial growth rate (<10 nm)
was observed for one event case. Fast changes of the sub-10 nm size
distribution on a timescale of a few minutes were captured by the
DMA-train measurement during early particle growth and are discussed in a
second event case. In two cases, particle formation and growth were detected
in the nucleation mode size range which did not exceed the 10 nm threshold.
This finding implies that NPF likely occurs more frequently than estimated
from studies where the lower nanometre size regime is not covered by the
size distribution measurements.</description><subject>Aerosol layers</subject><subject>Aerosol size distribution</subject><subject>Aerosols</subject><subject>Ageing</subject><subject>Aging</subject><subject>Airports</subject><subject>Atmospheric physics</subject><subject>Charged particles</subject><subject>Climate change</subject><subject>Diameters</subject><subject>Emission analysis</subject><subject>Emissions</subject><subject>Growth rate</subject><subject>Humidity</subject><subject>Measurement</subject><subject>Mobility</subject><subject>Nucleation</subject><subject>Particle formation</subject><subject>Particle size</subject><subject>Particle size distribution</subject><subject>Plumes</subject><subject>Pollution</subject><subject>Pollution sources</subject><subject>Runways</subject><subject>Sensors</subject><subject>Setting (Literature)</subject><subject>Size distribution</subject><subject>Time</subject><subject>Trace gases</subject><issn>1680-7324</issn><issn>1680-7316</issn><issn>1680-7324</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2020</creationdate><recordtype>article</recordtype><sourceid>PIMPY</sourceid><sourceid>DOA</sourceid><recordid>eNptkk2LFDEQhhtRcF29ewx4EuzdfHfnOAy7OjCs4sc5pJPKbIbpTpt0sx8nr_5Nf4mZnUUdkDpUUTz18ha8VfWa4DNBFD83dqwproXkonSKn1QnRLa4bhjlT_-Zn1cvct5iTAUm_KS6v4IbNJo0BbsD5GPqzRTigMzgUJ67muBfP34OPcrhHpALeUqhmx-IHkyeE_QwTBm5OYVhg6ZrQIt6vbq8QD7AziG4HSGFPYPCgD6Z8Trmd2h5N6Y5v6yeebPL8Oqxn1bfLi--Lj_U64_vV8vFurac4Kl2VrnGUskIBtYQSaXA1nFKFHBPVOudspYQ74FK64winbCiw5irrlVAMDutVgddF81Wj8WOSXc6mqAfFjFt9OP_GhsmG6AWK8W596ptOeGSMI49EdTLovXmoDWm-H2GPOltnNNQ7Gta0EbIhrG_1MYU0TD4OCVj-5CtXkjKGkFb2hTq7D9UKQd9sHEAH8r-6ODt0UFhJridNmbOWa--fD5m8YG1KeacwP95nGC9D4wugdG0zCUweh8Y9htNJLFp</recordid><startdate>20200513</startdate><enddate>20200513</enddate><creator>Brilke, Sophia</creator><creator>Fölker, Nikolaus</creator><creator>Müller, Thomas</creator><creator>Kandler, 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particle formation and sub-10 nm size distribution measurements during the A-LIFE field experiment in Paphos, Cyprus</title><author>Brilke, Sophia ; Fölker, Nikolaus ; Müller, Thomas ; Kandler, Konrad ; Gong, Xianda ; Peischl, Jeff ; Weinzierl, Bernadett ; Winkler, Paul M</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c410t-dc9d7c26310e37162650cd4219e4f198fd9cc11ffe26cda91b5c5b0049b89e103</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2020</creationdate><topic>Aerosol layers</topic><topic>Aerosol size distribution</topic><topic>Aerosols</topic><topic>Ageing</topic><topic>Aging</topic><topic>Airports</topic><topic>Atmospheric physics</topic><topic>Charged particles</topic><topic>Climate change</topic><topic>Diameters</topic><topic>Emission analysis</topic><topic>Emissions</topic><topic>Growth 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A-LIFE field experiment in Paphos, Cyprus</atitle><jtitle>Atmospheric chemistry and physics</jtitle><date>2020-05-13</date><risdate>2020</risdate><volume>20</volume><issue>9</issue><spage>5645</spage><epage>5656</epage><pages>5645-5656</pages><issn>1680-7324</issn><issn>1680-7316</issn><eissn>1680-7324</eissn><abstract>Atmospheric particle size distributions were measured in
Paphos, Cyprus, during the A-LIFE (absorbing aerosol layers in a
changing climate: ageing, lifetime and dynamics) field experiment
from 3 to 30 April 2017. The newly developed differential
mobility analyser train (DMA-train) was deployed for the
first time in an atmospheric environment for the direct measurement of the
nucleation mode size range between 1.8 and 10 nm diameter. The DMA-train
set-up consists of seven size channels, of which five are set to fixed
particle mobility diameters and two additional diameters are obtained by
alternating voltage settings in one DMA every 10 s. In combination with a
conventional mobility particle size spectrometer (MPSS) and an aerodynamic
particle sizer (APS) the complete atmospheric aerosol size distribution from
1.8 nm to 10 µm was covered. The focus of the A-LIFE study was to
characterize new particle formation (NPF) in the eastern Mediterranean
region at a measurement site with strong local pollution sources. The nearby
Paphos airport was found to be a large emission source for nucleation mode
particles, and we analysed the size distribution of the airport emission
plumes at approximately 500 m from the main runway. The analysis yielded nine
NPF events in 27 measurement days from the combined analysis of the
DMA-train, MPSS and trace gas monitors. Growth rate calculations were
performed, and a size dependency of the initial growth rate (<10 nm)
was observed for one event case. Fast changes of the sub-10 nm size
distribution on a timescale of a few minutes were captured by the
DMA-train measurement during early particle growth and are discussed in a
second event case. In two cases, particle formation and growth were detected
in the nucleation mode size range which did not exceed the 10 nm threshold.
This finding implies that NPF likely occurs more frequently than estimated
from studies where the lower nanometre size regime is not covered by the
size distribution measurements.</abstract><cop>Katlenburg-Lindau</cop><pub>Copernicus GmbH</pub><doi>10.5194/acp-20-5645-2020</doi><tpages>12</tpages><orcidid>https://orcid.org/0000-0003-3133-249X</orcidid><orcidid>https://orcid.org/0000-0002-9320-7101</orcidid><orcidid>https://orcid.org/0000-0001-7274-0639</orcidid><orcidid>https://orcid.org/0000-0003-4555-5686</orcidid><oa>free_for_read</oa></addata></record> |
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subjects | Aerosol layers Aerosol size distribution Aerosols Ageing Aging Airports Atmospheric physics Charged particles Climate change Diameters Emission analysis Emissions Growth rate Humidity Measurement Mobility Nucleation Particle formation Particle size Particle size distribution Plumes Pollution Pollution sources Runways Sensors Setting (Literature) Size distribution Time Trace gases |
title | New particle formation and sub-10 nm size distribution measurements during the A-LIFE field experiment in Paphos, Cyprus |
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