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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>3</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/amtd-3-637-2010</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/3/637/2010/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/3/637/2010/amtd-3-637-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/3/637/2010/amtd-3-637-2010.pdf</fulltext_pdf>
	<start_page>637</start_page>
	<end_page>674</end_page>
	<publication_date>2010-02-15</publication_date>
	<article_title content_type="html">Results and recommendations from an intercomparison of six Hygroscopicity-TDMA systems</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>A. Massling</name>
			<email>anma@dmu.dk</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>N. Niedermaier</name>
		</author>
		<author numeration="3" affiliations="1,3">
			<name>T. Hennig</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>E. Fors</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>E. Swietlicki</name>
		</author>
		<author numeration="6" affiliations="5">
			<name>M. Ehn</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>K. Hämeri</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>P. Villani</name>
		</author>
		<author numeration="9" affiliations="6">
			<name>P. Laj</name>
		</author>
		<author numeration="10" affiliations="7">
			<name>N. Good</name>
		</author>
		<author numeration="11" affiliations="7">
			<name>G. McFiggans</name>
		</author>
		<author numeration="12" affiliations="1">
			<name>A. Wiedensohler</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Leibniz Institute for Tropospheric Research, Leipzig, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Aarhus University, National Environmental Research Institute, Department of Atmospheric Environment, Roskilde, Denmark</affiliation>
		<affiliation numeration="3" content_type="html">Stockholm University, Department of Applied Environmental Science, Stockholm, Sweden</affiliation>
		<affiliation numeration="4" content_type="html">Lund University, Department of Physics, Lund, Sweden</affiliation>
		<affiliation numeration="5" content_type="html">University of Helsinki, Department of Physics, Helsinki, Finland</affiliation>
		<affiliation numeration="6" content_type="html">Université Blaise Pascal, Laboratoire de Météorologie Physique, Clermont Ferrand, France</affiliation>
		<affiliation numeration="7" content_type="html">University of Manchester, Department of Atmospheric and Environmental Sciences, Manchester, UK</affiliation>
	</affiliations>
	<abstract content_type="html">The performance of six custom-built Hygrocopicity-Tandem
Differential Mobility Analyzers (H-TDMA) systems was investigated in
the frame of an international calibration and intercomparison
workshop held in Leipzig, February 2006. The goal of the workshop
was to harmonize H-TDMA measurements and develop recommendations for
atmospheric measurements and their data evaluation. The H-TDMA
systems were compared in terms of the sizing of dry particles,
relative humidity (RH) uncertainty and consistency in determination
of number fractions of different hygroscopic particle groups. The
experiments were performed in an air-conditioned laboratory using
ammonium sulfate particles or an external mixture of ammonium
sulfate and soot particles.
&lt;br&gt;&lt;br&gt;
The sizing of dry particles of the six H-TDMA systems was within 0.2 to
4.2% of the selected particle diameter depending on investigated size and
individual system.
&lt;br&gt;&lt;br&gt;
With regard to RH uncertainties, the H-TDMA systems showed deviations up to
4.5% RH from the set point at RH=90% investigating the hygroscopic
growth of ammonium sulfate particles and comparing the results with theory.
&lt;br&gt;&lt;br&gt;
The evaluation of number fractions investigating an externally mixed aerosol
delivered differences up to +/&amp;minus;8% in calculated number fraction for one
and the same aerosol type.
&lt;br&gt;&lt;br&gt;
We analysed the datasets of the different H-TDMAs with one fitting
routine to investigate differences caused by the different data
evaluation procedures. The results showed that the differences were
reduced from +12/&amp;minus;13% to +8/&amp;minus;6%. We can conclude here that
a common data evaluation procedure to determine the number fraction
of externally mixed aerosols will improve the comparability of
H-TDMA measurements.
&lt;br&gt;&lt;br&gt;
We finally recommend, to ensure a good calibration of all flow,
temperature and RH sensors in the systems. It is most important to
thermally insulate the RH control unit and the second DMA and to
monitor those temperatures as accurately as 0.2 &amp;deg;C. For a
correct determination of external mixtures, it is necessary to take
into account size-dependent losses due to the diffusion in the
pluming between the DMAs and in the aerosol humidification unit.</abstract>
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</article>

