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	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>8</volume_number>
		<issue_number>16</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acp-8-4823-2008</doi>
	<article_url>http://www.atmos-chem-phys.net/8/4823/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/8/4823/2008/acp-8-4823-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/8/4823/2008/acp-8-4823-2008.pdf</fulltext_pdf>
	<start_page>4823</start_page>
	<end_page>4839</end_page>
	<publication_date>2008-08-19</publication_date>
	<article_title content_type="html">Basic characteristics of atmospheric particles, trace gases and meteorology in a relatively clean Southern African Savannah environment</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>L. Laakso</name>
			<email>lauri.laakso@iki.fi</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>H. Laakso</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>P. P. Aalto</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>P. Keronen</name>
		</author>
		<author numeration="5" affiliations="1,2">
			<name>T. Petäjä</name>
		</author>
		<author numeration="6" affiliations="1">
			<name>T. Nieminen</name>
		</author>
		<author numeration="7" affiliations="1">
			<name>T. Pohja</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>E. Siivola</name>
		</author>
		<author numeration="9" affiliations="1">
			<name>M. Kulmala</name>
		</author>
		<author numeration="10" affiliations="3">
			<name>N. Kgabi</name>
		</author>
		<author numeration="11" affiliations="3">
			<name>M. Molefe</name>
		</author>
		<author numeration="12" affiliations="3">
			<name>D. Mabaso</name>
		</author>
		<author numeration="13" affiliations="4">
			<name>D. Phalatse</name>
		</author>
		<author numeration="14" affiliations="5">
			<name>K. Pienaar</name>
		</author>
		<author numeration="15" affiliations="6">
			<name>V.-M. Kerminen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Physical Sciences, University of Helsinki, P. O. BOX 64, 00014 Helsinki, Finland</affiliation>
		<affiliation numeration="2" content_type="html">Earth and Sun Systems Laboratory, Atmospheric Chemistry Division, Nat. Center for Atmospheric Res., Boulder, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Physics, North-West University, Private Bag X 2046, Mmabatho, South Africa</affiliation>
		<affiliation numeration="4" content_type="html">Department of Biology, North-West University, Private Bag X 2046, Mmabatho, South Africa</affiliation>
		<affiliation numeration="5" content_type="html">School of Chemistry, North-West University, Private Bag X 6001, Potchefstroom, South Africa</affiliation>
		<affiliation numeration="6" content_type="html">Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">We have analyzed one year (July 2006–July 2007) of measurement data from
a relatively clean background site located in dry savannah in South Africa.
The annual-median trace gas concentrations were equal to 0.7 ppb for
SO&lt;sub&gt;2&lt;/sub&gt;, 1.4 ppb for NO&lt;sub&gt;x&lt;/sub&gt;, 36 ppb for O&lt;sub&gt;3&lt;/sub&gt; and 105 ppb for CO. The
corresponding PM&lt;sub&gt;1&lt;/sub&gt;, PM&lt;sub&gt;2.5&lt;/sub&gt; and PM&lt;sub&gt;10&lt;/sub&gt; concentrations were 9.0,
10.5 and 18.8 μg m&lt;sup&gt;&amp;minus;3&lt;/sup&gt;, and the annual median total particle number
concentration in the size range 10–840 nm was 2340 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;. During
Easterly winds, influence of industrial sources approximately 150 km away
from the measurement site was clearly visible, especially in SO&lt;sub&gt;2&lt;/sub&gt; and
NO&lt;sub&gt;x&lt;/sub&gt; concentrations. Of gases, NO&lt;sub&gt;x&lt;/sub&gt; and CO had a clear annual, and
SO&lt;sub&gt;2&lt;/sub&gt;, NO&lt;sub&gt;x&lt;/sub&gt; and O&lt;sub&gt;3&lt;/sub&gt; clear diurnal cycle.

Atmospheric new-particle formation was observed to take place in more than
90% of the analyzed days. The days with no new particle formation were
cloudy or rainy days. The formation rate of 10 nm particles varied in the
range of 0.1–28 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt; (median 1.9 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt; s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;) and
nucleation mode particle growth rates were in the range 3–21 nm h&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
(median 8.5 nm h&lt;sup&gt;&amp;minus;1&lt;/sup&gt;). Due to high formation and growth rates, observed
new particle formation gives a significant contribute to the number of cloud
condensation nuclei budget, having a potential to affect the regional
climate forcing patterns.</abstract>
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</article>

