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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>4</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2004</publication_year>
	</journal>
	<doi>10.5194/acpd-4-3947-2004</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/4/3947/2004/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/4/3947/2004/acpd-4-3947-2004.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/4/3947/2004/acpd-4-3947-2004.pdf</fulltext_pdf>
	<start_page>3947</start_page>
	<end_page>3973</end_page>
	<publication_date>2004-07-20</publication_date>
	<article_title content_type="html">Ion production rate in a boreal forest based on ion, particle and radiation measurements</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>T. Petäjä</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>K. E. J. Lehtinen</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>M. Kulmala</name>
		</author>
		<author numeration="5" affiliations="2">
			<name>J. Paatero</name>
		</author>
		<author numeration="6" affiliations="3">
			<name>U. Hõrrak</name>
		</author>
		<author numeration="7" affiliations="3">
			<name>H. Tammet</name>
		</author>
		<author numeration="8" affiliations="4">
			<name>J. Joutsensaari</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Physical Sciences, P.O. Box 64, FIN-00014 University of Helsinki, Finland</affiliation>
		<affiliation numeration="2" content_type="html">Finnish Meteorological Institute, Air Quality Research, Sahaajankatu 20E, FIN-00880 Helsinki, Finland</affiliation>
		<affiliation numeration="3" content_type="html">Institute of Environmental Physics, University of Tartu, 18 U¨ likooli Street, Tartu, 50090, Estonia</affiliation>
		<affiliation numeration="4" content_type="html">Department of Applied Physics, University of Kuopio, P.O. Box 1627, FIN-70211 Kuopio, Finland</affiliation>
	</affiliations>
	<abstract content_type="html">In this study the ion production rates in a boreal forest are
studied based on two different methods: 1) cluster ion and
particle concentration measurements, 2) external radiation and
radon concentration measurements.  Both methods produce reasonable
estimates for ion production rates. The average ion production
rate calculated from aerosol particle size distribution and air
ion mobility distribution measurements was 2.6 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;
and based on external radiation and radon measurements
4.5 cm&lt;sup&gt;&amp;minus;3&lt;/sup&gt;s&lt;sup&gt;&amp;minus;1&lt;/sup&gt;. The first method based on ion and particle
measurements gave lower values for the ion production rates
especially during the day. A possible reason for this is that
particle measurements started only from 3 nm, so the sink of small
ions during the nucleation events was underestimated. Another
reason is that the possible fogs, which caused an extra sink of
small ions are not taken into account in the calculations. It may
also be possible that the hygroscopic growth factors of aerosol
particles were underestimated.  A fourth possible reason for the
discrepancy is the nucleation mechanism itself. If the ions were
somehow present in the nucleation process, there could have been
an additional ion sink during the nucleation days. On the other
hand, not all the radiation energy is converted to ions and the
possible effect of alpha recoil is also omitted.</abstract>
	<references>
	</references>
</article>

