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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-12-3687-2012</article-id>
<title-group>
<article-title>Characterization of ions at Alpine waterfalls</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kolarž</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gaisberger</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Madl</surname>
<given-names>P.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hofmann</surname>
<given-names>W.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ritter</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hartl</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Physics, University of Belgrade, Pregrevica 118, 11080 Belgrade, Serbia</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Institute of Physiology and Pathophysiology, Paracelsus Medical University, Strubergasse 21, 5020 Salzburg, Austria</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Materials Research and Physics, Division of Physics and Biophysics, University of Salzburg, Hellbrunner Str. 34, 5020 Salzburg, Austria</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>These authors contributed equally to this work</addr-line>
</aff>
<pub-date pub-type="epub">
<day>24</day>
<month>04</month>
<year>2012</year>
</pub-date>
<volume>12</volume>
<issue>8</issue>
<fpage>3687</fpage>
<lpage>3697</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
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<self-uri xlink:href="http://www.atmos-chem-phys.net/12/3687/2012/acp-12-3687-2012.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/12/3687/2012/acp-12-3687-2012.pdf</self-uri>
<abstract>
<p>During a three-year field campaign of measuring waterfall generated ions, we
monitored five different waterfalls in the Austrian Alps. Most measurements
were performed at the Krimml waterfall (Salzburg, Austria), which is the
biggest waterfall in Europe, and the Gartl waterfall (Mölltal, Austria).
We characterized spatial, time and size distributions of waterfall-generated
ions under the influence of surrounding topography. The smallest ions with
boundary diameters of 0.9, 1.5 and 2 nm, were measured with a cylindrical
air ion detector (CDI-06), while ion sizes from 5.5 to 350 nm were measured
using a modified Grimm SMPS aerosol spectrometer. High negative ion
concentration gradients are detected in the vicinity of the waterfalls,
whereas the increase of positive ions was only moderate. Ions in the nano
range were the most abundant at 2 nm, and at 120 nm in the sub-micrometer
range.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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