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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-8-3107-2008</article-id>
<title-group>
<article-title>Long-term solar UV radiation reconstructed by ANN modelling with emphasis on spatial characteristics of input data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Feister</surname>
<given-names>U.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Junk</surname>
<given-names>J.</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>Woldt</surname>
<given-names>M.</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>Bais</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Helbig</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Janouch</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Josefsson</surname>
<given-names>W.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kazantzidis</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lindfors</surname>
<given-names>A.</given-names>
</name>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>den Outer</surname>
<given-names>P. N.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Slaper</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff9">
<sup>9</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Deutscher Wetterdienst, Richard Aßmann Observatorium Lindenberg, Am Observatorium 12, 15848 Lindenberg, Germany</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Public Research Centre – Gabriel Lippmann, Department of Environment and Agro-Biotechnologies (EVA), 41, rue du Bril, 4422 Belvaux Grand-Duchy of Luxembourg, Luxembourg</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Brandenburgische Techn. Univ. Cottbus, Lehrstuhl für Umweltmeteorologie, Burger Chaussee 2, 03044 Cottbus, Germany</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Aristotle University of Thessaloniki, Laboratory of Atmospheric Physics, 54124, Thessaloniki, Greece</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Universität Trier, Fachbereich VI, Fach Umweltmeteorologie, 54286 Trier, Germany</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Solar and Ozone Observatory, Czech Hydrometeorological Inst., Hvezdarna 456, 500 08 Hradec Kralove 8, Czech Republic</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>Swedish Meteorological and Hydrological Institute, 60176, Norrköping, Sweden</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Finnish Meteorological Institute, P.O. BOX 503 (Erik Palmenin aukio 1), 00101 Helsinki, Finland</addr-line>
</aff>
<aff id="aff9">
<label>9</label>
<addr-line>National Institute for Public Health and the Environment, A. van Leeuwenhoeklaan 9, P.O. Box 1, 3720 BA Bilthoven, The Netherlands</addr-line>
</aff>
<pub-date pub-type="epub">
<day>23</day>
<month>06</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>12</issue>
<fpage>3107</fpage>
<lpage>3118</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>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/3107/2008/acp-8-3107-2008.html">This article is available from http://www.atmos-chem-phys.net/8/3107/2008/acp-8-3107-2008.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/8/3107/2008/acp-8-3107-2008.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/8/3107/2008/acp-8-3107-2008.pdf</self-uri>
<abstract>
<p>Artificial Neural Networks (ANN) are efficient tools to derive solar UV
radiation from measured meteorological parameters such as global radiation,
aerosol optical depths and atmospheric column ozone. The ANN model has been
tested with different combinations of data from the two sites Potsdam and
Lindenberg, and used to reconstruct solar UV radiation at eight European
sites by more than 100 years into the past. Special emphasis will be given
to the discussion of small-scale characteristics of input data to the ANN
model.
&lt;br&gt;&lt;br&gt;
Annual totals of UV radiation derived from reconstructed daily UV values
reflect interannual variations and long-term patterns that are compatible
with variabilities and changes of measured input data, in particular global
dimming by about 1980/1990, subsequent global brightening, volcanic eruption
effects such as that of Mt. Pinatubo, and the long-term ozone decline since
the 1970s. Patterns of annual erythemal UV radiation are very similar at
sites located at latitudes close to each other, but different patterns occur
between UV radiation at sites in different latitude regions.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>