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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</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/acpd-8-47-2008</article-id>
<title-group>
<article-title>Variability of the total ozone trend over Europe for the period 1950&amp;ndash;2004 derived from reconstructed data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Krzyścin</surname>
<given-names>J. W.</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>Borkowski</surname>
<given-names>J. L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute of Geophysics, Polish Academy of Sciences, Warsaw, Poland</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>01</month>
<year>2008</year>
</pub-date>
<volume>8</volume>
<issue>1</issue>
<fpage>47</fpage>
<lpage>69</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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<abstract>
<p>Long-term variability of total ozone over Europe is discussed using results
of a flexible trend model applied to the reconstructed total ozone data for
the period 1950&amp;ndash;2004. The data base used was built within the objectives of
the COST action 726 &quot;Long-term changes and climatology of UV radiation over
Europe&quot;. The trend pattern, which comprises both anthropogenic and
&quot;natural&quot; component, is not a priori assumed but it is a result of a
smooth curve fit to the zonal monthly means and monthly grid values. The
trend values in 5-year and 10-year intervals in cold (October-next year
April) and warm (May&amp;ndash;September) seasons are calculated as the differences
between the smooth curve values at the end and beginning of selected time
intervals divided by length of the intervals. The confidence intervals for
the trend values are calculated by the block bootstrapping. The
statistically significant negative trends are found almost over whole Europe
only in the period 1985&amp;ndash;1994. Negative trends up to &amp;minus;3% per decade
appeared over small areas in earlier periods when the anthropogenic forcing
on the ozone layer was weak. The statistically positive trends are found
only during warm seasons 1995&amp;ndash;2004 over Svalbard archipelago. The reduction
of ozone level in 2004 relative to that before the satellite era is not
dramatic, i.e., up to ~&amp;minus;5% and ~&amp;minus;3.5% in the cold and
warm subperiod, respectively. Present ozone level is still depleted over
many popular resorts in southern Europe and northern Africa. For high
latitude regions the trend overturning could be inferred in last decade
(1995&amp;ndash;2004) as the ozone depleted areas are not found there in 2004 in spite
of substantial ozone depletion in the period 1985&amp;ndash;1994.</p>
</abstract>
<counts><page-count count="23"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>