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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>8</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-893-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/893/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/893/2008/acpd-8-893-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/893/2008/acpd-8-893-2008.pdf</fulltext_pdf>
	<start_page>893</start_page>
	<end_page>906</end_page>
	<publication_date>2008-01-18</publication_date>
	<article_title content_type="html">UV variability in Moscow according to long-term UV measurements and reconstruction model</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>N. Y. Chubarova</name>
			<email>chubarova@imp.kiae.ru</email>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Faculty of Geography, Moscow State University, Moscow, Russia</affiliation>
	</affiliations>
	<abstract content_type="html">Long-term measurements of erythemally weighted UV irradiance (&lt;i&gt;Q&lt;/i&gt;&lt;sub&gt;er&lt;/sub&gt;) have
been analyzed for the 1999&amp;ndash;2006 period as well as UV variability according
to reconstruction model since 1968. The estimates of different atmospheric
parameters effects, including NO&lt;sub&gt;2&lt;/sub&gt; content, on &lt;i&gt;Q&lt;/i&gt;&lt;sub&gt;er&lt;/sub&gt;)  have been
obtained on seasonal and interannual scales. It has been shown that NO&lt;sub&gt;2&lt;/sub&gt;
content in conditions of large megalopolis provides average &lt;i&gt;Q&lt;/i&gt;&lt;sub&gt;er&lt;/sub&gt; 
decrease of about 1.5&amp;ndash;2%. The seasonal variations of the observed UV
indices are discussed from the point of view of the impact on health. Using
the reconstruction model we showed a distinct growth in &lt;i&gt;Q&lt;/i&gt;&lt;sub&gt;er&lt;/sub&gt;  since 1980
due to decrease in total ozone (+2.5% per decade), effective cloud amount
transmission (+2.1% per decade) and aerosol loading (+1.1% per
decade). However, there is no changes in &lt;i&gt;Q&lt;/i&gt;&lt;sub&gt;er&lt;/sub&gt; over larger 1968&amp;ndash;2006
period due to significant decrease in effective cloud amount transmission
(&amp;minus;11% per decade) in 1968&amp;ndash;1980.</abstract>
	<references>
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</article>

