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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>10</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-3605-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/3605/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/3605/2010/acpd-10-3605-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/3605/2010/acpd-10-3605-2010.pdf</fulltext_pdf>
	<start_page>3605</start_page>
	<end_page>3625</end_page>
	<publication_date>2010-02-09</publication_date>
	<article_title content_type="html">On microphysical processes of noctilucent clouds (NLC): observations  and modeling of mean and width of the particle size-distribution</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>G. Baumgarten</name>
			<email>baumgarten@iap-kborn.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Fiedler</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>M. Rapp</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Leibniz-Institut für Atmosphärenphysik e.V., 18225 Kühlungsborn, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">Noctilucent clouds (NLC) in the polar summer mesopause region have
      been observed in Norway (69&amp;deg; N, 16&amp;deg; E) between 1998
      and 2009 by 3-color lidar technique. Assuming a mono-modal Gaussian
      size distribution we deduce mean and width of the particle sizes
      throughout the clouds. We observe a quasi linear relationship between
      distribution width and mean of the particle size at the top of the
      clouds and a deviation from this behavior for particle sizes larger
      than 40 nm, most often in the lower part of the layer. The
      vertically integrated particle properties show that 65% of the data
      follows the linear relationship with a slope of 0.42&amp;plusmn;0.02. For
      the vertically resolved particle properties (&amp;Delta;&lt;i&gt;z&lt;/i&gt;=0.15 km) the slope is smaller and only 0.39&amp;plusmn;0.03. We
      compare our observations to microphysical modeling of noctilucent
      clouds and find that the distribution width depends on turbulence, the
      time that turbulence can act (cloud age), and the sampling volume/time
      (atmospheric variability). The model results nicely reproduce the
      measurements and show that the observed slope can be explained by eddy
      diffusion profiles as observed from rocket measurements.</abstract>
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</article>

