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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>9</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-595-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/595/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/595/2009/acpd-9-595-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/595/2009/acpd-9-595-2009.pdf</fulltext_pdf>
	<start_page>595</start_page>
	<end_page>634</end_page>
	<publication_date>2009-01-08</publication_date>
	<article_title content_type="html">Airborne observations of a subvisible midlevel Arctic ice cloud: microphysical and radiative characterization</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Lampert</name>
			<email>astrid.lampert@awi.de</email>
		</author>
		<author numeration="2" affiliations="3">
			<name>A. Ehrlich</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>A. Dörnbrack</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>O. Jourdan</name>
		</author>
		<author numeration="5" affiliations="4">
			<name>J.-F. Gayet</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>G. Mioche</name>
		</author>
		<author numeration="7" affiliations="4,5">
			<name>V. Shcherbakov</name>
		</author>
		<author numeration="8" affiliations="1">
			<name>C. Ritter</name>
		</author>
		<author numeration="9" affiliations="3">
			<name>M. Wendisch</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Alfred Wegener Institute for Polar and Marine Research, 14473 Potsdam, Germany</affiliation>
		<affiliation numeration="2" content_type="html">Institut für Physik der Atmosphäre, DLR Oberpfaffenhofen, 82234 Oberpfaffenhofen, Germany</affiliation>
		<affiliation numeration="3" content_type="html">Johannes Gutenberg-Universität, 55099 Mainz, Germany</affiliation>
		<affiliation numeration="4" content_type="html">Laboratoire de Météorologie Physique UMR 6016 CNRS/Université Blaise Pascal, France</affiliation>
		<affiliation numeration="5" content_type="html">Laboratoire de Météorologie Physique, Institut Universitaire de Technologie de Montluçon, 03101 Montluçon Cedex, France</affiliation>
	</affiliations>
	<abstract content_type="html">During the Arctic Study of Tropospheric Aerosol, Clouds and Radiation
      (ASTAR) campaign, which was conducted in March and April 2007, an
      optically thin ice cloud was observed at around 3 km altitude
      south of Svalbard. The microphysical and radiative properties of this
      particular subvisible midlevel cloud were investigated with
      complementary remote sensing and in-situ
      instruments. Collocated airborne lidar remote-sensing and spectral
      solar radiation measurements were performed at a flight altitude of
      2300 m below the cloud base. Under almost stationary
      atmospheric conditions, the same subvisible midlevel cloud was probed
      with various in-situ sensors roughly 30 min later.
&lt;br&gt;&lt;br&gt;
      From individual ice crystal samples detected with the Cloud Particle
      Imager and the ensemble of particles measured with the Polar
      Nephelometer, we retrieved the single-scattering albedo, the
      scattering phase function as well as the volume extinction coefficient
      and the effective diameter of the crystal population. Furthermore,
      a lidar ratio of 21 (&amp;plusmn;6) sr was deduced by two independent
      methods. These parameters in conjunction with the cloud optical
      thickness obtained from the lidar measurements were used to compute
      spectral and broadband radiances and irradiances with a radiative
      transfer code. The simulated results agreed with the observed spectral
      downwelling radiance within the range given by the measurement
      uncertainty. Furthermore, the broadband radiative simulations
      estimated a net (solar plus thermal infrared) radiative forcing of the
      subvisible midlevel ice cloud of &amp;minus;0.4 W m&lt;sup&gt;&amp;minus;2&lt;/sup&gt;
      (&amp;minus;3.2 W m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; in the solar and +2.8 W m&lt;sup&gt;&amp;minus;2&lt;/sup&gt; in
      the thermal infrared wavelength range).</abstract>
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