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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques Discussions</journal_title>
		<journal_url>www.atmos-meas-tech-discuss.net</journal_url>
		<eissn>1867-8610</eissn>
		<volume_number>3</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/amtd-3-1933-2010</doi>
	<article_url>http://www.atmos-meas-tech-discuss.net/3/1933/2010/</article_url>
	<abstract_html>http://www.atmos-meas-tech-discuss.net/3/1933/2010/amtd-3-1933-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech-discuss.net/3/1933/2010/amtd-3-1933-2010.pdf</fulltext_pdf>
	<start_page>1933</start_page>
	<end_page>1970</end_page>
	<publication_date>2010-04-22</publication_date>
	<article_title content_type="html">The ground-based MW radiometer OZORAM on Spitsbergen &amp;ndash; description and validation of stratospheric and mesospheric O&lt;sub&gt;3&lt;/sub&gt;-measurements</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Palm</name>
			<email>mathias@iup.physik.uni-bremen.de</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>C. G. Hoffmann</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>S. H. W. Golchert</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>J. Notholt</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">IUP, Universität Bremen, Bremen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">This manuscript introduces the OZORAM ground based millimeter wave
  radiometer.  The instrument is deployed to the high Arctic
  (79&amp;deg; N, 12&amp;deg; E) for measurements of O&lt;sub&gt;3&lt;/sub&gt; in the
  upper stratosphere and lower mesosphere.

&lt;br&gt;&lt;br&gt;

  The discussion covers measurements taken since late 2006. To
  investigate instrumental biases, the results from September 2008
  till spring 2009 are compared to O&lt;sub&gt;3&lt;/sub&gt; profiles derived from
  measurements of two instruments onboard polar orbiting satellites,
  MLS onboard EOS-AURA and SABER onboard TIMED.  The agreement is
  within 20% in the stratosphere and 40% in the mesosphere. The
  deviations show strong systematic and oscillating features, for
  which the error discussion of the ground based
  instrument/measurement gives possible explanations.

&lt;br&gt;&lt;br&gt;

  Nonetheless, expected features like the diurnal cycle and O&lt;sub&gt;3&lt;/sub&gt;
  enhancements due to stratospheric warmings are readily observed,
  which could not originally be taken for granted given the large
  deviation from the satellite data.

&lt;br&gt;&lt;br&gt;

  The nature of the oscillatory deviation is further studied. This
  study points to a systematic error in the radiative
  transfer modeling caused by imperfect spectroscopic data.</abstract>
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</article>

