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<article language="en">
	<journal>
		<journal_title>Atmospheric Measurement Techniques</journal_title>
		<journal_url>www.atmos-meas-tech.net</journal_url>
		<issn>1867-1381</issn>
		<eissn>1867-8548</eissn>
		<volume_number>2</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/amt-2-423-2009</doi>
	<article_url>http://www.atmos-meas-tech.net/2/423/2009/</article_url>
	<abstract_html>http://www.atmos-meas-tech.net/2/423/2009/amt-2-423-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-meas-tech.net/2/423/2009/amt-2-423-2009.pdf</fulltext_pdf>
	<start_page>423</start_page>
	<end_page>435</end_page>
	<publication_date>2009-08-05</publication_date>
	<article_title content_type="html">Stratospheric isotopic water profiles from a single submillimeter limb scan by TELIS</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. de Lange</name>
			<email>a.de.lange@sron.nl</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>J. Landgraf</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>R. Hoogeveen</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">SRON Netherlands Institute for Space Research, Sorbonnelaan 2, Utrecht, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">Around 490 GHz relatively strong HDO and H&lt;sub&gt;2&lt;/sub&gt;&lt;sup&gt;18&lt;/sup&gt;O emission lines
can be found in the submillimeter thermal-emission spectrum of the Earth&apos;s
atmosphere, along with lines of the principal isotopologue of water vapour.
These can be used for remote sensing of the rare/principal isotope ratio in
the stratosphere. A sensitivity study has been performed for retrieval
simulations of water isotopologues from balloon-borne measurements by the
limb sounder TELIS (TErahertz and submillimeter LImb Sounder). The study
demonstrates the capability of TELIS to determine, from a single limb scan,
the profiles for H&lt;sub&gt;2&lt;/sub&gt;&lt;sup&gt;18&lt;/sup&gt;O and HDO between 20 km and 37 km with a
retrieval error of &amp;asymp;3 and a spatial resolution of 1.5 km, as
determined by the width of the averaging kernel. In addition HDO can be
retrieved in the range of 10–20 km, albeit with a strongly deteriorated
retrieval error. Expected uncertainties in instrumental parameters have only
limited impact on the retrieval results.</abstract>
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</article>

