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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>9</volume_number>
		<issue_number>21</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acp-9-8199-2009</doi>
	<article_url>http://www.atmos-chem-phys.net/9/8199/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/9/8199/2009/acp-9-8199-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/9/8199/2009/acp-9-8199-2009.pdf</fulltext_pdf>
	<start_page>8199</start_page>
	<end_page>8210</end_page>
	<publication_date>2009-11-02</publication_date>
	<article_title content_type="html">Retrieval of water vapor profile in the mesosphere from satellite ozone and hydroxyl measurements by the basic dynamic model of mesospheric photochemical system</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. Y. Kulikov</name>
			<email>kulm@appl.sci-nnov.ru</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. M. Feigin</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>G. R. Sonnemann</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Applied Physics of the Russian Academy of Science, Ulyanov Str. 46, 603950, Nizhny Novgorod, Russia</affiliation>
		<affiliation numeration="2" content_type="html">Leibniz-Institute of Atmospheric Physics at the University Rostock in Kühlungsborn, Schloss-Str. 6, 18225 Ostseebad Kühlungsborn, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">We propose an indirect method for retrieving a number of significant minor
gas constituents of the atmosphere. The technique is based on the use of
so-called basic dynamic models of atmospheric photochemical systems
simplified mathematically correctly in a special manner. It is applied to a
mesospheric system describing day evolution of key minor gas constituents at
these heights. We take as initial data experimental data of the
CRISTA-MAHRSI satellite campaign of August 1997 during which ozone and
hydroxyl (O&lt;sub&gt;3&lt;/sub&gt; and OH) concentrations were measured simultaneously. It is
demonstrated that the use of the basic dynamic model allows retrieval of
vertical distribution (within the 53–85 km range of heights) of water vapor
concentration that is one of the control parameters of the mesospheric
photochemistry.</abstract>
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</article>

