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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>5</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2005</publication_year>
	</journal>
	<doi>10.5194/acpd-5-1585-2005</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/5/1585/2005/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/5/1585/2005/acpd-5-1585-2005.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/5/1585/2005/acpd-5-1585-2005.pdf</fulltext_pdf>
	<start_page>1585</start_page>
	<end_page>1617</end_page>
	<publication_date>2005-03-15</publication_date>
	<article_title content_type="html">Retrieval of temperature and water vapor profiles from radio occultation refractivity and bending angle measurements using an optimal estimation approach: a simulation study</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>A. von Engeln</name>
		</author>
		<author numeration="2" affiliations="2">
			<name>G. Nedoluha</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Naval Research Laboratory, Remote Sensing Division, Washington, D.C., USA</affiliation>
		<affiliation numeration="2" content_type="html">Institute of Environmental Physics, University of Bremen, Bremen, Germany</affiliation>
	</affiliations>
	<abstract content_type="html">The Optimal Estimation Method is used to retrieve temperature and water vapor profiles
from simulated radio occultation measurements in order to assess possible assimilation
impacts of this data. High resolution ECMWF global fields are used by
5 a state-of-the-art radio occultation simulator to provide quasi-realistic bending angle
and refractivity profiles. Both types of profiles are used in the retrieval process to assess
their advantages and disadvantages. The impact of the GPS measurement is
expressed as an improvement over the a priori knowledge (taken from a 24 h old analysis).
Large improvements are found for temperature in the upper troposphere and
10 lower stratosphere. Only very small improvements are found in the lower troposphere,
where water vapor is present. Water vapor improvements are only significant between
about 1 km to 7 km. No pronounced difference is found between retrievals based upon
bending angles or refractivity. Results are compared to idealized retrievals, where the
atmosphere is spherically symmetric and instrument noise is not included. Comparing
15 idealized to quasi-realistic calculations shows that the main impact of a ray tracing algorithm
can be expected for low latitude water vapor, where the horizontal variability is
high. We also address the effect of altitude correlations in the temperature and water
vapor. Overall, we find that water vapor and temperature retrievals using bending angle
profiles are significantly more CPU intensive than refractivity profiles, but that they do
20 not provide significantly better results.</abstract>
	<references>
	</references>
</article>

