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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>10</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-11401-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/11401/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/11401/2010/acpd-10-11401-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/11401/2010/acpd-10-11401-2010.pdf</fulltext_pdf>
	<start_page>11401</start_page>
	<end_page>11448</end_page>
	<publication_date>2010-04-28</publication_date>
	<article_title content_type="html">Multi sensor reanalysis of total ozone</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>R. J. van der A</name>
			<email>avander@knmi.nl</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>M. A. F. Allaart</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>H. J. Eskes</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">KNMI, P.O. Box 201, 3730 AE De Bilt, The Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">A single coherent total ozone dataset, called the Multi Sensor Reanalysis
(MSR), has been created from all available ozone column data measured by
polar orbiting satellites in the near-ultraviolet Huggins band in the last
thirty years. Fourteen total ozone satellite retrieval datasets from the
instruments TOMS (on the satellites Nimbus-7 and Earth Probe), SBUV
(Nimbus-7, NOAA-9, NOAA-11 and NOAA-16), GOME (ERS-2), SCIAMACHY (Envisat),
OMI (EOS-Aura), and GOME-2 (Metop-A) have been used in the MSR. As first
step a bias correction scheme is applied to all satellite observations,
based on independent ground-based total ozone data from the World Ozone and
Ultraviolet Data Center. The correction is a function of solar zenith angle,
viewing angle, time (trend), and stratospheric temperature. As second step
data assimilation was applied to create a global dataset of total ozone
analyses. The data assimilation method is a sub-optimal implementation of
the Kalman filter technique, and is based on a chemical transport model
driven by ECMWF meteorological fields. The chemical transport model provides
a detailed description of (stratospheric) transport and uses
parameterisations for gas-phase and ozone hole chemistry. The MSR dataset
results from a 30-year data assimilation run with the 14 corrected satellite
datasets as input, and is available on a grid of
1&amp;times;1Â½ degrees with a sample
frequency of 6 h for the complete time period (1978â€“2008). The
Observation-minus-Analysis (OmA) statistics show that the bias of the MSR
analyses is less than 1 percent with an RMS standard deviation of about 2
percent as compared to the corrected satellite observations used.</abstract>
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</article>

