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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>9</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-15747-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/15747/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/15747/2009/acpd-9-15747-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/15747/2009/acpd-9-15747-2009.pdf</fulltext_pdf>
	<start_page>15747</start_page>
	<end_page>15767</end_page>
	<publication_date>2009-07-24</publication_date>
	<article_title content_type="html">Estimating trajectory uncertainties due to flow dependent errors in the atmospheric analysis</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>A. Engström</name>
			<email>anderse@misu.su.se</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>L. Magnusson</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Meteorology, Stockholm University, Stockholm, Sweden</affiliation>
	</affiliations>
	<abstract content_type="html">The uncertainty of a calculated trajectory is dependent on the uncertainty in
the atmospheric analysis. Using the Ensemble Transform method (originally
adapted for ensemble forecasting) we sample the analysis uncertainty in order
to create an ensemble of analyses where a trajectory is started from each
perturbed analysis. This method, called the Ensemble analysis method (EA), is
compared to the Initial spread method (IS), where the trajectory receptor
point is perturbed in the horizontal and vertical direction to create a set
of trajectories used to estimate trajectory uncertainty. The deviation growth
is examined for a one-month period and for 15 different locations. We find up
to a 40% increase in trajectory deviation in the mid-latitudes using the EA
method. A simple model for trajectory deviation growth speed is set up and
validated. It is shown that the EA method result in a faster error growth
compared to the IS method. In addition, two case studies are examined to
qualitatively illustrate how the flow dependent analysis uncertainty can
impact the trajectory calculations. We find a more irregular behavior for the
EA trajectories compared to the IS trajectories and a significantly increased
uncertainty in the trajectory origin. By perturbing the analysis in
consistency with the analysis uncertainties the error in backward trajectory
calculations can be more consistently estimated.</abstract>
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</article>

