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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>3</volume_number>
		<issue_number>4</issue_number>
		<publication_year>2003</publication_year>
	</journal>
	<doi>10.5194/acpd-3-4515-2003</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/3/4515/2003/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/3/4515/2003/acpd-3-4515-2003.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/3/4515/2003/acpd-3-4515-2003.pdf</fulltext_pdf>
	<start_page>4515</start_page>
	<end_page>4548</end_page>
	<publication_date>2003-08-29</publication_date>
	<article_title content_type="html">Source-receptor matrix calculation with a Source-receptor matrix calculation with a backward mode</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>P. Seibert</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Frank</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Institute of Meteorology and Physics, University of Natural Resources (BOKU), Wien, Austria</affiliation>
	</affiliations>
	<abstract content_type="html">The possibility to calculate linear-source receptor
      relationships for the transport of atmospheric trace substances with a Lagrangian particle dispersion model (LPDM) running in backward mode is
      shown and presented with many tests and examples. The derivation includes the action of sources and of any first-order processes
      (transformation with prescribed rates, dry and wet deposition, radioactive decay, ...). The backward mode is computationally
      advantageous if the number of receptors is less than the number of sources
      considered. The combination of an LPDM with the backward (adjoint) methodology is especially attractive  for the application to point
      measurements, which can be handled without artificial numerical diffusion. Practical hints are provided for source-receptor calculations
      with different settings, both in forward and backward mode.  The equivalence of forward and backward calculations is shown in simple
      tests for release and sampling of particles,  pure wet deposition, pure convective redistribution and realistic transport over a short
      distance.  Furthermore, an application example explaining measurements of Cs-137 in Stockholm as transport from areas contaminated heavily in
      the Chernobyl disaster is included.</abstract>
	<references>
	</references>
</article>

