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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>2</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2002</publication_year>
	</journal>
	<doi>10.5194/acpd-2-1765-2002</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/2/1765/2002/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/2/1765/2002/acpd-2-1765-2002.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/2/1765/2002/acpd-2-1765-2002.pdf</fulltext_pdf>
	<start_page>1765</start_page>
	<end_page>1790</end_page>
	<publication_date>2002-10-28</publication_date>
	<article_title content_type="html">On the use of mass-conserving wind fields in chemistry-transport models</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>B. Bregman</name>
		</author>
		<author numeration="2" affiliations="1">
			<name>A. Segers</name>
		</author>
		<author numeration="3" affiliations="2">
			<name>M. Krol</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>E. Meijer</name>
		</author>
		<author numeration="5" affiliations="1">
			<name>P. van Velthoven</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Royal Netherlands Meteorological Institute, P.O. Box 201, 3730 AE, De Bilt, Netherlands</affiliation>
		<affiliation numeration="2" content_type="html">Institute for Marine and Atmospheric Research Utrecht, Princetonplein 5, 3584 CC, Netherlands</affiliation>
	</affiliations>
	<abstract content_type="html">A new method has been developed that provides mass-conserving wind fields for
      global chemistry-transport models. In previous global Eulerian modeling studies a mass-imbalance was found between the model mass transport and the
      surface pressure tendencies. Several methods have been suggested to correct
      for this imbalance, but so far no satisfactory solution has been found. Our
      new method solves these problems by using the wind fields in a spherical harmonical form (divergence and vorticity) by mimicing the physics of the
      weather forecast model as closely as possible. A 3-D chemistry-transport model
      was used to show that the calculated ozone fields with the new processing method agree remarkably better with ozone observations in the upper
      troposphere and lower stratosphere. In addition, the calculated age of air in
      the lower stratosphere show better agreement with observations, although the
      air remains still too young in the extra tropical stratosphere.</abstract>
	<references>
	</references>
</article>

