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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>3</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-13177-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/13177/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/13177/2009/acpd-9-13177-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/13177/2009/acpd-9-13177-2009.pdf</fulltext_pdf>
	<start_page>13177</start_page>
	<end_page>13198</end_page>
	<publication_date>2009-06-15</publication_date>
	<article_title content_type="html">Patterns of Saharan dust transport over the Atlantic: winter vs. summer, based on CALIPSO first year data</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>Y. Ben-Ami</name>
			<email>yuval.ben-ami@weizmann.ac.il</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>I. Koren</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>O. Altaratz</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Environmental Sciences and Energy Research, Weizmann Institute of Science, Rehovot, Israel</affiliation>
	</affiliations>
	<abstract content_type="html">One of the most important factors that determines the transported dust
effect is its vertical distribution in the atmosphere. Until the launch of
the Cloud-Aerosol Lidar and Infrared Pathfinder Satellite Observation
(CALIPSO), the vertical distribution was studied mostly by in-situ
measurements and models. CALIPSO, as a part of the A-Train constellation has
opened an opportunity to study the transported dust vertical structure in a
large number of events (sufficient statistics).
&lt;br&gt;&lt;br&gt;
In this study the vertical structure of Saharan dust and stratiform clouds
is analyzed over the Atlantic Ocean for the 2006–2007 winter (December–February) and the summer of 2006 (June–August). By using CALIPSO
backscatter measurements over the dust route, we describe the differences in
dust transport between the seasons. We show a bi-modal distribution of the
average dust plumes height in both seasons (it is less clear in the winter).
It suggests that a significant part of the dust is transported near and
within the marine boundary layer and interacts with shallow clouds on both
seasons.</abstract>
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