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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>6</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-23589-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/23589/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/23589/2009/acpd-9-23589-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/23589/2009/acpd-9-23589-2009.pdf</fulltext_pdf>
	<start_page>23589</start_page>
	<end_page>23622</end_page>
	<publication_date>2009-11-05</publication_date>
	<article_title content_type="html">On the transitions in marine boundary layer cloudiness</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>I. Sandu</name>
			<email>irina.sandu@zmaw.de</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>B. Stevens</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>R. Pincus</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Max Planck Institute for Meteorology, Hamburg, Germany</affiliation>
		<affiliation numeration="2" content_type="html">University of California at Los Angeles, Los Angeles, California, USA</affiliation>
		<affiliation numeration="3" content_type="html">University of Colorado/NOAA Earth System Research Lab, Boulder, Colorado, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Satellite observations and
meteorological reanalysis are used to examine the transition from unbroken sheets of stratocumulus to
fields of scattered cumulus, and the processes controlling them, in four
subtropical ocean basins. A Lagrangian analysis suggests that both the transition,
defined as the temporal evolution in cloudiness, and the processes driving the
transition, are quite similar among the oceanic basins. The transitions
in marine boundary layer cloudiness are an extremely persistent feature
of the subtropical ocean&apos;s environment, so that the transitions&apos; characteristics
obtained by documenting the flow of thousands of individual air masses are well
reproduced by the mean (or climatological) fields of the different data sets.
This opens new opportunities for future observations and modeling studies of
these transitions.</abstract>
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</article>

