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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>10</volume_number>
		<issue_number>2</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-3301-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/3301/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/3301/2010/acpd-10-3301-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/3301/2010/acpd-10-3301-2010.pdf</fulltext_pdf>
	<start_page>3301</start_page>
	<end_page>3318</end_page>
	<publication_date>2010-02-08</publication_date>
	<article_title content_type="html">A comparison of ship and satellite measurements of cloud properties in the southeast Pacific stratus deck</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. A. Brunke</name>
			<email>brunke@atmo.arizona.edu</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>S. P. de Szoeke</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>P. Zuidema</name>
		</author>
		<author numeration="4" affiliations="1">
			<name>X. Zeng</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">The University of Arizona, Department of Atmospheric Sciences,  Tucson, Arizona, USA</affiliation>
		<affiliation numeration="2" content_type="html">Oregon State University, College of Oceanic and Atmospheric Sciences,  Corvallis, Oregon, USA</affiliation>
		<affiliation numeration="3" content_type="html">University of Miami, Rosentiel School of Marine and Atmospheric  Science, Miami, Florida, USA</affiliation>
	</affiliations>
	<abstract content_type="html">Here, liquid water path (LWP), cloud fraction, cloud top height, and
      cloud base height are retrieved by a suite of satellite instruments
      (the CPR aboard CloudSat, CALIOP aboard CALIPSO, and MODIS aboard
      Aqua) and compared to ship observations from research cruises made in
      2001 and 2003–2007 into the stratus/stratocumulus deck over the
      southeast Pacific Ocean. It is found that CloudSat LWP is generally
      too high over this region and the CloudSat/CALIPSO cloud bases are too
      low which is to be expected from the increased sensitivity to
      precipitation by both the radar and lidar. This results in
      a relationship (LWP~&lt;i&gt;h&lt;/i&gt;&lt;sup&gt;9&lt;/sup&gt;) between CloudSat LWP and CALIPSO
      cloud thickness (&lt;i&gt;h&lt;/i&gt;) that is very different from the adiabatic
      relationship (LWP~&lt;i&gt;h&lt;/i&gt;&lt;sup&gt;2&lt;/sup&gt;) from in situ
      observations. Furthermore, comparing results from a global model
      (CAM3.1) to ship observations reveals that, while the simulated LWP is
      quite reasonable, the model cloud is too thick and too low, allowing
      the model to have LWPs that are almost independent of &lt;i&gt;h&lt;/i&gt;. Such
      differences may be reduced in future versions of both the satellite
      data and the model.</abstract>
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</article>

