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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics</journal_title>
		<journal_url>www.atmos-chem-phys.net</journal_url>
		<issn>1680-7316</issn>
		<eissn>1680-7324</eissn>
		<volume_number>10</volume_number>
		<issue_number>10</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acp-10-4757-2010</doi>
	<article_url>http://www.atmos-chem-phys.net/10/4757/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys.net/10/4757/2010/acp-10-4757-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys.net/10/4757/2010/acp-10-4757-2010.pdf</fulltext_pdf>
	<start_page>4757</start_page>
	<end_page>4774</end_page>
	<publication_date>2010-05-26</publication_date>
	<article_title content_type="html">The PreVOCA experiment: modeling the lower troposphere in the Southeast Pacific</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>M. C. Wyant</name>
			<email>mwyant@atmos.washington.edu</email>
		</author>
		<author numeration="2" affiliations="1">
			<name>R. Wood</name>
		</author>
		<author numeration="3" affiliations="1">
			<name>C. S. Bretherton</name>
		</author>
		<author numeration="4" affiliations="2">
			<name>C. R. Mechoso</name>
		</author>
		<author numeration="5" affiliations="3">
			<name>J. Bacmeister</name>
		</author>
		<author numeration="6" affiliations="4">
			<name>M. A. Balmaseda</name>
		</author>
		<author numeration="7" affiliations="5">
			<name>B. Barrett</name>
		</author>
		<author numeration="8" affiliations="6">
			<name>F. Codron</name>
		</author>
		<author numeration="9" affiliations="7">
			<name>P. Earnshaw</name>
		</author>
		<author numeration="10" affiliations="8">
			<name>J. Fast</name>
		</author>
		<author numeration="11" affiliations="9">
			<name>C. Hannay</name>
		</author>
		<author numeration="12" affiliations="4">
			<name>J. W. Kaiser</name>
		</author>
		<author numeration="13" affiliations="10">
			<name>H. Kitagawa</name>
		</author>
		<author numeration="14" affiliations="11">
			<name>S. A. Klein</name>
		</author>
		<author numeration="15" affiliations="4">
			<name>M. Köhler</name>
		</author>
		<author numeration="16" affiliations="12">
			<name>J. Manganello</name>
		</author>
		<author numeration="17" affiliations="13">
			<name>H.-L. Pan</name>
		</author>
		<author numeration="18" affiliations="2">
			<name>F. Sun</name>
		</author>
		<author numeration="19" affiliations="14">
			<name>S. Wang</name>
		</author>
		<author numeration="20" affiliations="15">
			<name>Y. Wang</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">Department of Atmospheric Sciences, University of Washington, Seattle, WA, USA</affiliation>
		<affiliation numeration="2" content_type="html">Department of Atmospheric and Oceanic Sciences, University of California, Los Angeles, Los Angeles, CA, USA</affiliation>
		<affiliation numeration="3" content_type="html">Global Modeling and Assimiliation Office, NASA Goddard Space Flight Center, Greenbelt, MD, USA</affiliation>
		<affiliation numeration="4" content_type="html">Research Department, European Center for Medium-Range Weather Forecasts, Reading, UK</affiliation>
		<affiliation numeration="5" content_type="html">Department of Geophysics, University of Chile, Santiago, Chile</affiliation>
		<affiliation numeration="6" content_type="html">Université Pierre et Marie Curie, Laboratoire de Meteorologie Dynamique, Paris, France</affiliation>
		<affiliation numeration="7" content_type="html">Met Office, Exeter, Devon, UK</affiliation>
		<affiliation numeration="8" content_type="html">Atmospheric Sciences and Global Change, Pacific Northwest National Laboratory, Richland, WA, USA</affiliation>
		<affiliation numeration="9" content_type="html">Climate and Global Dynamics Division, National Center for Atmospheric Research, Boulder, CO, USA</affiliation>
		<affiliation numeration="10" content_type="html">Meteorological College, Japan Meteorological Agency, Tokyo, Japan</affiliation>
		<affiliation numeration="11" content_type="html">Program for Climate Model Diagnosis and Intercomparison, Lawrence Livermore National Laboratory,  Livermore, CA, USA</affiliation>
		<affiliation numeration="12" content_type="html">Center for Ocean-Land-Atmosphere Studies, Calverton, MD, USA</affiliation>
		<affiliation numeration="13" content_type="html">Environmental Modeling Center, National Centers for Environmental Prediction, Camp Springs, Maryland, USA</affiliation>
		<affiliation numeration="14" content_type="html">Marine Meteorology Division, Naval Research Laboratory, Monterey, CA, USA</affiliation>
		<affiliation numeration="15" content_type="html">International Pacific Research Center, School of Ocean and Earth Science and Technology, University of Hawaii at Manoa, Honolulu, HI, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The Preliminary VOCALS Model Assessment (PreVOCA) aims to
      assess contemporary atmospheric modeling of the subtropical
      South East Pacific, with a particular focus on the clouds and
      the marine boundary layer (MBL).  Models results from fourteen
      modeling centers were collected including operational forecast
      models, regional models, and global climate models for the
      month of October 2006. Forecast models and global climate
      models produced daily forecasts, while most regional models
      were run continuously during the study period, initialized and
      forced at the boundaries with global model analyses. Results
      are compared in the region from 40&amp;deg; S to the equator
      and from 110&amp;deg; W to 70&amp;deg; W, corresponding to the
      Pacific coast of South America. Mean-monthly model surface
      winds agree well with QuikSCAT observed winds and models agree
      fairly well on mean weak large-scale subsidence in the region
      next to the coast. However they have greatly differing geographic
      patterns of mean cloud fraction with only a few models
      agreeing well with MODIS observations. Most models also
      underestimate the MBL depth by several hundred meters in the
      eastern part of the study region. The diurnal cycle of liquid
      water path is underestimated by most models at the
      85&amp;deg; W 20&amp;deg; S stratus buoy site compared with
      satellite, consistent with previous modeling studies. The low
      cloud fraction is also underestimated during all parts of the
      diurnal cycle compared to surface-based climatologies.  Most
      models qualitatively capture the MBL deepening around 15 October 2006 at the stratus buoy, associated with colder air at
      700 hPa.</abstract>
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