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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>8</volume_number>
		<issue_number>5</issue_number>
		<publication_year>2008</publication_year>
	</journal>
	<doi>10.5194/acpd-8-17549-2008</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/8/17549/2008/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/8/17549/2008/acpd-8-17549-2008.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/8/17549/2008/acpd-8-17549-2008.pdf</fulltext_pdf>
	<start_page>17549</start_page>
	<end_page>17580</end_page>
	<publication_date>2008-09-26</publication_date>
	<article_title content_type="html">Physical interpretation of the spectral radiative signature in the transition zone between cloud-free and cloudy regions</article_title>
	<authors>
		<author numeration="1" affiliations="1">
			<name>J. C. Chiu</name>
			<email>christine.chiu@nasa.gov</email>
		</author>
		<author numeration="2" affiliations="2">
			<name>A. Marshak</name>
		</author>
		<author numeration="3" affiliations="3">
			<name>Y. Knyazikhin</name>
		</author>
		<author numeration="4" affiliations="4">
			<name>P. Pilewskie</name>
		</author>
		<author numeration="5" affiliations="2,5">
			<name>W. J. Wiscombe</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">University of Maryland Baltimore County, Baltimore, MD, USA</affiliation>
		<affiliation numeration="2" content_type="html">NASA/Goddard Space Flight Center, Greenbelt, MD, USA</affiliation>
		<affiliation numeration="3" content_type="html">Boston University, Boston, MA, USA</affiliation>
		<affiliation numeration="4" content_type="html">University of Colorado at Boulder, Boulder, CO, USA</affiliation>
		<affiliation numeration="5" content_type="html">Brookhaven National Laboratory, New York, NY, USA</affiliation>
	</affiliations>
	<abstract content_type="html">One-second-resolution zenith radiance measurements from the Atmospheric
Radiation Measurement program&apos;s new shortwave spectrometer (SWS) provide a unique
opportunity to analyze the transition zone between cloudy and cloud-free
air, which has considerable bearing on the aerosol indirect effect. In the
transition zone, we find a remarkable linear relationship between the sum
and difference of radiances at 870 and 1640 nm wavelengths. The intercept of
the relationship is determined primarily by aerosol properties, and the
slope by cloud properties. We then show that this linearity can be predicted
from simple theoretical considerations and furthermore that it supports the
hypothesis of inhomogeneous mixing, whereby optical depth increases as a
cloud is approached but the effective drop size remains unchanged. In
addition, the width of transition zones from SWS data is in the range of
50–150 m, which differs from the width in satellite observations (a few
kilometers) and in airborne lidar data (1–2 km).</abstract>
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