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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>1</issue_number>
		<publication_year>2010</publication_year>
	</journal>
	<doi>10.5194/acpd-10-785-2010</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/10/785/2010/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/10/785/2010/acpd-10-785-2010.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/10/785/2010/acpd-10-785-2010.pdf</fulltext_pdf>
	<start_page>785</start_page>
	<end_page>819</end_page>
	<publication_date>2010-01-15</publication_date>
	<article_title content_type="html">Impact of brown and clear carbon on light absorption enhancement, single  scatter albedo and absorption wavelength dependence of black carbon</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>D. A. Lack</name>
			<email>daniel.lack@noaa.gov</email>
		</author>
		<author numeration="2" affiliations="3">
			<name>C. D. Cappa</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">NOAA Earth System Research Laboratory, Chemical Sciences Division,  325 Broadway, Boulder, 80304, CO, USA</affiliation>
		<affiliation numeration="2" content_type="html">Cooperative Institute for Research in Environmental Sciences,  University of Colorado, 216 UCB, Boulder, 80309, CO, USA</affiliation>
		<affiliation numeration="3" content_type="html">Department of Civil and Environmental Engineering, University of  California, Davis, California, USA</affiliation>
	</affiliations>
	<abstract content_type="html">The presence of clear coatings on atmospheric black carbon (BC) particles is
known to enhance the magnitude of light absorption by the BC cores. Based on
calculations using core/shell Mie theory, we demonstrate the enhancement of
light absorption (&lt;i&gt;E&lt;/i&gt;&lt;sub&gt;Abs&lt;/sub&gt;) by atmospheric black carbon (BC) when
coated in mildly absorbing material (C&lt;sub&gt;Brown&lt;/sub&gt;) is reduced, relative
to the enhancement by non-absorbing coatings (C&lt;sub&gt;Clear&lt;/sub&gt;). This
reduction, sensitive to C&lt;sub&gt;Brown&lt;/sub&gt; shell thickness and imaginary
refractive index (RI), can be up to 50% for 400 nm radiation and 25%
averaged across the visible radiation spectrum for reasonable core/shell
diameters. The enhanced direct radiative forcing possible due to the
enhancement effect of C&lt;sub&gt;Clear&lt;/sub&gt; is therefore reduced if the coating is
absorbing. Additionally, the need to explicitly treat
      BC as an internal, as opposed to external, mixture with C&lt;sub&gt;Brown&lt;/sub&gt; is shown to be
      important to the calculated single scatter albedo only whensub models treat BC as large
      spherical cores (&gt;50 nm). For smaller BC cores (or fractal agglomerates) consideration
      of the BC and C&lt;sub&gt;Brown&lt;/sub&gt; as an external mixture leads to relatively small errors in
      the particle single scatter albedo of &lt;0.03. It is often assumed that observation of an
      absorption Angstrom exponent (AAE) &gt;1 indicates non-BC absorption. Here, it is shown that
      BC cores coated in C&lt;sub&gt;Clear&lt;/sub&gt;can reasonably have an AAE of up to 1.6, a result that
      complicates the attribution of observed light absorption to C&lt;sub&gt;Brown&lt;/sub&gt; within ambient
      particles. However, an  AAE&lt;1.6 does not exclude the possibility of
C&lt;sub&gt;Brown&lt;/sub&gt;, rather C&lt;sub&gt;Brown&lt;/sub&gt; cannot be confidently assigned
unless AAE&gt;1.6. Comparison of these results to some ambient AAE
data shows that large-scale attribution of C&lt;sub&gt;Brown&lt;/sub&gt; is a challenging
task using current in-situ measurement methods. We suggest that coincident
measurements of particle core and shell sizes along with the AAE may be
necessary to distinguish absorbing and non-absorbing OC.</abstract>
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</article>

