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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACP</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACP</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-13-2455-2013</article-id>
<title-group>
<article-title>Identification of key aerosol populations through their size and composition resolved spectral scattering and absorption</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Costabile</surname>
<given-names>F.</given-names>
<ext-link>https://orcid.org/0000-0002-9590-3776</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Barnaba</surname>
<given-names>F.</given-names>
<ext-link>https://orcid.org/0000-0002-1927-6926</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Angelini</surname>
<given-names>F.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Gobbi</surname>
<given-names>G. P.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Institute for Atmospheric Sciences and Climate, National Research Council (ISAC-CNR), Rome, Italy</addr-line>
</aff>
<pub-date pub-type="epub">
<day>05</day>
<month>03</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>5</issue>
<fpage>2455</fpage>
<lpage>2470</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 F. Costabile et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://acp.copernicus.org/articles/13/2455/2013/acp-13-2455-2013.html">This article is available from https://acp.copernicus.org/articles/13/2455/2013/acp-13-2455-2013.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/articles/13/2455/2013/acp-13-2455-2013.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/articles/13/2455/2013/acp-13-2455-2013.pdf</self-uri>
<abstract>
<p>Characterizing chemical and physical aerosol properties is important
  to understand their sources, effects, and feedback mechanisms in the
  atmosphere. This study proposes a scheme to classify aerosol
  populations based on their spectral optical properties (absorption
  and scattering). The scheme is obtained thanks to the outstanding
 set of information on particle size and composition these properties
  contain.  The spectral variability of the aerosol single scattering
  albedo (dSSA), and the extinction, scattering and absorption Angstrom exponents
  (EAE, SAE and AAE, respectively) were observed on the basis of two-year
  measurements of aerosol optical properties (scattering and
  absorption coefficients at blue, green and red wavelengths)
  performed in the suburbs of Rome (Italy). Optical measurements of
  various aerosol types were coupled to measurements of particle
  number size distributions and relevant optical properties
  simulations (Mie theory). These latter allowed the investigation of the
  role of the particle size and composition in the bulk aerosol
  properties observed. The combination of simulations and measurements
  suggested a general &quot;paradigm&quot; built on dSSA, SAE and AAE to
  optically classify aerosols. The paradigm proved suitable to
  identify the presence of key aerosol populations, including soot,
  biomass burning, organics, dust and marine particles.  The work  
highlights that (i) aerosol populations show distinctive
  combinations of SAE and dSSA times AAE, these variables being linked
  by a linear inverse relation varying with varying SSA; (ii) fine
  particles show EAE &gt; 1.5, whilst EAE &lt; 2 is found for both coarse
  particles and ultrafine soot-rich aerosols; (iii) fine and coarse
  particles both show SSA &gt; 0.8, whilst ultrafine urban Aitken mode and soot
particles show SSA &lt; 0.8. The proposed paradigm agrees with aerosol
observations performed during past major field campaigns, this indicating
that relations concerning the paradigm have a general validity.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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