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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ACPD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Chemistry and Physics Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">ACPD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Chem. Phys. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name></publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-11-20667-2011</article-id>
<title-group>
<article-title>Impact of continental outflow on chemistry of atmospheric aerosols over tropical Bay of Bengal</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Srinivas</surname>
<given-names>B.</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>Kumar</surname>
<given-names>A.</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>Sarin</surname>
<given-names>M. M.</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>Sudheer</surname>
<given-names>A. K.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Physical Research Laboratory, Navarangapura, Ahmedabad 380 009, India</addr-line>
</aff>
<pub-date pub-type="epub">
<day>20</day>
<month>07</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>7</issue>
<fpage>20667</fpage>
<lpage>20711</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 B. Srinivas et al.</copyright-statement>
<copyright-year>2011</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/preprints/11/20667/2011/acpd-11-20667-2011.html">This article is available from https://acp.copernicus.org/preprints/11/20667/2011/acpd-11-20667-2011.html</self-uri>
<self-uri xlink:href="https://acp.copernicus.org/preprints/11/20667/2011/acpd-11-20667-2011.pdf">The full text article is available as a PDF file from https://acp.copernicus.org/preprints/11/20667/2011/acpd-11-20667-2011.pdf</self-uri>
<abstract>
<p>The continental outflow from Indo-Gangetic Plain and south-east Asia
dominates the widespread dispersal of pollutants over tropical Bay of Bengal
(BoB) during the late NE-monsoon (January–March). It is thus pertinent to assess
the impact on marine atmospheric boundary layer of BoB. The chemical data,
based on analyses of size-segregated (PM&lt;sub&gt;2.5&lt;/sub&gt; and PM&lt;sub&gt;10&lt;/sub&gt;) aerosols,
suggest the dominance of nss-SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt; (range: 1.3 to 28 μg m&lt;sup&gt;−3&lt;/sup&gt;)
in PM&lt;sub&gt;2.5&lt;/sub&gt;. Almost all SO&lt;sub&gt;4&lt;/sub&gt;&lt;sup&gt;2&amp;minus;&lt;/sup&gt; is of anthropogenic
origin and accounts for as much as 65 % of the water-soluble inorganic
constituents. The impact of anthropogenic sources is further evident from
the widespread depletion of chloride (range: 40 to 100 %) compared to
sea-salt composition. The carbonaceous species (EC and OC) contribute nearly
25 % to PM&lt;sub&gt;2.5&lt;/sub&gt;;  and significant linear relationship with K&lt;sup&gt;+&lt;/sup&gt;
suggests biomass burning as their dominant source (biofuels and agricultural
waste). The enhancement in the fractional solubility of aerosol Fe, as
assessed in PM&lt;sub&gt;2.5&lt;/sub&gt;, re-emphasizes the impact of combustion sources
(biomass and fossil-fuel) and chemical processing (of dust) during the
long-range transport. The high enrichment factors of heavy metals (Pb and
Cd) further demonstrate the influence of pollution sources on the chemistry
of MABL. The downwind transport of pollutants and exchange across air-sea
interface can, thus, have profound impact on the ocean surface
biogeochemistry.</p>
</abstract>
<counts><page-count count="45"/></counts>
</article-meta>
</front>
<body/>
<back>
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