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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>
</journal-title-group>
<issn pub-type="epub">1680-7324</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>GÃ¶ttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acp-11-8271-2011</article-id>
<title-group>
<article-title>Effect of the summer monsoon on aerosols at two measurement stations in Northern India â€“ Part 1: PM and BC concentrations</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>HyvÃ¤rinen</surname>
<given-names>A.-P.</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>Raatikainen</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Brus</surname>
<given-names>D.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Komppula</surname>
<given-names>M.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Panwar</surname>
<given-names>T. S.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Hooda</surname>
<given-names>R. K.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Sharma</surname>
<given-names>V. P.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Lihavainen</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Finnish Meteorological Institute, Erik PalmÃ©nin aukio 1, P.O. Box 503, 00101, Helsinki, Finland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratory of Aerosol Chemistry and Physics, Institute of Chemical Process Fundamentals Academy of Sciences of the Czech Republic, RozvojovÃ¡ 135, 165 02 Prague 6, Czech Republic</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Finnish Meteorological Institute, Yliopistonranta 1F, P.O. Box 1627, 70211 Kuopio, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>The Energy and Resources Institute (TERI), Darbari Seth Block, IHC Complex, Lodhi Road, New Delhi 110 003, India</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>currently at: School of Earth &amp; Atmospheric Sciences, Georgia Institute of Technology, 311 Ferst Drive, Atlanta, GA 30332-0340, USA</addr-line>
</aff>
<pub-date pub-type="epub">
<day>15</day>
<month>08</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>16</issue>
<fpage>8271</fpage>
<lpage>8282</lpage>
<permissions>
<license xlink:type="simple">
<license-p>This is an open-access article ditributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.</license-p>
</license>
</permissions>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/8271/2011/acp-11-8271-2011.html">This article is available from http://www.atmos-chem-phys.net/11/8271/2011/acp-11-8271-2011.html</self-uri>
<self-uri xlink:href="http://www.atmos-chem-phys.net/11/8271/2011/acp-11-8271-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys.net/11/8271/2011/acp-11-8271-2011.pdf</self-uri>
<abstract>
<p>Particulate matter (PM) and equivalent black carbon (BCe) concentrations were
measured at two locations in northern India during 2006â€“2010. The first
measurement station was a background site in Mukteshwar, about 350 km
northeast of New Delhi, in the foothills of the Indian Himalayas. The second
measurement site was located in Gual Pahari, about 25 km south of New Delhi.
Here we focused on resolving the effects of the Indian summer monsoon on the
particulate matter and equivalent black carbon concentrations at two
stations. The average monsoon time concentrations were decreased by
55â€“70 % compared to the pre-monsoon average concentrations at both
stations, decreasing as a function of the total local rainfall during the
monsoon season. In Mukteshwar during the monsoon, the 24 h PM&lt;sub&gt;2.5&lt;/sub&gt;
concentrations were nearly always below the Indian National Air Quality
Standard of 60 Î¼g m&lt;sup&gt;âˆ’3&lt;/sup&gt;. In Gual Pahari, 13 % of days
exceeded this level during the monsoon season. However, the 24 h guideline
of 25 Î¼g m&lt;sup&gt;âˆ’3&lt;/sup&gt; given by the World Health Organization was more
difficult to meet. In addition to loss processes, aerosol concentrations
during the early monsoon were found to be affected by primary emissions, most
likely from dust events
from the Thar Desert. This resulted in elevated fractions of the coarse mode,
PM&lt;sub&gt;2.5&amp;ndash;10&lt;/sub&gt; at both stations. In Mukteshwar, additional dust contribution
came from east of the station, from the Himalayan region. We also determined
the characteristic transition times between the pre-monsoon, monsoon and
post-monsoon. The onset and withdrawal transitions occurred faster in
Mukteshwar than in Gual Pahari, both being typically less than 10 days.
Transition periods in Gual Pahari took between 17 and 31 days. The shorter
transition times in Mukteshwar were probably related to the more intense
rains due to the mountain location, and the fact that the station was most of
the time in the free troposphere.</p>
</abstract>
<counts><page-count count="12"/></counts>
</article-meta>
</front>
<body/>
<back>
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</article>