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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>
</journal-title-group>
<issn pub-type="epub">1680-7375</issn>
<publisher><publisher-name>Copernicus GmbH</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/acpd-11-10485-2011</article-id>
<title-group>
<article-title>Study on long-term aerosol distribution over the land of East China using MODIS data</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>He</surname>
<given-names>Q.</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>Li</surname>
<given-names>C.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Geng</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>Lei</surname>
<given-names>Y.</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>Li</surname>
<given-names>Y.</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>Tie</surname>
<given-names>X.</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>Yin</surname>
<given-names>Q.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Shanghai Meteorological Bureau, Shanghai, China</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Laboratory for Climate and Ocean-Atmosphere Studies, Department of Atmospheric Sciences, School of Physics, Peking University, Beijing, China</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Meteorological Observation Centre of CMA, Beijing, China</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Shanxi Meteorological Bureau, Taiyuan, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>04</day>
<month>04</month>
<year>2011</year>
</pub-date>
<volume>11</volume>
<issue>4</issue>
<fpage>10485</fpage>
<lpage>10523</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>
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<self-uri xlink:href="http://www.atmos-chem-phys-discuss.net/11/10485/2011/acpd-11-10485-2011.pdf">The full text article is available as a PDF file from http://www.atmos-chem-phys-discuss.net/11/10485/2011/acpd-11-10485-2011.pdf</self-uri>
<abstract>
<p>East China is among the fastest developing and most populous area in Asia,
where atmospheric aerosol loading is high due to heavy urban and industrial
emission. These aerosols may have significant impact on regional climate and
environment. In this report, MODIS level 2 aerosol products (2000–2007) were
used to study aerosol spatial and temporal distributions, as well as their
variations with local meteorological conditions over East China. By
combining Aerosol Optical Depth (AOD) and aerosol Fine Mode Fraction (FMF),
we found that the urban/industrial aerosol and dust are two dominant species
over northern part, whereas continental, marine and mixed aerosols dominate
the southern part of East China, except for Poyang Lake Plain. Both annual
mean AOD and area with high AOD increased from 2000 to 2007, with the
largest increase seen in Yangtze River Delta region (YRD). In summer, AOD in
East China reached the maximum of about 0.8 in YRD, dominated by fine mode
particles. The minimum AOD occurred in winter with mostly coarse mode
particles. The higher AOD in spring is attributed to coarse particles. Local
aerosol properties were analyzed in three typical zones: the northern dry
zone (I), the central urban/industrial zone (II)
and the southern natural background zone (III). Monthly mean AODs in zone I and II were above
0.5 throughout the entire year, with the maximum AOD in June. High FMFs in
this period indicated heavy urban and industrial pollutions. Monthly mean
AODs and FMFs in zone III reached maximum of 0.51 in April and
September (up to 90.7%) respectively. High AOD in spring in zone III
 appears mostly due to the long-range dust transport from the North.
In fact, dust particles contributed 50–80% to aerosol loading in zone
I and II, but only 20% in zone III. The effect of meteorological conditions such as temperature,
relative humidity (RH) and wind on aerosol loadings over East China were
also investigated.</p>
</abstract>
<counts><page-count count="39"/></counts>
</article-meta>
</front>
<body/>
<back>
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