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<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMTD</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques Discussions</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMTD</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech. Discuss.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8610</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/amtd-4-7597-2011</article-id>
<title-group>
<article-title>Aerosol optical depth retrieval in the Arctic region using MODIS based on prior knowledge</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Mei</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Xue</surname>
<given-names>Y.</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>de Leeuw</surname>
<given-names>G.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
<xref ref-type="aff" rid="aff4">
<sup>4</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>Hou</surname>
<given-names>T.</given-names>
</name>
<xref ref-type="aff" rid="aff6">
<sup>6</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Guang</surname>
<given-names>J.</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>Yang</surname>
<given-names>L.</given-names>
</name>
<xref ref-type="aff" rid="aff7">
<sup>7</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="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Xu</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>He</surname>
<given-names>X.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff8">
<sup>8</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>State Key Laboratory of Remote Sensing Science, Jointly Sponsored by the Institute of Remote Sensing  Applications of Chinese Academy of Sciences and Beijing Normal University, Institute of Remote  Sensing Applications, Chinese Academy of Sciences, Beijin</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Faculty of Computing, London Metropolitan University, 166-220 Holloway  Road, London N7 8DB, UK</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Department of Physics, University of Helsinki, Helsinki, Finland</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Finnish Meteorological Institute, Climate Change Unit, Helsinki, Finland</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Netherlands Organisation for Applied Scientific Research TNO, Utrecht, The Netherlands</addr-line>
</aff>
<aff id="aff6">
<label>6</label>
<addr-line>Center for Earth Observation and Digital Earth of the Chinese Academy of Sciences, Beijing 100094,  China</addr-line>
</aff>
<aff id="aff7">
<label>7</label>
<addr-line>School of Geography, Beijing Normal University, Beijing 100875, China</addr-line>
</aff>
<aff id="aff8">
<label>8</label>
<addr-line>Graduate University of the Chinese Academy of Sciences, Beijing 100049, China</addr-line>
</aff>
<pub-date pub-type="epub">
<day>19</day>
<month>12</month>
<year>2011</year>
</pub-date>
<volume>4</volume>
<issue>6</issue>
<fpage>7597</fpage>
<lpage>7622</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2011 L. Mei 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://amt.copernicus.org/preprints/4/7597/2011/amtd-4-7597-2011.html">This article is available from https://amt.copernicus.org/preprints/4/7597/2011/amtd-4-7597-2011.html</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/preprints/4/7597/2011/amtd-4-7597-2011.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/preprints/4/7597/2011/amtd-4-7597-2011.pdf</self-uri>
<abstract>
<p>The Arctic is especially vulnerable to the long-term transport of aerosols and other pollutants
  because aerosols can affect the albedo of the surface by deposition on snow and ice. However,
  aerosol observations for this area are sparse and hence there is considerable uncertainty in the
  knowledge on the properties of the Arctic aerosol. Arctic aerosol observations are needed to fill
  this gap because these are among the basic and most important parameters for researching the
  Arctic environment. Atmospheric remote sensing using satellites offers us an opportunity to
  describe the aerosol distribution in terms of both local, regional and global coverage. However,
  AOD retrieval over a bright surface remains a difficult task because it is hard to separate and
  explicitly describe the contribution of the observed signal reflected by the variable surface and
  back scattering by the semi-transparent aerosols, especially with a large solar or sensor zenith
  angle. In this paper, an approach using a synergetic approach with Moderate Resolution Imaging
  Spectroradiometer (MODIS) data based on prior knowledge is presented. The detailed analysis of the
  model demonstrates that it is suitable for Arctic region AOD retrieval. Six AERONET stations at
  high latitude (Andenes, Barrow, Ittoqqortoormiit, OPAL, Thule, and Tiksi) were used for
  validation, and the correlation coefficient between retrieved AODs and AERONET AODs was 0.75 and
  the retrieval absolute error is approximately 0.1, while the relative error is 20% (at some
  stations with clear skies as low as 10% was found). Furthermore, the Russian wildfires that
  occurred in late July of 2010 and their effect on the Arctic environment is presented; Satellite
  retrieved AODs in the Arctic increased to 1.0 during 1 August and 15 August 2010, even 2.0, during
  the burning phase, and subsequently returned to normal values (lower than 0.1), which was fully in
  line with the AERONET observations. This indicates that the fire plumes were transported to the
  Arctic region.</p>
</abstract>
<counts><page-count count="26"/></counts>
</article-meta>
</front>
<body/>
<back>
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