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<front>
<journal-meta>
<journal-id journal-id-type="publisher">AMT</journal-id>
<journal-title-group>
<journal-title>Atmospheric Measurement Techniques</journal-title>
<abbrev-journal-title abbrev-type="publisher">AMT</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Atmos. Meas. Tech.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1867-8548</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/amt-5-2703-2012</article-id>
<title-group>
<article-title>Comparison of satellite microwave backscattering (ASCAT) and visible/near-infrared reflectances (PARASOL) for the estimation of aeolian aerodynamic roughness length in arid and semi-arid regions</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Prigent</surname>
<given-names>C.</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>Jiménez</surname>
<given-names>C.</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>Catherinot</surname>
<given-names>J.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>CNRS &amp;ndash; UMR8112, Laboratoire d&apos;Etudes du Rayonnement et de la Matière en Astrophysique, Observatoire de Paris, Paris, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>11</month>
<year>2012</year>
</pub-date>
<volume>5</volume>
<issue>11</issue>
<fpage>2703</fpage>
<lpage>2712</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2012 C. Prigent et al.</copyright-statement>
<copyright-year>2012</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/articles/5/2703/2012/amt-5-2703-2012.html">This article is available from https://amt.copernicus.org/articles/5/2703/2012/amt-5-2703-2012.html</self-uri>
<self-uri xlink:href="https://amt.copernicus.org/articles/5/2703/2012/amt-5-2703-2012.pdf">The full text article is available as a PDF file from https://amt.copernicus.org/articles/5/2703/2012/amt-5-2703-2012.pdf</self-uri>
<abstract>
<p>Previous studies examined the possibility to estimate the aeolian aerodynamic
roughness length from satellites, either from visible/near-infrared
observations or from microwave backscattering measurements. Here we compare
the potential of the two approaches and propose to merge the two sources of
information to benefit from their complementary aspects, i.e. the high
spatial resolution of the visible/near-infrared (6 km for PARASOL that is
part of the A-Train) and the independence from atmospheric contamination of
the active microwaves (ASCAT on board MetOp with a lower spatial resolution
of 25 km). A global map of the aeolian aerodynamic roughness length at 6 km
resolution is derived, for arid and semi-arid regions. It shows very good
consistency with the existing information on the properties of these
surfaces. The dataset is available to the community, for use in atmospheric
dust transport models.</p>
</abstract>
<counts><page-count count="10"/></counts>
</article-meta>
</front>
<body/>
<back>
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