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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ISPRS-Archives</journal-id>
<journal-title-group>
<journal-title>The International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">ISPRS-Archives</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Int. Arch. Photogramm. Remote Sens. Spatial Inf. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2194-9034</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/isprs-archives-XLI-B4-117-2016</article-id>
<title-group>
<article-title>EVALUATION OF ASTER GDEM V3 USING ICESAT LASER ALTIMETRY</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Carabajal</surname>
<given-names>C. 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>Boy</surname>
<given-names>J.-P.</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Sigma Space Corporation @ NASA/GSFC, Planetary Geodynamics Laboratory – Code 698, Greenbelt, MD 20771, USA</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>EOST/IPGS (UMR 7516 Université de Strasbourg / CNRS), 5 rue René Descartes, 67084 Strasbourg, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>13</day>
<month>06</month>
<year>2016</year>
</pub-date>
<volume>XLI-B4</volume>
<fpage>117</fpage>
<lpage>124</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2016 C. C. Carabajal</copyright-statement>
<copyright-year>2016</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://isprs-archives.copernicus.org/articles/XLI-B4/117/2016/isprs-archives-XLI-B4-117-2016.html">This article is available from https://isprs-archives.copernicus.org/articles/XLI-B4/117/2016/isprs-archives-XLI-B4-117-2016.html</self-uri>
<self-uri xlink:href="https://isprs-archives.copernicus.org/articles/XLI-B4/117/2016/isprs-archives-XLI-B4-117-2016.pdf">The full text article is available as a PDF file from https://isprs-archives.copernicus.org/articles/XLI-B4/117/2016/isprs-archives-XLI-B4-117-2016.pdf</self-uri>
<abstract>
<p>We have used a set of Ground Control Points (GCPs) derived from altimetry measurements from the Ice, Cloud and land Elevation
Satellite (ICESat) to evaluate the quality of the 30 m posting ASTER (Advanced Spaceborne Thermal Emission and Reflection
Radiometer) Global Digital Elevation Model (GDEM) V3 elevation products produced by NASA/METI for Greenland and
Antarctica. These data represent the highest quality globally distributed altimetry measurements that can be used for geodetic ground
control, selected by applying rigorous editing criteria, useful at high latitudes, where other topographic control is scarce. Even if
large outliers still remain in all ASTER GDEM V3 data for both, Greenland and Antarctica, they are significantly reduced when
editing ASTER by number of scenes (N≥5) included in the elevation processing. For 667,354 GCPs in Greenland, differences show a
mean of 13.74 m, a median of -6.37 m, with an RMSE of 109.65 m. For Antarctica, 6,976,703 GCPs show a mean of 0.41 m, with a
median of -4.66 m, and a 54.85 m RMSE, displaying smaller means, similar medians, and less scatter than GDEM V2. Mean and
median differences between ASTER and ICESat are lower than 10 m, and RMSEs lower than 10 m for Greenland, and 20 m for
Antarctica when only 9 to 31 scenes are included.</p>
</abstract>
<counts><page-count count="8"/></counts>
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