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<front>
<journal-meta>
<journal-id journal-id-type="publisher">EGUsphere</journal-id>
<journal-title-group>
<journal-title>EGUsphere</journal-title>
<abbrev-journal-title abbrev-type="publisher">EGUsphere</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">EGUsphere</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub"></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/egusphere-2026-5055</article-id>
<title-group>
<article-title>3D surface displacements from digital image correlation on terrain models</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Oestreicher</surname>
<given-names>Nicolas</given-names>
<ext-link>https://orcid.org/0000-0003-2686-5769</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Denzinger</surname>
<given-names>Florian</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Manconi</surname>
<given-names>Andrea</given-names>
<ext-link>https://orcid.org/0000-0003-2930-4422</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>WSL Institute for Snow and Avalanche Research SLF, Davos Dorf, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Climate Change, Extremes and Natural Hazards in Alpine Regions Centre CERC, Davos Dorf, Switzerland</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>These authors contributed equally to this work.</addr-line>
</aff>
<pub-date pub-type="epub">
<day>25</day>
<month>09</month>
<year>2026</year>
</pub-date>
<volume>2026</volume>
<fpage>1</fpage>
<lpage>26</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Nicolas Oestreicher et al.</copyright-statement>
<copyright-year>2026</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5055/">This article is available from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5055/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5055/egusphere-2026-5055.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2026/egusphere-2026-5055/egusphere-2026-5055.pdf</self-uri>
<abstract>
<p>We present a methodology to retrieve 3D surface displacement based on Digital Image Correlation (DIC) applied&lt;br /&gt;to multitemporal terrain models. Our approach has been developed to overcome the DIC limitation in the vertical component&lt;br /&gt;of the displacement field when horizontal shifts are larger than the grid sampling. To validate the performance, we applied&lt;br /&gt;the approach to two terrain models acquired over the Brienz/Brinzauls landslide, where surface displacements affect the entire&lt;br /&gt;slope with heterogeneous amplitudes and directions. The comparison with in-situ measurements shows that DIC can accurately&lt;br /&gt;retrieve horizontal and vertical displacements, providing a clear representation of the spatial extent of the mass movement, as&lt;br /&gt;well as an accurate distinction of the internal landslide compartments. Our results are in good agreement with those obtained&lt;br /&gt;using a state-of-the-art point correlation method, but require less preprocessing and computational effort. Thus, the proposed&lt;br /&gt;DIC strategy can be considered as a valid alternative for measuring 3D surface displacements in scenarios where multitemporal&lt;br /&gt;terrain models are available.</p>
</abstract>
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