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<front>
<journal-meta>
<journal-id journal-id-type="publisher">ISPRS-Annals</journal-id>
<journal-title-group>
<journal-title>ISPRS Annals of the Photogrammetry, Remote Sensing and Spatial Information Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">ISPRS-Annals</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">ISPRS Ann. Photogramm. Remote Sens. Spatial Inf. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">2194-9050</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-annals-XI-3-2026-903-2026</article-id>
<title-group>
<article-title>Tracking Snow Avalanches: Integrating Field Observations and Satellite-Derived Indicators</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kaushik</surname>
<given-names>Suvrat</given-names>
<ext-link>https://orcid.org/0000-0002-8947-5234</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Karbou</surname>
<given-names>Fatima</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>Viallon-Galinier</surname>
<given-names>Léo</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>Mauss</surname>
<given-names>Adrien</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Météo-France, CNRS, CNRM, Centre d’ Études de la Neige, 38000, Grenoble, France</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Météo-France, Centre de Météorologie Spatiale (CMS), 22300, Lannion, France</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>07</month>
<year>2026</year>
</pub-date>
<volume>XI-3-2026</volume>
<fpage>903</fpage>
<lpage>910</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2026 Suvrat Kaushik 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://isprs-annals.copernicus.org/articles/XI-3-2026/903/2026/isprs-annals-XI-3-2026-903-2026.html">This article is available from https://isprs-annals.copernicus.org/articles/XI-3-2026/903/2026/isprs-annals-XI-3-2026-903-2026.html</self-uri>
<self-uri xlink:href="https://isprs-annals.copernicus.org/articles/XI-3-2026/903/2026/isprs-annals-XI-3-2026-903-2026.pdf">The full text article is available as a PDF file from https://isprs-annals.copernicus.org/articles/XI-3-2026/903/2026/isprs-annals-XI-3-2026-903-2026.pdf</self-uri>
<abstract>
<p>In this study, we integrated information from the French avalanche database, high-resolution digital elevation models (DEMs), and Sentinel-1 SAR images to model avalanche extents for events occurring across three distinct time periods in three French massifs. The modelled avalanche extents were compared with manually delineated polygons mapped over SAR RGB composites generated using the principles applied in colour-based change-detection algorithms. The comparison revealed strong correspondence between the two independent approaches, with IoU values ranging from 0.42 to 0.47 and F1 scores from 0.58 to 0.63 across the different massifs. We further analyzed the distribution of SAR backscatter values in pre- and post-event images across different zones of the avalanche paths. The results indicated that a fixed 3 dB threshold would most likely be insufficient to capture the full avalanche extent, as some zones showed backscatter increases of less than 3 dB in post-event SAR imagery. As a result, a multi-threshold approach based on different avalanche zones is recommended. Finally, we assessed the potential of Sentinel-2 optical imagery to detect surface changes and characterize the physical behaviour of avalanche-affected paths following intense avalanche events. However, the results were inconsistent, showing the expected trends in one study area but nearly opposite patterns in the other, suggesting that integrating optical data for automated avalanche mapping may not always be reliable.</p>
</abstract>
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