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<front>
<journal-meta>
<journal-id journal-id-type="publisher">NHESS</journal-id>
<journal-title-group>
<journal-title>Natural Hazards and Earth System Sciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">NHESS</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Nat. Hazards Earth Syst. Sci.</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1684-9981</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/nhess-13-3169-2013</article-id>
<title-group>
<article-title>Shallow landslide&apos;s stochastic risk modelling based on the precipitation event of August 2005 in Switzerland: results and implications</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nicolet</surname>
<given-names>P.</given-names>
<ext-link>https://orcid.org/0000-0001-8777-9472</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>Foresti</surname>
<given-names>L.</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>Caspar</surname>
<given-names>O.</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>Jaboyedoff</surname>
<given-names>M.</given-names>
<ext-link>https://orcid.org/0000-0002-6419-695X</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Center of Research on Terrestrial Environment, University of Lausanne, Lausanne, Switzerland</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Royal Meteorological Institute of Belgium, Brussels, Belgium</addr-line>
</aff>
<pub-date pub-type="epub">
<day>09</day>
<month>12</month>
<year>2013</year>
</pub-date>
<volume>13</volume>
<issue>12</issue>
<fpage>3169</fpage>
<lpage>3184</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 P. Nicolet et al.</copyright-statement>
<copyright-year>2013</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://nhess.copernicus.org/articles/13/3169/2013/nhess-13-3169-2013.html">This article is available from https://nhess.copernicus.org/articles/13/3169/2013/nhess-13-3169-2013.html</self-uri>
<self-uri xlink:href="https://nhess.copernicus.org/articles/13/3169/2013/nhess-13-3169-2013.pdf">The full text article is available as a PDF file from https://nhess.copernicus.org/articles/13/3169/2013/nhess-13-3169-2013.pdf</self-uri>
<abstract>
<p>Due to their relatively unpredictable characteristics,
      shallow landslides represent a risk for human
      infrastructures. Multiple shallow landslides can be triggered by
       widespread intense
      precipitation events. The event of August 2005 in Switzerland
      is used in order to propose a risk model to predict the expected
      number of landslides based on the precipitation amounts and
      lithological units. The spatial distribution of rainfall is
      characterized by merging data coming from operational weather radars
      and a dense network of rain gauges with an artificial neural
      network. Lithologies are grouped into four main units, with similar
      characteristics. Then, from a landslide inventory containing more than
      5000 landslides, a probabilistic relation linking the precipitation
      amount and the lithology to the number of landslides in
      a 1 km&lt;sup&gt;2&lt;/sup&gt; cell, is derived. In a next step, this relation is
      used to randomly redistribute the landslides using Monte Carlo
      simulations. The probability for a landslide to reach a building is
      assessed using stochastic geometry and the damage cost is assessed
      from the estimated mean damage cost using an exponential distribution
      to account for the variability. Although the model reproduces well
      the number of landslides, the number of affected buildings is underestimated. This seems to result from the human
      influence on landslide occurrence. Such a model might be useful to
      characterize the risk resulting from shallow  landslides and its
      variability.</p>
</abstract>
<counts><page-count count="16"/></counts>
</article-meta>
</front>
<body/>
<back>
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