<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>Wicki, Adrian</dc:creator>
  <dc:creator>Lehmann, Peter</dc:creator>
  <dc:creator>Hauck, Christian</dc:creator>
  <dc:creator>Seneviratne, Sonia I.</dc:creator>
  <dc:creator>Waldner, Peter</dc:creator>
  <dc:creator>Stähli, Manfred</dc:creator>
  <dc:date>2020-04-15</dc:date>
  <dc:description xmlns:ns0="xml" ns0:lang="en">In mountainous terrain, rainfall-induced landslides pose a serious risk to people  and infrastructure. Regional landslide early warning systems (LEWS) have  proven to be a cost-efficient tool to inform the public about the imminent  landslide danger. While most operational LEWS are based on rainfall  exceedance thresholds only, recent studies have demonstrated an improvement  of the forecast quality after the inclusion of soil hydrological information. In this  study, the potential of in situ soil moisture measurements for regional landslide  early warning is assessed. For the first time, a comprehensive soil moisture  measurement database was compiled for Switzerland and compared with a  national landslide database (Swiss flood and landslide damage database,  WSL). The time series were homogenized and normalized to represent  saturation values. From ensembles of sensors, the mean and standard  deviation saturation were calculated and infiltration events were delimited,  characterized, and classified as landslide-triggering or non-triggering based on  the occurrence of landslides within a specified forecast distance. A logistic  regression function was applied to model the landslide activity based on the  infiltration event characteristics and several models were analysed and  compared with receiver operating characteristics (ROC). A strong distance  dependence becomes apparent showing a forecast goodness decrease with  increasing distance between water content measurement site and landslide,  and a better forecast goodness for long-lasting as opposed to short-duration  precipitation events. While most variability can be explained by the two event  properties antecedent saturation and change of saturation during an infiltration  event, event properties that describe antecedent conditions are more important  for long-lasting as opposed to short-duration precipitation events that can be  better explained by properties describing event dynamics. Overall, the analysis  demonstrated that in situ soil moisture data effectively contains specific  information useful for landslide early warning.</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>https://folia.unifr.ch/global/documents/308430</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308430/files/hau_aps.pdf</dc:identifier>
  <dc:identifier>https://folia.unifr.ch/documents/308430/files/hau_aps_sm.pdf</dc:identifier>
  <dc:language>eng</dc:language>
  <dc:relation>info:eu-repo/semantics/altIdentifier/doi/10.1007/s10346-020-01400-y</dc:relation>
  <dc:rights>info:eu-repo/semantics/openAccess</dc:rights>
  <dc:rights>License undefined</dc:rights>
  <dc:source>Landslides. - 2020, vol. 17, no. 8, p. 1881-1896</dc:source>
  <dc:subject>info:eu-repo/classification/udc/55</dc:subject>
  <dc:title xmlns:ns1="xml" ns1:lang="en">Assessing the potential of soil moisture measurements for regional landslide early warning</dc:title>
  <dc:type>http://purl.org/coar/resource_type/c_6501</dc:type>
</oai_dc:dc>
