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  <controlfield tag="001">4152</controlfield>
  <controlfield tag="005">20190221073103.0</controlfield>
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    <subfield code="a">CTALK-2019-0100</subfield>
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  <datafield tag="100" ind1=" " ind2=" ">
    <subfield code="a">Delforge, D.</subfield>
  </datafield>
  <datafield tag="245" ind1=" " ind2=" ">
    <subfield code="a">Hydrological connectivity from causal analysis of time series in the Lhomme Karst System, Belgium</subfield>
  </datafield>
  <datafield tag="260" ind1=" " ind2=" ">
    <subfield code="c">2019</subfield>
  </datafield>
  <datafield tag="269" ind1=" " ind2=" ">
    <subfield code="c">2019-04-08</subfield>
  </datafield>
  <datafield tag="520" ind1=" " ind2=" ">
    <subfield code="a">The  hydrological  behaviour  of  karstic  systems  is  difficult  to  theorize  holistically  because  of  their  specificheterogeneities leading to distinctive nonlinear processes. Karstified systems present great opportunities for fieldexploration and hydrogeological monitoring of the vadose zone through its network of caves and conduits. Theseunique but explorable environments are predisposed to an inductive scientific approach where transfer processesassociated with hydrological connections are directly inferred from the data.This is done conventionally using dye tracing from which connections and transfer times are undeniably revealed.However, single tests do not allow appreciating the dynamic character of the hydrological connections. Nowadays,several  data  analysis  methods  aim  at  the  detection  of  causal  relationships  between  time  series  allowing  theinvestigation of dynamics and interactions. Some are designed for linear systems as the simple cross-correlationmethod or the Granger causality, while others are suitable for nonlinear interactions, such as the Convergent CrossMapping method.Here, these methods are applied in order to draw up causal maps and compare short-term (up to 2 days) interactionsin the Lhomme Karst System in Belgium. The Lhomme Karst System has been monitored since 2013 and manytime series are available: meteorological data, soil moisture, drip discharges in the caves, piezometric levels, andlocal gravimetric time series. In addition, dye tracing experiments revealing connections and characteristic transfertimes were conducted. The different causal maps are compared and causal interactions are appreciated throughthe  current  knowledge  of  the  system  and  discussed  in  relation  to  the  question:  can  we  infer  true  hydrologicalconnections and processes from the empirical determination of causal relationships between hydrological timeseries?</subfield>
  </datafield>
  <datafield tag="536" ind1=" " ind2=" ">
    <subfield code="a">FRIA/</subfield>
    <subfield code="c">FRIA/</subfield>
    <subfield code="f">FRIA</subfield>
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  <datafield tag="594" ind1=" " ind2=" ">
    <subfield code="a">NO</subfield>
  </datafield>
  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">Karst</subfield>
  </datafield>
  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">Rochefort</subfield>
  </datafield>
  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">Causal analysis</subfield>
  </datafield>
  <datafield tag="653" ind1="1" ind2=" ">
    <subfield code="a">Non-linear system</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Van Camp, M.</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Vanclooster, M.</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Hallet, V.</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Kaufmann, O.</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Poulain, A.</subfield>
  </datafield>
  <datafield tag="700" ind1=" " ind2=" ">
    <subfield code="a">Watlet, A.</subfield>
  </datafield>
  <datafield tag="773" ind1=" " ind2=" ">
    <subfield code="t">EGU, Vienna</subfield>
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  <datafield tag="856" ind1="0" ind2=" ">
    <subfield code="f">michel.vancamp@observatoire.be</subfield>
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  <datafield tag="906" ind1=" " ind2=" ">
    <subfield code="a">Contributed</subfield>
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    <subfield code="a">CTALKCONT</subfield>
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