Multi-Methodological Investigation of the Biersdorf Hillslope Debris Flow (Rheinland-Pfalz, Germany) Associated to the Torrential Rainfall Event of 14 July 2021

Publikationstyp:
Zeitschriftenaufsatz
Metadaten:
Autoren
  • Teemu Hagge-Kubat
  • Peter Fischer
  • Philip Suesser
  • Philipp Rotter
  • Ansgar Wehinger
  • Andreas Voett
  • Frieder Enzmann
Autoren-URL
https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=fis-test-1&SrcAuth=WosAPI&KeyUT=WOS:000818129100001&DestLinkType=FullRecord&DestApp=WOS_CPL
DOI
10.3390/geosciences12060245
eISSN
2076-3263
Externe Identifier
  • Clarivate Analytics Document Solution ID: 2N1DO
Ausgabe der Veröffentlichung
6
Zeitschrift
GEOSCIENCES
Schlüsselwörter
  • torrential rainfall event of 14 July 2021
  • Eifel flood
  • mass movement
  • hillslope debris flow
  • multi-methodological approach
  • runout modelling
  • MABEIS-project
Artikelnummer
ARTN 245
Datum der Veröffentlichung
2022
Status
Published
Titel
Multi-Methodological Investigation of the Biersdorf Hillslope Debris Flow (Rheinland-Pfalz, Germany) Associated to the Torrential Rainfall Event of 14 July 2021
Sub types
  • Article
Ausgabe der Zeitschrift
12

Datenquelle: Web of Science (Lite)

Andere Metadatenquellen:
Abstract
<jats:p>The investigation of mass movements is of major interest in mountain regions as these events represent a significant hazard for people and cause severe damage to crucial infrastructure. The torrential rainfall event that mainly occurred on the 14 July 2021 in western Central Europe not only led to severe flooding catastrophes (e.g., Meuse, Ahr and Erft rivers) but also triggered hundreds of mass movements in the low mountain range. Here, we investigate a hillslope debris flow that occurred in Biersdorf in the Eifel area (Rhenish Massif, Rheinland-Pfalz) using a comprehensive geomorphological–geophysical approach in order to better understand the triggering mechanisms and process dynamics. We combined field studies by means of Electrical Resistivity Tomography (ERT), Direct Push Hydraulic Profiling (HPT) and sediment coring with UAV-generated photogrammetry, as well as debris flow runout modelling. Our results show that for the Biersdorf hillslope debris flow, the geomorphological and geotectonic position played a crucial role. The hillslope debris flow was triggered at a normal fault separating well-draining limestones of the Lower Muschelkalk, from dense weathered clay and sandstones of the Upper Buntsandstein. The combination of a large surface runoff and strong interflow at the sliding surface caused a transformation from an initial translational slide into the high-energy and widespread hillslope debris flow. We further created and validated a stand-alone model of the debris flow on a local scale achieving promising results. The model yields a 97% match to the observed runout area as well as to deposition spreads and heights. Thus, our study provides a pathway for analyzing hillslope debris flows triggered by torrential rainfall events in low mountain ranges. General knowledge on hillslope debris flows, risk assessment and hazard prevention were improved, and results can be transferred to other regions to improve risk assessment and hazard prevention.</jats:p>
Autoren
  • Teemu Hagge-Kubat
  • Peter Fischer
  • Philip Süßer
  • Philipp Rotter
  • Ansgar Wehinger
  • Andreas Vött
  • Frieder Enzmann
DOI
10.3390/geosciences12060245
eISSN
2076-3263
Ausgabe der Veröffentlichung
6
Zeitschrift
Geosciences
Sprache
en
Online publication date
2022
Paginierung
245 - 245
Status
Published online
Herausgeber
MDPI AG
Herausgeber URL
http://dx.doi.org/10.3390/geosciences12060245
Datum der Datenerfassung
2022
Titel
Multi-Methodological Investigation of the Biersdorf Hillslope Debris Flow (Rheinland-Pfalz, Germany) Associated to the Torrential Rainfall Event of 14 July 2021
Ausgabe der Zeitschrift
12

Datenquelle: Crossref

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