Articles | Volume 18, issue 1
https://doi.org/10.5194/nhess-18-31-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/nhess-18-31-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Invited perspectives: Hydrological perspectives on precipitation intensity-duration thresholds for landslide initiation: proposing hydro-meteorological thresholds
Water Resources Section, Faculty of Civil Engineering and
Geosciences, Delft University of Technology, Delft, the Netherlands
Roberto Greco
Dipartimento di Ingegneria Civile Design Edilizia e Ambiente,
Università degli Studi della Campania Luigi Vanvitelli, Aversa (CE),
Italy
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Discussed (final revised paper)
Latest update: 23 Nov 2024
Short summary
The vast majority of shallow landslides and debris flows are precipitation initiated and predicted using historical landslides plotted versus observed precipitation information. However, this approach has severe limitations. This is partly due to the fact that it is not precipitation that initiates a landslide or debris flow but rather the hydrological dynamics in the soil and slope. We propose to include hydrological information in the regional hydro-meteorological hazard assessment.
The vast majority of shallow landslides and debris flows are precipitation initiated and...
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