EGU2020-10327, updated on 11 Jan 2021
https://doi.org/10.5194/egusphere-egu2020-10327
EGU General Assembly 2020
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Debris-flow volume quantile prediction from catchment morphometry

Alexander Densmore1 and Tjalling de Haas2
Alexander Densmore and Tjalling de Haas
  • 1Institute of Hazard, Risk, and Resilience and Department of Geography, Durham University, Durham, United Kingdom (a.l.densmore@durham.ac.uk)
  • 2Department of Physical Geography, Universiteit Utrecht, Utrecht, The Netherlands (T.deHaas@uu.nl)

Estimation of the volumes of potential future debris flows is key for hazard assessment and mitigation. Worldwide, however, there are few catchments for which detailed volume-frequency information is available. We (1) reconstruct volume-frequency curves for 10 debris-flow catchments in Saline Valley, California, USA, from a large number of well-preserved, unmodified surficial flow deposits, and (2) assess the correlations between lobe-volume quantiles and a set of morphometric catchment characteristics. We find statistically-significant correlations between lobe-volume quantiles, including median and maximum, and catchment relief, length (planimetric distance from the fan apex to the most distant point along the watershed boundary), perimeter, and Melton ratio (relief divided by the square root of catchment area). These findings show that it may be possible to roughly estimate debris-flow lobe-volume quantiles from basic catchment characteristics that can be obtained from globally-available elevation data. This may assist with design-volume estimation in debris-flow catchments where past flow volumes are otherwise unknown.

How to cite: Densmore, A. and de Haas, T.: Debris-flow volume quantile prediction from catchment morphometry, EGU General Assembly 2020, Online, 4–8 May 2020, EGU2020-10327, https://doi.org/10.5194/egusphere-egu2020-10327, 2020