Coarse‐grained debris flow dynamics on erodible beds
S Lanzoni, C Gregoretti… - Journal of Geophysical …, 2017 - Wiley Online Library
A systematic set of flume experiments is used to investigate the features of velocity profiles
within the body of coarse‐grained debris flows and the dependence of the transport …
within the body of coarse‐grained debris flows and the dependence of the transport …
The morphological response of the Tegnas alpine catchment (Northeast Italy) to a Large Infrequent Disturbance
Abstract A recent storm (27th–30th October 2018), named Vaia, hit most part of the
Northeast of Italy affecting the geomorphic aspect of almost all mountain catchments of the …
Northeast of Italy affecting the geomorphic aspect of almost all mountain catchments of the …
Relevance of erosion processes when modelling in-channel gravel debris flows for efficient hazard assessment
A storm, composed of two delayed cells, hit the Monte Antelao slopes (Dolomites, North
Eastern Italy) in the early morning of July 18th, 2009. The resulting runoff triggered two …
Eastern Italy) in the early morning of July 18th, 2009. The resulting runoff triggered two …
GIS-based cell model for simulating debris flow runout on a fan
C Gregoretti, M Degetto, M Boreggio - Journal of Hydrology, 2016 - Elsevier
A GIS-based cell model, based on a kinematic approach is proposed to simulate debris flow
routing on a fan. The sediment–water mixture is modeled as a monophasic continuum, and …
routing on a fan. The sediment–water mixture is modeled as a monophasic continuum, and …
Runoff of small rocky headwater catchments: Field observations and hydrological modeling
C Gregoretti, M Degetto, M Bernard… - Water Resources …, 2016 - Wiley Online Library
In dolomitic headwater catchments, intense rainstorms of short duration produce runoff
discharges that often trigger debris flows on the scree slopes at the base of rock cliffs. In …
discharges that often trigger debris flows on the scree slopes at the base of rock cliffs. In …
Rainfall threshold calculation for debris flow early warning in areas with scarcity of data
HL Pan, YJ Jiang, J Wang… - Natural Hazards and Earth …, 2018 - nhess.copernicus.org
Debris flows are natural disasters that frequently occur in mountainous areas, usually
accompanied by serious loss of lives and properties. One of the most commonly used …
accompanied by serious loss of lives and properties. One of the most commonly used …
Exploring the initiating mechanism, monitoring equipment and warning indicators of gully-type debris flow for disaster reduction: a review
Y Du, H Liu, H Li, M Xie, SD Chicas, J Wu, F Lv, Y Wu - Natural Hazards, 2024 - Springer
Debris flow is a type of natural disaster characterized by sudden outbreaks, rapid movement,
short duration, and extreme destructive power, posing a serious threat to human lives and …
short duration, and extreme destructive power, posing a serious threat to human lives and …
An integrated study to evaluate debris flow hazard in alpine environment
Debris flows are among the most dangerous natural processes affecting the alpine
environment due to their magnitude (volume of transported material) and the long runout …
environment due to their magnitude (volume of transported material) and the long runout …
The debris flow occurred at Ru Secco Creek, Venetian Dolomites, on 4 August 2015: analysis of the phenomenon, its characteristics and reproduction by models
C Gregoretti, M Degetto, M Bernard… - Frontiers in Earth …, 2018 - frontiersin.org
On 4 August 2015, a very high intensity storm, 31.5 mm in 20 min (94.5 mm/h), hit the massif
of Mount Antelao on the Venetian Dolomites triggering three stony debris flows …
of Mount Antelao on the Venetian Dolomites triggering three stony debris flows …
A field investigation on debris flows in the incised Tongde sedimentary basin on the northeastern edge of the Tibetan Plateau
An investigation on 152 gullies along the Daheba River in the Tongde sedimentary basin
was performed. Debris flows develop in gullies with an excess topography ZE, which …
was performed. Debris flows develop in gullies with an excess topography ZE, which …