scholarly journals Debris flow modelling in Julian Alps using FLO-2D

Author(s):  
C. Calligaris ◽  
M. A. Boniello ◽  
L. Zini
2021 ◽  
Vol 1092 (1) ◽  
pp. 012041
Author(s):  
M A Khan ◽  
Z Mustaffa ◽  
A L B Balogun ◽  
M A M Al-Bared ◽  
A Ahmad

2021 ◽  
Author(s):  
Miguel Arestegui ◽  
Miluska Ordoñez ◽  
Abel Cisneros ◽  
Giorgio Madueño ◽  
Cinthia Almeida ◽  
...  

<p>Debris flow, locally known as huaycos, impact the east part of the metropolitan city of Lima, capital of Peru. However, after many extreme events such as the one related to the 2017 “Coastal Niño” or the one in 1987, there is a lack of historical data and sufficiently accurate monitoring systems.</p><p> </p><p>The fact that this area is densely populated presents obvious challenges, from social and physical perspectives, but also some opportunities. We present our experience using open source & low cost rain gauges on previously unmonitored microwatershed, as part of a broader watershed-level monitoring system enhancement by SENAMHI (National Meteorological and Hydrological Service). We also present our experience on linking monitoring systems, debris flow modelling and community based risk management towards developing operational EWS.</p>


2013 ◽  
Vol 5 (3) ◽  
Author(s):  
Mamodu Adegbe ◽  
Dinand Alkema ◽  
Victor G. Jetten ◽  
Ako Thomas Agbor ◽  
Idris Nda Abdullahi ◽  
...  
Keyword(s):  

Author(s):  
Andrej Šmuc ◽  
Karolina Janecka ◽  
Michał Lempa ◽  
Ryszard J. Kaczka

AbstractMass movements represent important processes that shape relief in Alpine areas. In this article, we present the spatio-temporal dynamics of the Ciprnik landslide (Julian Alps, NW Slovenia) and interpret its triggering and evolution. In the study area, mass movement activity is characterised by two phases: normal deposition on the fluvial fans that dominated up to 2000, and a more active phase related to the triggering of the Ciprnik complex landslide and formation of an additional debris-flow fan. The Ciprnik landslide started as a translational movement over the discontinuity plane that was mobilised into a debris-flow. The triggering and slope failure resulted from a combination of tectonics (i.e. dip-slope position of the strata, and strong fracturing), lithology (alternation of thin beds of carbonates and fine-grained clastics), and accumulation of precipitation. The debris-flow fan remains active and interfingers with adjacent active fluvial fans.


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