Investigation of Post-Fire Debris Flows in Montecito

Debris flows in a burned area, post-fire debris flows, are considered as one of the most dangerous geo-hazards due to their high velocity, long run-out distance, and huge destruction to infrastructures. The rainfall threshold to trigger such hazards is often reduced compared with normal debris flow...

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Main Authors: Yifei Cui, Deqiang Cheng, Dave Chan
Format: Article
Language:English
Published: MDPI AG 2018-12-01
Series:ISPRS International Journal of Geo-Information
Subjects:
Online Access:http://www.mdpi.com/2220-9964/8/1/5
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spelling doaj-2f69b84401b84d62aae9033b60d4f0de2020-11-25T00:10:21ZengMDPI AGISPRS International Journal of Geo-Information2220-99642018-12-0181510.3390/ijgi8010005ijgi8010005Investigation of Post-Fire Debris Flows in MontecitoYifei Cui0Deqiang Cheng1Dave Chan2Department of Civil and Environmental Engineering, Hong Kong University of Science and Technology, Clear Water Bay, Hong Kong, ChinaKey Laboratory of Mountain Hazards and Earth Surface Process, Institute of Mountain Hazards and Environment, Chinese Academy of Sciences, Chengdu 610041, ChinaDepartment of Civil and Environmental Engineering, University of Alberta, Edmonton, AB T6G 2W2, CanadaDebris flows in a burned area, post-fire debris flows, are considered as one of the most dangerous geo-hazards due to their high velocity, long run-out distance, and huge destruction to infrastructures. The rainfall threshold to trigger such hazards is often reduced compared with normal debris flow because ashes generated by mountain fires reduce the permeability of the top soil layer, thus increasing surface runoff. At the same time, burnt material and residual debris have very poor geo-mechanical characteristics, e.g., their internal friction angle and cohesion are typically low, and thus an intense rainfall can easily trigger some debris flows. Studying post-fire debris flow enables us to get a deeper understanding of disaster management. In this paper, the debris flow that occurred in Montecito, California, USA, and was affected by the Thomas Fire was used as a case study. Five major watersheds were extracted based on the digital elevation model (DEM). Remote sensing images were used to analyze the wildfire process, the extent of the burned areas, and the burn severity. The hypsometric integral (HI) and short-duration rainfall records of the watersheds around Montecito when the post-fire debris flows occurred were analyzed. Steep terrain, loose and abundant deposits, and sufficient water supply are the important conditions affecting the formation of debris flows. Taking watersheds as the research objects, HI was used to describe the geomorphic and topographic features, open-access rainfall data was used to represent the water supply, and burn severity represented the abundance of material sources. An occurrence probability model of post-fire debris flow based on HI, short-duration heavy rainfall, and burn severity was developed by using a logistic regression model in post-fire areas. By using this model, the occurrence probability of the post-fire debris flow in different watersheds around Montecito was analyzed based on the precipitation with time. Especially, the change characteristics of occurrence probability of debris flows over time based on the model bring a new perspective to observe the obvious change of the danger of post-fire debris flows and it is very useful for early warning of post-fire debris flows.http://www.mdpi.com/2220-9964/8/1/5post-fire debris flowMontecitohypsometric integrallogistic regression modelrainfallThomas Firemountain hazard
collection DOAJ
language English
format Article
sources DOAJ
author Yifei Cui
Deqiang Cheng
Dave Chan
spellingShingle Yifei Cui
Deqiang Cheng
Dave Chan
Investigation of Post-Fire Debris Flows in Montecito
ISPRS International Journal of Geo-Information
post-fire debris flow
Montecito
hypsometric integral
logistic regression model
rainfall
Thomas Fire
mountain hazard
author_facet Yifei Cui
Deqiang Cheng
Dave Chan
author_sort Yifei Cui
title Investigation of Post-Fire Debris Flows in Montecito
title_short Investigation of Post-Fire Debris Flows in Montecito
title_full Investigation of Post-Fire Debris Flows in Montecito
title_fullStr Investigation of Post-Fire Debris Flows in Montecito
title_full_unstemmed Investigation of Post-Fire Debris Flows in Montecito
title_sort investigation of post-fire debris flows in montecito
publisher MDPI AG
series ISPRS International Journal of Geo-Information
issn 2220-9964
publishDate 2018-12-01
description Debris flows in a burned area, post-fire debris flows, are considered as one of the most dangerous geo-hazards due to their high velocity, long run-out distance, and huge destruction to infrastructures. The rainfall threshold to trigger such hazards is often reduced compared with normal debris flow because ashes generated by mountain fires reduce the permeability of the top soil layer, thus increasing surface runoff. At the same time, burnt material and residual debris have very poor geo-mechanical characteristics, e.g., their internal friction angle and cohesion are typically low, and thus an intense rainfall can easily trigger some debris flows. Studying post-fire debris flow enables us to get a deeper understanding of disaster management. In this paper, the debris flow that occurred in Montecito, California, USA, and was affected by the Thomas Fire was used as a case study. Five major watersheds were extracted based on the digital elevation model (DEM). Remote sensing images were used to analyze the wildfire process, the extent of the burned areas, and the burn severity. The hypsometric integral (HI) and short-duration rainfall records of the watersheds around Montecito when the post-fire debris flows occurred were analyzed. Steep terrain, loose and abundant deposits, and sufficient water supply are the important conditions affecting the formation of debris flows. Taking watersheds as the research objects, HI was used to describe the geomorphic and topographic features, open-access rainfall data was used to represent the water supply, and burn severity represented the abundance of material sources. An occurrence probability model of post-fire debris flow based on HI, short-duration heavy rainfall, and burn severity was developed by using a logistic regression model in post-fire areas. By using this model, the occurrence probability of the post-fire debris flow in different watersheds around Montecito was analyzed based on the precipitation with time. Especially, the change characteristics of occurrence probability of debris flows over time based on the model bring a new perspective to observe the obvious change of the danger of post-fire debris flows and it is very useful for early warning of post-fire debris flows.
topic post-fire debris flow
Montecito
hypsometric integral
logistic regression model
rainfall
Thomas Fire
mountain hazard
url http://www.mdpi.com/2220-9964/8/1/5
work_keys_str_mv AT yifeicui investigationofpostfiredebrisflowsinmontecito
AT deqiangcheng investigationofpostfiredebrisflowsinmontecito
AT davechan investigationofpostfiredebrisflowsinmontecito
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