2009
DOI: 10.1002/hyp.7369
|View full text |Cite
|
Sign up to set email alerts
|

Investigating the impact of the Chi‐Chi earthquake on the occurrence of debris flows using artificial neural networks

Abstract: Abstract:Debris flows have caused enormous losses of property and human life in Taiwan during the last two decades. An efficient and reliable method for predicting the occurrence of debris flows is required. The major goal of this study is to explore the impact of the Chi-Chi earthquake on the occurrence of debris flows by applying the artificial neural network (ANN) that takes both hydrological and geomorphologic influences into account. The Chen-Yu-Lan River watershed, which is located in central Taiwan, is … Show more

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
2
1

Citation Types

0
3
0

Year Published

2013
2013
2024
2024

Publication Types

Select...
7

Relationship

0
7

Authors

Journals

citations
Cited by 13 publications
(3 citation statements)
references
References 25 publications
0
3
0
Order By: Relevance
“…The variables that determine the debris-flow hazard of an area can be grouped into two general categories: 1) the intrinsic or static variables that contribute to debris-flow susceptibility, such as geology, slope gradient, slope aspect, longterm drainage patterns, elevation, and material cohesion; and 2) the dynamic or extrinsic variables that tend to trigger debris flows in an area of given susceptibility, such as heavy rainfall events and earthquakes [3], [5], [12], [50]. In this study, we are carrying on a debris-flow susceptibility investigation that is by definition the spatial analysis of the intrinsic factors; it expresses the likelihood of debris-flow occurrences at each spatial element [21].…”
Section: Identification Of Factors Controlling the Distribution Ofmentioning
confidence: 99%
“…The variables that determine the debris-flow hazard of an area can be grouped into two general categories: 1) the intrinsic or static variables that contribute to debris-flow susceptibility, such as geology, slope gradient, slope aspect, longterm drainage patterns, elevation, and material cohesion; and 2) the dynamic or extrinsic variables that tend to trigger debris flows in an area of given susceptibility, such as heavy rainfall events and earthquakes [3], [5], [12], [50]. In this study, we are carrying on a debris-flow susceptibility investigation that is by definition the spatial analysis of the intrinsic factors; it expresses the likelihood of debris-flow occurrences at each spatial element [21].…”
Section: Identification Of Factors Controlling the Distribution Ofmentioning
confidence: 99%
“…Lin et al, 2003;Dadson et al, 2004;Koi et al, 2008;Liu et al, 2008;Chang et al, 2009;Chen et al, 2011;; J.C. Tang et al, 2012;Xu et al, 2012). Due to earthquake-induced landslides and other reasons, the activity of debris flows may change significantly after a strong earthquake compared with that before the earthquake (Dadson et al, 2004;Koi et al, 2008; J.C. .…”
Section: Introductionmentioning
confidence: 99%
“…The magnitude and frequency of debris flows can increase sharply while the critical rainfall to trigger the debris flows can decrease obviously (e.g. Lin et al, 2003;Chang et al, 2009;Chen et al, 2011;Tang et al, 2012). A stronger ground motion would lead to a larger change in debris flow density (Liu et al, 2008).…”
Section: Introductionmentioning
confidence: 99%