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Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides
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| Zeitschriftentitel: | Hydrological Processes |
|---|---|
| Personen und Körperschaften: | , , |
| In: | Hydrological Processes, 23, 2009, 10, S. 1444-1460 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
Wiley
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| Schlagwörter: |
| author_facet |
Frattini, Paolo Crosta, Giovanni Sosio, Rosanna Frattini, Paolo Crosta, Giovanni Sosio, Rosanna |
|---|---|
| author |
Frattini, Paolo Crosta, Giovanni Sosio, Rosanna |
| spellingShingle |
Frattini, Paolo Crosta, Giovanni Sosio, Rosanna Hydrological Processes Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides Water Science and Technology |
| author_sort |
frattini, paolo |
| spelling |
Frattini, Paolo Crosta, Giovanni Sosio, Rosanna 0885-6087 1099-1085 Wiley Water Science and Technology http://dx.doi.org/10.1002/hyp.7269 <jats:title>Abstract</jats:title><jats:p>Probabilistic thresholds for triggering shallow landslides by rainfall are developed using two approaches: a logistic regression model and Iverson's physically based model. Both approaches are applied to a 180 km<jats:sup>2</jats:sup> area in northern Italy. For the physically based model a Monte Carlo approach is used to obtain probabilities of slope failure associated with differing combinations of rainfall intensity and duration as well as differing topographic settings. For the logistic regression model hourly and daily rainfall data and split‐sample testing are used to explore the effect of antecedent rainfall on triggering thresholds. It is demonstrated that both the statistical and physically based models provide stochastic thresholds that express the probability of landslide triggering. The resulting thresholds are comparable, even though the two approaches are conceptually different. The physically based model also provides an estimate of the percentage of potentially unstable areas in which failure can be triggered with a certain probability. The return period of rainfall responsible for landslide triggering is studied by using a Gumbel scaling model of rainfall intensity–duration–frequency curves. It is demonstrated that antecedent rainfall must be taken into account in landslide forecasting, and a method is proposed to correct the rainfall return period by filtering the rainfall maxima with a fixed threshold of antecedent rainfall. This correction produces an increase of the return periods, especially for rainstorms of short duration. Copyright © 2009 John Wiley & Sons, Ltd.</jats:p> Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides Hydrological Processes |
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Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
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Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
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Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
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Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
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Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_short |
Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_sort |
approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| topic |
Water Science and Technology |
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http://dx.doi.org/10.1002/hyp.7269 |
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2009 |
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1444-1460 |
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<jats:title>Abstract</jats:title><jats:p>Probabilistic thresholds for triggering shallow landslides by rainfall are developed using two approaches: a logistic regression model and Iverson's physically based model. Both approaches are applied to a 180 km<jats:sup>2</jats:sup> area in northern Italy. For the physically based model a Monte Carlo approach is used to obtain probabilities of slope failure associated with differing combinations of rainfall intensity and duration as well as differing topographic settings. For the logistic regression model hourly and daily rainfall data and split‐sample testing are used to explore the effect of antecedent rainfall on triggering thresholds. It is demonstrated that both the statistical and physically based models provide stochastic thresholds that express the probability of landslide triggering. The resulting thresholds are comparable, even though the two approaches are conceptually different. The physically based model also provides an estimate of the percentage of potentially unstable areas in which failure can be triggered with a certain probability. The return period of rainfall responsible for landslide triggering is studied by using a Gumbel scaling model of rainfall intensity–duration–frequency curves. It is demonstrated that antecedent rainfall must be taken into account in landslide forecasting, and a method is proposed to correct the rainfall return period by filtering the rainfall maxima with a fixed threshold of antecedent rainfall. This correction produces an increase of the return periods, especially for rainstorms of short duration. Copyright © 2009 John Wiley & Sons, Ltd.</jats:p> |
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| description | <jats:title>Abstract</jats:title><jats:p>Probabilistic thresholds for triggering shallow landslides by rainfall are developed using two approaches: a logistic regression model and Iverson's physically based model. Both approaches are applied to a 180 km<jats:sup>2</jats:sup> area in northern Italy. For the physically based model a Monte Carlo approach is used to obtain probabilities of slope failure associated with differing combinations of rainfall intensity and duration as well as differing topographic settings. For the logistic regression model hourly and daily rainfall data and split‐sample testing are used to explore the effect of antecedent rainfall on triggering thresholds. It is demonstrated that both the statistical and physically based models provide stochastic thresholds that express the probability of landslide triggering. The resulting thresholds are comparable, even though the two approaches are conceptually different. The physically based model also provides an estimate of the percentage of potentially unstable areas in which failure can be triggered with a certain probability. The return period of rainfall responsible for landslide triggering is studied by using a Gumbel scaling model of rainfall intensity–duration–frequency curves. It is demonstrated that antecedent rainfall must be taken into account in landslide forecasting, and a method is proposed to correct the rainfall return period by filtering the rainfall maxima with a fixed threshold of antecedent rainfall. This correction produces an increase of the return periods, especially for rainstorms of short duration. Copyright © 2009 John Wiley & Sons, Ltd.</jats:p> |
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| spelling | Frattini, Paolo Crosta, Giovanni Sosio, Rosanna 0885-6087 1099-1085 Wiley Water Science and Technology http://dx.doi.org/10.1002/hyp.7269 <jats:title>Abstract</jats:title><jats:p>Probabilistic thresholds for triggering shallow landslides by rainfall are developed using two approaches: a logistic regression model and Iverson's physically based model. Both approaches are applied to a 180 km<jats:sup>2</jats:sup> area in northern Italy. For the physically based model a Monte Carlo approach is used to obtain probabilities of slope failure associated with differing combinations of rainfall intensity and duration as well as differing topographic settings. For the logistic regression model hourly and daily rainfall data and split‐sample testing are used to explore the effect of antecedent rainfall on triggering thresholds. It is demonstrated that both the statistical and physically based models provide stochastic thresholds that express the probability of landslide triggering. The resulting thresholds are comparable, even though the two approaches are conceptually different. The physically based model also provides an estimate of the percentage of potentially unstable areas in which failure can be triggered with a certain probability. The return period of rainfall responsible for landslide triggering is studied by using a Gumbel scaling model of rainfall intensity–duration–frequency curves. It is demonstrated that antecedent rainfall must be taken into account in landslide forecasting, and a method is proposed to correct the rainfall return period by filtering the rainfall maxima with a fixed threshold of antecedent rainfall. This correction produces an increase of the return periods, especially for rainstorms of short duration. Copyright © 2009 John Wiley & Sons, Ltd.</jats:p> Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides Hydrological Processes |
| spellingShingle | Frattini, Paolo, Crosta, Giovanni, Sosio, Rosanna, Hydrological Processes, Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides, Water Science and Technology |
| title | Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_full | Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_fullStr | Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_full_unstemmed | Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_short | Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_sort | approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| title_unstemmed | Approaches for defining thresholds and return periods for rainfall‐triggered shallow landslides |
| topic | Water Science and Technology |
| url | http://dx.doi.org/10.1002/hyp.7269 |