An assessment procedure for glacial hazards in the Swiss Alps

Glacial hazards such as ice avalanches, glacial lake outburst floods, and debris flows have caused severe damage in populated mountain regions such as the Swiss Alps. Assessment of such hazards must consider basic glaciological, geomorphological, and hydraulic principles together with experience gai...

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Bibliographic Details
Published inCanadian geotechnical journal Vol. 41; no. 6; pp. 1068 - 1083
Main Authors Huggel, Christian, Haeberli, Wilfried, Kääb, Andreas, Bieri, Daniel, Richardson, Shaun
Format Journal Article
LanguageEnglish
Published Ottawa, Canada NRC Research Press 01.12.2004
National Research Council of Canada
Canadian Science Publishing NRC Research Press
Subjects
Online AccessGet full text
ISSN0008-3674
1208-6010
DOI10.1139/t04-053

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Abstract Glacial hazards such as ice avalanches, glacial lake outburst floods, and debris flows have caused severe damage in populated mountain regions such as the Swiss Alps. Assessment of such hazards must consider basic glaciological, geomorphological, and hydraulic principles together with experience gained from previous events. An approach is presented here to assess the maximum event magnitude and probability of occurrence of glacial hazards. Analysis of magnitude is based on empirical relationships derived from published case histories from the Swiss Alps and other mountain regions. Probability of occurrence is difficult to estimate because of rapid changes in the nature of glacial systems, the low frequency of events, and the high complexity of the involved processes. Here, the probability is specified in qualitative and systematic terms based on indicators such as dam type, geometry, and freeboard height (for glacial lakes) and tendency of avalanche repetition, precursor events, and increased water supply to the glacier bed (for ice avalanche events). The assessment procedures are applied to a recent lake outburst with subsequent debris flow and to an ice avalanche in the Swiss Alps. The results yield reasonable event maxima that were not exceeded by actual events. The methods provide first-order assessments and may be applied in dynamic mountain environments where population and infrastructure growth require continuous evaluation of hazards.Key words: glacial hazards, lake outburst, debris flow, ice avalanche, hazard assessment procedure, probability of occurrence.
AbstractList Glacial hazards such as ice avalanches, glacial lake outburst floods, and debris flows have caused severe damage in populated mountain regions such as the Swiss Alps. Assessment of such hazards must consider basic glaciological, geomorphological, and hydraulic principles together with experience gained from previous events. An approach is presented here to assess the maximum event magnitude and probability of occurrence of glacial hazards. Analysis of magnitude is based on empirical relationships derived from published case histories from the Swiss Alps and other mountain regions. Probability of occurrence is difficult to estimate because of rapid changes in the nature of glacial systems, the low frequency of events, and the high complexity of the involved processes. Here, the probability is specified in qualitative and systematic terms based on indicators such as dam type, geometry, and freeboard height (for glacial lakes) and tendency of avalanche repetition, precursor events, and increased water supply to the glacier bed (for ice avalanche events). The assessment procedures are applied to a recent lake outburst with subsequent debris flow and to an ice avalanche in the Swiss Alps. The results yield reasonable event maxima that were not exceeded by actual events. The methods provide first-order assessments and may be applied in dynamic mountain environments where population and infrastructure growth require continuous evaluation of hazards. [PUBLICATION ABSTRACT]
Glacial hazards such as ice avalanches, glacial lake outburst floods, and debris flows have caused severe damage in populated mountain regions such as the Swiss Alps. Assessment of such hazards must consider basic glaciological, geomorphological, and hydraulic principles together with experience gained from previous events. An approach is presented here to assess the maximum event magnitude and probability of occurrence of glacial hazards. Analysis of magnitude is based on empirical relationships derived from published case histories from the Swiss Alps and other mountain regions. Probability of occurrence is difficult to estimate because of rapid changes in the nature of glacial systems, the low frequency of events, and the high complexity of the involved processes. Here, the probability is specified in qualitative and systematic terms based on indicators such as dam type, geometry, and freeboard height (for glacial lakes) and tendency of avalanche repetition, precursor events, and increased water supply to the glacier bed (for ice avalanche events). The assessment procedures are applied to a recent lake outburst with subsequent debris flow and to an ice avalanche in the Swiss Alps. The results yield reasonable event maxima that were not exceeded by actual events. The methods provide first-order assessments and may be applied in dynamic mountain environments where population and infrastructure growth require continuous evaluation of hazards. [PUBLICATION ABSTRACT] Key words: glacial hazards, lake outburst, debris flow, ice avalanche, hazard assessment procedure, probability of occurrence.
Glacial hazards such as ice avalanches, glacial lake outburst floods, and debris flows have caused severe damage in populated mountain regions such as the Swiss Alps. Assessment of such hazards must consider basic glaciological, geomorphological, and hydraulic principles together with experience gained from previous events. An approach is presented here to assess the maximum event magnitude and probability of occurrence of glacial hazards. Analysis of magnitude is based on empirical relationships derived from published case histories from the Swiss Alps and other mountain regions. Probability of occurrence is difficult to estimate because of rapid changes in the nature of glacial systems, the low frequency of events, and the high complexity of the involved processes. Here, the probability is specified in qualitative and systematic terms based on indicators such as dam type, geometry, and freeboard height (for glacial lakes) and tendency of avalanche repetition, precursor events, and increased water supply to the glacier bed (for ice avalanche events). The assessment procedures are applied to a recent lake outburst with subsequent debris flow and to an ice avalanche in the Swiss Alps. The results yield reasonable event maxima that were not exceeded by actual events. The methods provide first-order assessments and may be applied in dynamic mountain environments where population and infrastructure growth require continuous evaluation of hazards.Key words: glacial hazards, lake outburst, debris flow, ice avalanche, hazard assessment procedure, probability of occurrence.
Abstract_FL Des dangers glaciaires tels que des avalanches, des inondations par déversements de lacs glaciaires ont causé des dommages importants dans les régions montagneuses peuplées telles que les Alpes suisses. L'évaluation de tels dangers doit prendre en compte les principes de base de glaciologie, de géomorphologie, et d'hydraulique de même que de l'expérience obtenue par les événements antérieures. On présente ici une approche pour évaluer l'événement d'amplitude et de probabilité d'occurrence maximales d'événements de dangers glaciaires. L'analyse de l'amplitude est basée sur des relations empiriques dérivées d'histoires de cas publiées pour les Alpes Suisses et autres régions montagneuses. La probabilité d'occurrence est difficile à estimer à cause des changements rapides de la nature des systèmes glaciaires, de la faible fréquence des événements, et de la forte complexité des processus impliqués. Ici, la probabilité est spécifiée en termes qualitatifs et systématiques basés sur des indicateurs tels que le type de barrage, sa géométrie et sa hauteur de revanche (pour les lacs glaciaires), la tendance à la répétition d'avalanches, les événements précurseurs, et l'accroissement de l'alimentation en eau du lit des glaciers (pour les événements d'avalanches de glace). Les procédures d'évaluation sont appliquées à un récent déversement de lac avec écoulement de débris subséquent et à une avalanche de glace dans les Alpes suisses. Les méthodes fournissent des évaluations de premier ordre et peuvent être appliquées à des environnements montagneux dynamiques où l'accroissement des populations et des infrastructures requiert une évaluation continue des dangers.Mots clés : dangers glaciaires, déversement de lac, écoulement de débris, avalanche de glace, procédure d'évaluation de risque, probabilité d'occurrence.[Traduit par la Rédaction]
Author Kääb, Andreas
Richardson, Shaun
Bieri, Daniel
Haeberli, Wilfried
Huggel, Christian
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  fullname: Richardson, Shaun
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Issue 6
Keywords experimental studies
glaciers
glaciology
floods
damage
Europe
glacial lakes
probability
ice
indicators
dams
frequency
amplitude
hydraulics
avalanches
ICI Company
debris
geometry
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Snippet Glacial hazards such as ice avalanches, glacial lake outburst floods, and debris flows have caused severe damage in populated mountain regions such as the...
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nrcresearch
SourceType Aggregation Database
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Enrichment Source
Publisher
StartPage 1068
SubjectTerms Avalanches
Debris flow
Detritus
Earth sciences
Earth, ocean, space
Engineering and environment geology. Geothermics
Engineering geology
Exact sciences and technology
Glacial drift
Glacial lakes
Glaciers
Hazards
Ice
Mountain regions
Probability
Water supply
Title An assessment procedure for glacial hazards in the Swiss Alps
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