Risk estimation for future glacier lake outburst floods based on local land-use changes

Effects of climate change are particularly strong in high-mountain regions. Most visibly, glaciers are shrinking at a rapid pace, and as a consequence, glacier lakes are forming or growing. At the same time the stability of mountain slopes is reduced by glacier retreat, permafrost thaw and other fac...

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Published in:Natural Hazards and Earth System Sciences
Main Authors: Nussbaumer, S., Schaub, Y., Huggel, C., Walz, A.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/nhess-14-1611-2014
https://nhess.copernicus.org/articles/14/1611/2014/
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spelling ftcopernicus:oai:publications.copernicus.org:nhess21469 2023-05-15T17:58:03+02:00 Risk estimation for future glacier lake outburst floods based on local land-use changes Nussbaumer, S. Schaub, Y. Huggel, C. Walz, A. 2018-09-27 application/pdf https://doi.org/10.5194/nhess-14-1611-2014 https://nhess.copernicus.org/articles/14/1611/2014/ eng eng doi:10.5194/nhess-14-1611-2014 https://nhess.copernicus.org/articles/14/1611/2014/ eISSN: 1684-9981 Text 2018 ftcopernicus https://doi.org/10.5194/nhess-14-1611-2014 2020-07-20T16:25:02Z Effects of climate change are particularly strong in high-mountain regions. Most visibly, glaciers are shrinking at a rapid pace, and as a consequence, glacier lakes are forming or growing. At the same time the stability of mountain slopes is reduced by glacier retreat, permafrost thaw and other factors, resulting in an increasing landslide hazard which can potentially impact lakes and therewith trigger far-reaching and devastating outburst floods. To manage risks from existing or future lakes, strategies need to be developed to plan in time for adequate risk reduction measures at a local level. However, methods to assess risks from future lake outbursts are not available and need to be developed to evaluate both future hazard and future damage potential. Here a method is presented to estimate future risks related to glacier lake outbursts for a local site in southern Switzerland (Naters, Valais). To generate two hazard scenarios, glacier shrinkage and lake formation modelling was applied, combined with simple flood modelling and field work. Furthermore, a land-use model was developed to quantify and allocate land-use changes based on local-to-regional storylines and three scenarios of land-use driving forces. Results are conceptualized in a matrix of three land-use and two hazard scenarios for the year 2045, and show the distribution of risk in the community of Naters, including high and very high risk areas. The study underlines the importance of combined risk management strategies focusing on land-use planning, on vulnerability reduction, as well as on structural measures (where necessary) to effectively reduce future risks related to lake outburst floods. Text permafrost Copernicus Publications: E-Journals Natural Hazards and Earth System Sciences 14 6 1611 1624
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collection Copernicus Publications: E-Journals
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language English
description Effects of climate change are particularly strong in high-mountain regions. Most visibly, glaciers are shrinking at a rapid pace, and as a consequence, glacier lakes are forming or growing. At the same time the stability of mountain slopes is reduced by glacier retreat, permafrost thaw and other factors, resulting in an increasing landslide hazard which can potentially impact lakes and therewith trigger far-reaching and devastating outburst floods. To manage risks from existing or future lakes, strategies need to be developed to plan in time for adequate risk reduction measures at a local level. However, methods to assess risks from future lake outbursts are not available and need to be developed to evaluate both future hazard and future damage potential. Here a method is presented to estimate future risks related to glacier lake outbursts for a local site in southern Switzerland (Naters, Valais). To generate two hazard scenarios, glacier shrinkage and lake formation modelling was applied, combined with simple flood modelling and field work. Furthermore, a land-use model was developed to quantify and allocate land-use changes based on local-to-regional storylines and three scenarios of land-use driving forces. Results are conceptualized in a matrix of three land-use and two hazard scenarios for the year 2045, and show the distribution of risk in the community of Naters, including high and very high risk areas. The study underlines the importance of combined risk management strategies focusing on land-use planning, on vulnerability reduction, as well as on structural measures (where necessary) to effectively reduce future risks related to lake outburst floods.
format Text
author Nussbaumer, S.
Schaub, Y.
Huggel, C.
Walz, A.
spellingShingle Nussbaumer, S.
Schaub, Y.
Huggel, C.
Walz, A.
Risk estimation for future glacier lake outburst floods based on local land-use changes
author_facet Nussbaumer, S.
Schaub, Y.
Huggel, C.
Walz, A.
author_sort Nussbaumer, S.
title Risk estimation for future glacier lake outburst floods based on local land-use changes
title_short Risk estimation for future glacier lake outburst floods based on local land-use changes
title_full Risk estimation for future glacier lake outburst floods based on local land-use changes
title_fullStr Risk estimation for future glacier lake outburst floods based on local land-use changes
title_full_unstemmed Risk estimation for future glacier lake outburst floods based on local land-use changes
title_sort risk estimation for future glacier lake outburst floods based on local land-use changes
publishDate 2018
url https://doi.org/10.5194/nhess-14-1611-2014
https://nhess.copernicus.org/articles/14/1611/2014/
genre permafrost
genre_facet permafrost
op_source eISSN: 1684-9981
op_relation doi:10.5194/nhess-14-1611-2014
https://nhess.copernicus.org/articles/14/1611/2014/
op_doi https://doi.org/10.5194/nhess-14-1611-2014
container_title Natural Hazards and Earth System Sciences
container_volume 14
container_issue 6
container_start_page 1611
op_container_end_page 1624
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