Ice‐jam flood risk assessment and mapping

Abstract In northern regions, river ice‐ jam flooding can be more severe than open‐water flooding causing property and infrastructure damages, loss of human life and adverse impacts on aquatic ecosystems. Very little has been performed to assess the risk induced by ice‐related floods because most ri...

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Published in:Hydrological Processes
Main Authors: Lindenschmidt, Karl‐Erich, Das, Apurba, Rokaya, Prabin, Chu, Thuan
Other Authors: Natural Sciences and Engineering Research Council
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2016
Subjects:
Online Access:http://dx.doi.org/10.1002/hyp.10853
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spelling crwiley:10.1002/hyp.10853 2024-10-13T14:10:08+00:00 Ice‐jam flood risk assessment and mapping Lindenschmidt, Karl‐Erich Das, Apurba Rokaya, Prabin Chu, Thuan Natural Sciences and Engineering Research Council 2016 http://dx.doi.org/10.1002/hyp.10853 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.10853 https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10853 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Hydrological Processes volume 30, issue 21, page 3754-3769 ISSN 0885-6087 1099-1085 journal-article 2016 crwiley https://doi.org/10.1002/hyp.10853 2024-09-17T04:44:37Z Abstract In northern regions, river ice‐ jam flooding can be more severe than open‐water flooding causing property and infrastructure damages, loss of human life and adverse impacts on aquatic ecosystems. Very little has been performed to assess the risk induced by ice‐related floods because most risk assessments are limited to open‐water floods. The specific objective of this study is to incorporate ice‐jam numerical modelling tools (e.g. RIVICE, Monte‐Carlo simulation) into flood hazard and risk assessment along the Peace River at the Town of Peace River (TPR) in Alberta, Canada. Adequate historical data for different ice‐jam and open‐water flooding events were available for this study site and were useful in developing ice‐affected stage‐frequency curves. These curves were then applied to calibrate a numerical hydraulic model, which simulated different ice jams and flood scenarios along the Peace River at the TPR. A Monte‐Carlo analysis was then carried out to acquire an ensemble of water level profiles to determine the 1 : 100‐year and 1 : 200‐year annual exceedance probability flood stages for the TPR. These flood stages were then used to map flood hazard and vulnerability of the TPR. Finally, the flood risk for a 200‐year return period was calculated to be an average of $32/m 2 /a ($/m 2 /a corresponds to a unit of annual expected damages or risk). Copyright © 2016 John Wiley & Sons, Ltd. Article in Journal/Newspaper Peace River Wiley Online Library Canada Hydrological Processes 30 21 3754 3769
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract In northern regions, river ice‐ jam flooding can be more severe than open‐water flooding causing property and infrastructure damages, loss of human life and adverse impacts on aquatic ecosystems. Very little has been performed to assess the risk induced by ice‐related floods because most risk assessments are limited to open‐water floods. The specific objective of this study is to incorporate ice‐jam numerical modelling tools (e.g. RIVICE, Monte‐Carlo simulation) into flood hazard and risk assessment along the Peace River at the Town of Peace River (TPR) in Alberta, Canada. Adequate historical data for different ice‐jam and open‐water flooding events were available for this study site and were useful in developing ice‐affected stage‐frequency curves. These curves were then applied to calibrate a numerical hydraulic model, which simulated different ice jams and flood scenarios along the Peace River at the TPR. A Monte‐Carlo analysis was then carried out to acquire an ensemble of water level profiles to determine the 1 : 100‐year and 1 : 200‐year annual exceedance probability flood stages for the TPR. These flood stages were then used to map flood hazard and vulnerability of the TPR. Finally, the flood risk for a 200‐year return period was calculated to be an average of $32/m 2 /a ($/m 2 /a corresponds to a unit of annual expected damages or risk). Copyright © 2016 John Wiley & Sons, Ltd.
author2 Natural Sciences and Engineering Research Council
format Article in Journal/Newspaper
author Lindenschmidt, Karl‐Erich
Das, Apurba
Rokaya, Prabin
Chu, Thuan
spellingShingle Lindenschmidt, Karl‐Erich
Das, Apurba
Rokaya, Prabin
Chu, Thuan
Ice‐jam flood risk assessment and mapping
author_facet Lindenschmidt, Karl‐Erich
Das, Apurba
Rokaya, Prabin
Chu, Thuan
author_sort Lindenschmidt, Karl‐Erich
title Ice‐jam flood risk assessment and mapping
title_short Ice‐jam flood risk assessment and mapping
title_full Ice‐jam flood risk assessment and mapping
title_fullStr Ice‐jam flood risk assessment and mapping
title_full_unstemmed Ice‐jam flood risk assessment and mapping
title_sort ice‐jam flood risk assessment and mapping
publisher Wiley
publishDate 2016
url http://dx.doi.org/10.1002/hyp.10853
https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fhyp.10853
https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10853
geographic Canada
geographic_facet Canada
genre Peace River
genre_facet Peace River
op_source Hydrological Processes
volume 30, issue 21, page 3754-3769
ISSN 0885-6087 1099-1085
op_rights http://onlinelibrary.wiley.com/termsAndConditions#vor
op_doi https://doi.org/10.1002/hyp.10853
container_title Hydrological Processes
container_volume 30
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