Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada

The Town of Hay River, located in the Northwest Territories, Canada, is vulnerable to ice jam flooding occurring in the adjacent Hay River delta. The most extreme flooding events have occurred when ice jams in the channels of the delta were pushed downstream towards the mouth at Great Slave Lake. Th...

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Bibliographic Details
Main Authors: De Coste, Michael, She, Yuntong, Blackburn, Julia
Format: Article in Journal/Newspaper
Language:unknown
Published: NRC Research Press (a division of Canadian Science Publishing) 2017
Subjects:
Online Access:http://hdl.handle.net/1807/78063
http://www.nrcresearchpress.com/doi/abs/10.1139/cjce-2017-0123
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author De Coste, Michael
She, Yuntong
Blackburn, Julia
author_facet De Coste, Michael
She, Yuntong
Blackburn, Julia
author_sort De Coste, Michael
collection University of Toronto: Research Repository T-Space
description The Town of Hay River, located in the Northwest Territories, Canada, is vulnerable to ice jam flooding occurring in the adjacent Hay River delta. The most extreme flooding events have occurred when ice jams in the channels of the delta were pushed downstream towards the mouth at Great Slave Lake. This movement has been linked to incoming waves from ice jam release in the upstream reaches of the Hay River. This study incorporated the effect of an upstream ice jam release wave into the prediction of ice jam caused flood levels in the delta by integrating three one-dimensional models. The method was validated with observed breakup events and then used to simulate various combinations of ice and water conditions in the river and the delta. Multiple linear regression analyses were applied to the results to develop a prediction tool for assessing ice jam flood risk. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author.
format Article in Journal/Newspaper
genre Great Slave Lake
Hay River
Northwest Territories
genre_facet Great Slave Lake
Hay River
Northwest Territories
geographic Canada
Great Slave Lake
Hay River
Northwest Territories
geographic_facet Canada
Great Slave Lake
Hay River
Northwest Territories
id ftunivtoronto:oai:localhost:1807/78063
institution Open Polar
language unknown
long_lat ENVELOPE(-114.001,-114.001,61.500,61.500)
ENVELOPE(-115.847,-115.847,60.787,60.787)
op_collection_id ftunivtoronto
op_relation 0315-1468
http://hdl.handle.net/1807/78063
http://www.nrcresearchpress.com/doi/abs/10.1139/cjce-2017-0123
publishDate 2017
publisher NRC Research Press (a division of Canadian Science Publishing)
record_format openpolar
spelling ftunivtoronto:oai:localhost:1807/78063 2025-01-16T22:04:30+00:00 Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada De Coste, Michael She, Yuntong Blackburn, Julia 2017-05-24 http://hdl.handle.net/1807/78063 http://www.nrcresearchpress.com/doi/abs/10.1139/cjce-2017-0123 unknown NRC Research Press (a division of Canadian Science Publishing) 0315-1468 http://hdl.handle.net/1807/78063 http://www.nrcresearchpress.com/doi/abs/10.1139/cjce-2017-0123 Article 2017 ftunivtoronto 2020-06-17T12:05:32Z The Town of Hay River, located in the Northwest Territories, Canada, is vulnerable to ice jam flooding occurring in the adjacent Hay River delta. The most extreme flooding events have occurred when ice jams in the channels of the delta were pushed downstream towards the mouth at Great Slave Lake. This movement has been linked to incoming waves from ice jam release in the upstream reaches of the Hay River. This study incorporated the effect of an upstream ice jam release wave into the prediction of ice jam caused flood levels in the delta by integrating three one-dimensional models. The method was validated with observed breakup events and then used to simulate various combinations of ice and water conditions in the river and the delta. Multiple linear regression analyses were applied to the results to develop a prediction tool for assessing ice jam flood risk. The accepted manuscript in pdf format is listed with the files at the bottom of this page. The presentation of the authors' names and (or) special characters in the title of the manuscript may differ slightly between what is listed on this page and what is listed in the pdf file of the accepted manuscript; that in the pdf file of the accepted manuscript is what was submitted by the author. Article in Journal/Newspaper Great Slave Lake Hay River Northwest Territories University of Toronto: Research Repository T-Space Canada Great Slave Lake ENVELOPE(-114.001,-114.001,61.500,61.500) Hay River ENVELOPE(-115.847,-115.847,60.787,60.787) Northwest Territories
spellingShingle De Coste, Michael
She, Yuntong
Blackburn, Julia
Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada
title Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada
title_full Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada
title_fullStr Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada
title_full_unstemmed Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada
title_short Incorporating the effects of upstream ice jam release in the prediction of flood levels in the Hay River Delta, Canada
title_sort incorporating the effects of upstream ice jam release in the prediction of flood levels in the hay river delta, canada
url http://hdl.handle.net/1807/78063
http://www.nrcresearchpress.com/doi/abs/10.1139/cjce-2017-0123