A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management

This study used a comparison of one hundred and forty-eight historical (1888-1913) and current (2008-2014) oblique photographs from thirty-two stations to identify land cover changes that have occurred in portions of the Bow and Elbow valleys as well as surrounding Kananaskis Country region. Implica...

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Bibliographic Details
Main Author: Taggart-Hodge, Tanya
Other Authors: Higgs, Eric
Language:English
en
Published: 2016
Subjects:
Online Access:http://hdl.handle.net/1828/7655
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spelling ndltd-uvic.ca-oai-dspace.library.uvic.ca-1828-76552016-12-10T17:01:40Z A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management Taggart-Hodge, Tanya Higgs, Eric Mountains Bow watershed Canmore Banff Mountain Legacy Project Repeat Photography Land cover Landscape Rocky Mountains Environmental sciences Environmental studies Change detection Ecological restoration Novel ecosystems River Human footprint This study used a comparison of one hundred and forty-eight historical (1888-1913) and current (2008-2014) oblique photographs from thirty-two stations to identify land cover changes that have occurred in portions of the Bow and Elbow valleys as well as surrounding Kananaskis Country region. Implications of these changes for flooding and flood management were explored. Forest cover was found to have drastically increased over the past century, particularly in the Bow valley, as did areas of direct human development. In the same time period, grasslands increased in the Elbow valley but decreased in the Bow, while regenerating areas decreased uniformly throughout both valleys. An analysis of pre (2008)-and-post (2014) flood conditions demonstrated no change in coniferous forest cover in both valleys over the 6-year period, but uncovered a decline of 20% in the Elbow and 3% in the Bow in the broadleaf/mixedwood category. The Elbow’s channel zone was larger in 2014 compared to 2008, whereas the extent of the Bow’s channel zone remained constant. However, both the Bow and Elbow’s bare exposed bars increased substantially, most likely as a result of the 2013 flood. The major source of water flows that contributed to the 2013 flood event originated in high elevation rock and scree areas, which, unlike floodplains, are elements of the watershed that cannot be manipulated over time. It is now recognized that forest cover should act as a buffer to floods. Nevertheless, the 2013 flood event occurred despite the massive buffering effect of a huge increase in older forest stands across the study area. The final discussion includes recommendations for improving flood management in the area. Graduate 0329, 0768, 0478 tanya.taggarthodge@gmail.com 2016-12-09T22:59:40Z 2016-12-09T22:59:40Z 2016 2016-12-09 Thesis http://hdl.handle.net/1828/7655 English en Available to the World Wide Web http://creativecommons.org/licenses/by-nc-nd/2.5/ca/
collection NDLTD
language English
en
sources NDLTD
topic Mountains
Bow watershed
Canmore
Banff
Mountain Legacy Project
Repeat Photography
Land cover
Landscape
Rocky Mountains
Environmental sciences
Environmental studies
Change detection
Ecological restoration
Novel ecosystems
River
Human footprint
spellingShingle Mountains
Bow watershed
Canmore
Banff
Mountain Legacy Project
Repeat Photography
Land cover
Landscape
Rocky Mountains
Environmental sciences
Environmental studies
Change detection
Ecological restoration
Novel ecosystems
River
Human footprint
Taggart-Hodge, Tanya
A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management
description This study used a comparison of one hundred and forty-eight historical (1888-1913) and current (2008-2014) oblique photographs from thirty-two stations to identify land cover changes that have occurred in portions of the Bow and Elbow valleys as well as surrounding Kananaskis Country region. Implications of these changes for flooding and flood management were explored. Forest cover was found to have drastically increased over the past century, particularly in the Bow valley, as did areas of direct human development. In the same time period, grasslands increased in the Elbow valley but decreased in the Bow, while regenerating areas decreased uniformly throughout both valleys. An analysis of pre (2008)-and-post (2014) flood conditions demonstrated no change in coniferous forest cover in both valleys over the 6-year period, but uncovered a decline of 20% in the Elbow and 3% in the Bow in the broadleaf/mixedwood category. The Elbow’s channel zone was larger in 2014 compared to 2008, whereas the extent of the Bow’s channel zone remained constant. However, both the Bow and Elbow’s bare exposed bars increased substantially, most likely as a result of the 2013 flood. The major source of water flows that contributed to the 2013 flood event originated in high elevation rock and scree areas, which, unlike floodplains, are elements of the watershed that cannot be manipulated over time. It is now recognized that forest cover should act as a buffer to floods. Nevertheless, the 2013 flood event occurred despite the massive buffering effect of a huge increase in older forest stands across the study area. The final discussion includes recommendations for improving flood management in the area. === Graduate === 0329, 0768, 0478 === tanya.taggarthodge@gmail.com
author2 Higgs, Eric
author_facet Higgs, Eric
Taggart-Hodge, Tanya
author Taggart-Hodge, Tanya
author_sort Taggart-Hodge, Tanya
title A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management
title_short A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management
title_full A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management
title_fullStr A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management
title_full_unstemmed A century of landscape-level changes in the Bow watershed, Alberta, Canada, and implications for flood management
title_sort century of landscape-level changes in the bow watershed, alberta, canada, and implications for flood management
publishDate 2016
url http://hdl.handle.net/1828/7655
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