Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada

Warmer air temperatures projected for the mid-21st century under climate change are expected to translate to increased evaporation and a re-distribution of precipitation around the world, including in the mid-latitude, continental Athabasca River region in northern Alberta, Canada. This study exami...

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Main Author: Walker, Gillian Sarah
Other Authors: Prowse, Terry Donald
Language:English
en
Published: 2016
Subjects:
Online Access:http://hdl.handle.net/1828/7253
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spelling ndltd-uvic.ca-oai-dspace.library.uvic.ca-1828-72532016-05-06T17:04:15Z Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada Walker, Gillian Sarah Prowse, Terry Donald Water balance Lakes Athabasca River Regional Climate Model Alberta Climate Change Precipitation Evaporation Surface Water Water Water Level Warmer air temperatures projected for the mid-21st century under climate change are expected to translate to increased evaporation and a re-distribution of precipitation around the world, including in the mid-latitude, continental Athabasca River region in northern Alberta, Canada. This study examines how these projected changes will affect the water balance of various lake sizes. A thermodynamic lake model, MyLake, is used to determine evaporation over three theoretical lake basins – a shallow lake, representative of perched basins in the Peace-Athabasca Delta near Fort Chipewyan; an intermediate-depth lake representative of industrial water storage near Fort McMurray; and a deep lake representative of future off-stream storage of water by industry, also near Fort McMurray. Bias-corrected climate data from an ensemble of Regional Climate Models are incorporated in MyLake, and the water balance is completed by calculating the change in storage as the difference between precipitation and evaporation. Results indicate that evaporation and precipitation are projected to increase in the future by similar magnitudes, thus not significantly changing the long-term water balance of the lakes. However, intra-annual precipitation and evaporation patterns are projected to shift within the year, changing seasonal water level cycles, and the magnitudes and frequencies of extreme 1-, 3- and 5-day weather events are projected to increase. These results demonstrate that future climate change adaptation and mitigation strategies should take into account increases in intra-annual variability and extreme events on water levels of lakes in mid-latitude, interior hydroclimatic regimes. Graduate 0368 walkerg@uvic.ca 2016-05-02T18:10:16Z 2016-05-02T18:10:16Z 2016 2016-05-02 Thesis http://hdl.handle.net/1828/7253 English en Available to the World Wide Web http://creativecommons.org/licenses/by-nc/2.5/ca/
collection NDLTD
language English
en
sources NDLTD
topic Water balance
Lakes
Athabasca River
Regional Climate Model
Alberta
Climate Change
Precipitation
Evaporation
Surface Water
Water
Water Level
spellingShingle Water balance
Lakes
Athabasca River
Regional Climate Model
Alberta
Climate Change
Precipitation
Evaporation
Surface Water
Water
Water Level
Walker, Gillian Sarah
Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada
description Warmer air temperatures projected for the mid-21st century under climate change are expected to translate to increased evaporation and a re-distribution of precipitation around the world, including in the mid-latitude, continental Athabasca River region in northern Alberta, Canada. This study examines how these projected changes will affect the water balance of various lake sizes. A thermodynamic lake model, MyLake, is used to determine evaporation over three theoretical lake basins – a shallow lake, representative of perched basins in the Peace-Athabasca Delta near Fort Chipewyan; an intermediate-depth lake representative of industrial water storage near Fort McMurray; and a deep lake representative of future off-stream storage of water by industry, also near Fort McMurray. Bias-corrected climate data from an ensemble of Regional Climate Models are incorporated in MyLake, and the water balance is completed by calculating the change in storage as the difference between precipitation and evaporation. Results indicate that evaporation and precipitation are projected to increase in the future by similar magnitudes, thus not significantly changing the long-term water balance of the lakes. However, intra-annual precipitation and evaporation patterns are projected to shift within the year, changing seasonal water level cycles, and the magnitudes and frequencies of extreme 1-, 3- and 5-day weather events are projected to increase. These results demonstrate that future climate change adaptation and mitigation strategies should take into account increases in intra-annual variability and extreme events on water levels of lakes in mid-latitude, interior hydroclimatic regimes. === Graduate === 0368 === walkerg@uvic.ca
author2 Prowse, Terry Donald
author_facet Prowse, Terry Donald
Walker, Gillian Sarah
author Walker, Gillian Sarah
author_sort Walker, Gillian Sarah
title Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada
title_short Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada
title_full Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada
title_fullStr Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada
title_full_unstemmed Effects of climate variability and change on surface water storage within the hydroclimatic regime of the Athabasca River, Alberta, Canada
title_sort effects of climate variability and change on surface water storage within the hydroclimatic regime of the athabasca river, alberta, canada
publishDate 2016
url http://hdl.handle.net/1828/7253
work_keys_str_mv AT walkergilliansarah effectsofclimatevariabilityandchangeonsurfacewaterstoragewithinthehydroclimaticregimeoftheathabascariveralbertacanada
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