Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model

Reviewed The rising global temperature is shifting the runoff patterns of snowmelt-dominated alpine watersheds, resulting in increased cold season flows, earlier spring peak flows, and reduced summer runoff. Projections of future runoff are beneficial in preparing for the anticipated changes in stre...

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Main Authors: Siemens, Kyle, Dibike, Yonas, Shrestha, Rajesh R., Prowse, Terry
Format: Article in Journal/Newspaper
Language:English
Published: Water 2021
Subjects:
Online Access:http://hdl.handle.net/1828/13019
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author Siemens, Kyle
Dibike, Yonas
Shrestha, Rajesh R.
Prowse, Terry
author_facet Siemens, Kyle
Dibike, Yonas
Shrestha, Rajesh R.
Prowse, Terry
author_sort Siemens, Kyle
collection Unknown
description Reviewed The rising global temperature is shifting the runoff patterns of snowmelt-dominated alpine watersheds, resulting in increased cold season flows, earlier spring peak flows, and reduced summer runoff. Projections of future runoff are beneficial in preparing for the anticipated changes in streamflow regimes. This study applied the degree–day Snowmelt Runoff Model (SRM) in combination with the MODIS to remotely sense snow cover observations for modeling the snowmelt runoff response of the Upper Athabasca River Basin in western Canada. After assessing its ability to simulate the observed historical flows, the SRM was applied for projecting future runoff in the basin. The inclusion of a spatial and temporal variation in the degree–day factor (DDF) and separation of the DDF for glaciated and non-glaciated areas were found to be important for improved simulation of varying snow conditions over multiple years. The SRM simulations, driven by an ensemble of six statistically downscaled GCM runs under the RCP8.5 scenario for the future period (2070–2080), show a consistent pattern in projected runoff change, with substantial increases in May runoff, smaller increases over the winter months, and decreased runoff in the summer months (June–August). Despite the SRM’s relative simplicity and requirement of only a few input variables, the model performed well in simulating historical flows, and provides runoff projections consistent with historical trends and previous modeling studies. This work was partially supported by a Discovery Grant from the Natural Sciences and Engineering Council of Canada (NSERC) to one of the co-authors and Environment and Climate Change Canada’s Climate Change and Adaptation program. Faculty
format Article in Journal/Newspaper
genre Athabasca River
genre_facet Athabasca River
geographic Athabasca River
Canada
geographic_facet Athabasca River
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institution Open Polar
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op_relation Siemens, K., Dibike, Y., Shrestha, R. R., & Prowse, T. (2021). Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model. Water, 13(9), 1-19. https://doi.org/10.3390/w13091199.
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spelling fttriple:oai:gotriple.eu:13019 2025-01-16T20:56:59+00:00 Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model Siemens, Kyle Dibike, Yonas Shrestha, Rajesh R. Prowse, Terry 2021-06-06 http://hdl.handle.net/1828/13019 en eng Water Siemens, K., Dibike, Y., Shrestha, R. R., & Prowse, T. (2021). Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model. Water, 13(9), 1-19. https://doi.org/10.3390/w13091199. 13019 http://hdl.handle.net/1828/13019 undefined UVic’s Research and Learning Repository envir geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2021 fttriple 2023-01-22T17:40:13Z Reviewed The rising global temperature is shifting the runoff patterns of snowmelt-dominated alpine watersheds, resulting in increased cold season flows, earlier spring peak flows, and reduced summer runoff. Projections of future runoff are beneficial in preparing for the anticipated changes in streamflow regimes. This study applied the degree–day Snowmelt Runoff Model (SRM) in combination with the MODIS to remotely sense snow cover observations for modeling the snowmelt runoff response of the Upper Athabasca River Basin in western Canada. After assessing its ability to simulate the observed historical flows, the SRM was applied for projecting future runoff in the basin. The inclusion of a spatial and temporal variation in the degree–day factor (DDF) and separation of the DDF for glaciated and non-glaciated areas were found to be important for improved simulation of varying snow conditions over multiple years. The SRM simulations, driven by an ensemble of six statistically downscaled GCM runs under the RCP8.5 scenario for the future period (2070–2080), show a consistent pattern in projected runoff change, with substantial increases in May runoff, smaller increases over the winter months, and decreased runoff in the summer months (June–August). Despite the SRM’s relative simplicity and requirement of only a few input variables, the model performed well in simulating historical flows, and provides runoff projections consistent with historical trends and previous modeling studies. This work was partially supported by a Discovery Grant from the Natural Sciences and Engineering Council of Canada (NSERC) to one of the co-authors and Environment and Climate Change Canada’s Climate Change and Adaptation program. Faculty Article in Journal/Newspaper Athabasca River Unknown Athabasca River Canada
spellingShingle envir
geo
Siemens, Kyle
Dibike, Yonas
Shrestha, Rajesh R.
Prowse, Terry
Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model
title Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model
title_full Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model
title_fullStr Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model
title_full_unstemmed Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model
title_short Runoff Projection from an Alpine Watershed in Western Canada: Application of a Snowmelt Runoff Model
title_sort runoff projection from an alpine watershed in western canada: application of a snowmelt runoff model
topic envir
geo
topic_facet envir
geo
url http://hdl.handle.net/1828/13019