Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin
Climate change is anticipated to impact the hydrology of the Saskatchewan River, which originates in the Canadian Rockies mountain range. To better understand the climate change impacts in the mountain headwaters of this basin, a physically based hydrological model was developed for this basin using...
Published in: | Hydrology and Earth System Sciences |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2020
|
Subjects: | |
Online Access: | https://doi.org/10.5194/hess-24-2731-2020 https://doaj.org/article/46290a7f35a349329ed23ba1b676b8cb |
id |
ftdoajarticles:oai:doaj.org/article:46290a7f35a349329ed23ba1b676b8cb |
---|---|
record_format |
openpolar |
spelling |
ftdoajarticles:oai:doaj.org/article:46290a7f35a349329ed23ba1b676b8cb 2023-05-15T18:40:42+02:00 Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin X. Fang J. W. Pomeroy 2020-05-01T00:00:00Z https://doi.org/10.5194/hess-24-2731-2020 https://doaj.org/article/46290a7f35a349329ed23ba1b676b8cb EN eng Copernicus Publications https://www.hydrol-earth-syst-sci.net/24/2731/2020/hess-24-2731-2020.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 doi:10.5194/hess-24-2731-2020 1027-5606 1607-7938 https://doaj.org/article/46290a7f35a349329ed23ba1b676b8cb Hydrology and Earth System Sciences, Vol 24, Pp 2731-2754 (2020) Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 article 2020 ftdoajarticles https://doi.org/10.5194/hess-24-2731-2020 2022-12-31T04:05:22Z Climate change is anticipated to impact the hydrology of the Saskatchewan River, which originates in the Canadian Rockies mountain range. To better understand the climate change impacts in the mountain headwaters of this basin, a physically based hydrological model was developed for this basin using the Cold Regions Hydrological Modelling platform (CRHM) for Marmot Creek Research Basin ( ∼9.4 km 2 ), located in the Front Ranges of the Canadian Rockies. Marmot Creek is composed of ecozones ranging from montane forests to alpine tundra and alpine exposed rock and includes both large and small clearcuts. The model included blowing and intercepted snow redistribution, sublimation, energy-balance snowmelt, slope and canopy effects on melt, Penman–Monteith evapotranspiration, infiltration to frozen and unfrozen soils, hillslope hydrology, streamflow routing, and groundwater components and was parameterised without calibration from streamflow. Near-surface outputs from the 4 km Weather Research and Forecasting (WRF) model were bias-corrected using the quantile delta mapping method with respect to meteorological data from five stations located from low-elevation montane forests to alpine ridgetops and running over October 2005–September 2013. The bias-corrected WRF outputs during a current period (2005–2013) and a future pseudo global warming period (PGW, 2091–2099) were used to drive model simulations to assess changes in Marmot Creek's hydrology. Under a “business-as-usual” forcing scenario, Representative Concentration Pathway 8.5 (RCP8.5) in PGW, the basin will warm up by 4.7 ∘ C and receive 16 % more precipitation, which will lead to a 40 mm decline in seasonal peak snowpack, 84 mm decrease in snowmelt volume, 0.2 mm d −1 slower melt rate, and 49 d shorter snow-cover duration. The alpine snow season will be shortened by almost 1.5 months, but at some lower elevations there will be large decreases in peak snowpack ( ∼45 %) in addition to a shorter snow season. Declines in the peak snowpack will be much greater in ... Article in Journal/Newspaper Tundra Directory of Open Access Journals: DOAJ Articles Marmot Creek ENVELOPE(-131.321,-131.321,63.766,63.766) Hydrology and Earth System Sciences 24 5 2731 2754 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 |
spellingShingle |
Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 X. Fang J. W. Pomeroy Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin |
topic_facet |
Technology T Environmental technology. Sanitary engineering TD1-1066 Geography. Anthropology. Recreation G Environmental sciences GE1-350 |
description |
Climate change is anticipated to impact the hydrology of the Saskatchewan River, which originates in the Canadian Rockies mountain range. To better understand the climate change impacts in the mountain headwaters of this basin, a physically based hydrological model was developed for this basin using the Cold Regions Hydrological Modelling platform (CRHM) for Marmot Creek Research Basin ( ∼9.4 km 2 ), located in the Front Ranges of the Canadian Rockies. Marmot Creek is composed of ecozones ranging from montane forests to alpine tundra and alpine exposed rock and includes both large and small clearcuts. The model included blowing and intercepted snow redistribution, sublimation, energy-balance snowmelt, slope and canopy effects on melt, Penman–Monteith evapotranspiration, infiltration to frozen and unfrozen soils, hillslope hydrology, streamflow routing, and groundwater components and was parameterised without calibration from streamflow. Near-surface outputs from the 4 km Weather Research and Forecasting (WRF) model were bias-corrected using the quantile delta mapping method with respect to meteorological data from five stations located from low-elevation montane forests to alpine ridgetops and running over October 2005–September 2013. The bias-corrected WRF outputs during a current period (2005–2013) and a future pseudo global warming period (PGW, 2091–2099) were used to drive model simulations to assess changes in Marmot Creek's hydrology. Under a “business-as-usual” forcing scenario, Representative Concentration Pathway 8.5 (RCP8.5) in PGW, the basin will warm up by 4.7 ∘ C and receive 16 % more precipitation, which will lead to a 40 mm decline in seasonal peak snowpack, 84 mm decrease in snowmelt volume, 0.2 mm d −1 slower melt rate, and 49 d shorter snow-cover duration. The alpine snow season will be shortened by almost 1.5 months, but at some lower elevations there will be large decreases in peak snowpack ( ∼45 %) in addition to a shorter snow season. Declines in the peak snowpack will be much greater in ... |
format |
Article in Journal/Newspaper |
author |
X. Fang J. W. Pomeroy |
author_facet |
X. Fang J. W. Pomeroy |
author_sort |
X. Fang |
title |
Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin |
title_short |
Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin |
title_full |
Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin |
title_fullStr |
Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin |
title_full_unstemmed |
Diagnosis of future changes in hydrology for a Canadian Rockies headwater basin |
title_sort |
diagnosis of future changes in hydrology for a canadian rockies headwater basin |
publisher |
Copernicus Publications |
publishDate |
2020 |
url |
https://doi.org/10.5194/hess-24-2731-2020 https://doaj.org/article/46290a7f35a349329ed23ba1b676b8cb |
long_lat |
ENVELOPE(-131.321,-131.321,63.766,63.766) |
geographic |
Marmot Creek |
geographic_facet |
Marmot Creek |
genre |
Tundra |
genre_facet |
Tundra |
op_source |
Hydrology and Earth System Sciences, Vol 24, Pp 2731-2754 (2020) |
op_relation |
https://www.hydrol-earth-syst-sci.net/24/2731/2020/hess-24-2731-2020.pdf https://doaj.org/toc/1027-5606 https://doaj.org/toc/1607-7938 doi:10.5194/hess-24-2731-2020 1027-5606 1607-7938 https://doaj.org/article/46290a7f35a349329ed23ba1b676b8cb |
op_doi |
https://doi.org/10.5194/hess-24-2731-2020 |
container_title |
Hydrology and Earth System Sciences |
container_volume |
24 |
container_issue |
5 |
container_start_page |
2731 |
op_container_end_page |
2754 |
_version_ |
1766230111239012352 |