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Heterogeneous snowpack response and snow drought occurrence across river basins of northwestern North America under 1.0°C to 4.0°C global warming
by
Cannon, Alex J.
, Bonsal, Barrie R.
, Shrestha, Rajesh R.
, Najafi, Mohammad Reza
, Bonnyman, James M.
in
Anthropogenic climate changes
/ Anthropogenic factors
/ artificial intelligence
/ Atmospheric Sciences
/ Climate change
/ Climate Change/Climate Change Impacts
/ Climate control
/ Climate models
/ decline
/ Drought
/ Earth and Environmental Science
/ Earth Sciences
/ Freshwater
/ Global warming
/ Human influences
/ Inland water environment
/ Learning algorithms
/ Machine learning
/ Mean temperatures
/ Precipitation
/ Regional climate models
/ Regional climates
/ River basins
/ Rivers
/ Saskatchewan
/ Snow
/ Snow-water equivalent
/ Snowpack
/ Socioeconomic factors
/ Spatial variations
/ Storage
/ Temperature
/ Temperature control
/ Thresholds
/ Yukon Territory
2021
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Heterogeneous snowpack response and snow drought occurrence across river basins of northwestern North America under 1.0°C to 4.0°C global warming
by
Cannon, Alex J.
, Bonsal, Barrie R.
, Shrestha, Rajesh R.
, Najafi, Mohammad Reza
, Bonnyman, James M.
in
Anthropogenic climate changes
/ Anthropogenic factors
/ artificial intelligence
/ Atmospheric Sciences
/ Climate change
/ Climate Change/Climate Change Impacts
/ Climate control
/ Climate models
/ decline
/ Drought
/ Earth and Environmental Science
/ Earth Sciences
/ Freshwater
/ Global warming
/ Human influences
/ Inland water environment
/ Learning algorithms
/ Machine learning
/ Mean temperatures
/ Precipitation
/ Regional climate models
/ Regional climates
/ River basins
/ Rivers
/ Saskatchewan
/ Snow
/ Snow-water equivalent
/ Snowpack
/ Socioeconomic factors
/ Spatial variations
/ Storage
/ Temperature
/ Temperature control
/ Thresholds
/ Yukon Territory
2021
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Heterogeneous snowpack response and snow drought occurrence across river basins of northwestern North America under 1.0°C to 4.0°C global warming
by
Cannon, Alex J.
, Bonsal, Barrie R.
, Shrestha, Rajesh R.
, Najafi, Mohammad Reza
, Bonnyman, James M.
in
Anthropogenic climate changes
/ Anthropogenic factors
/ artificial intelligence
/ Atmospheric Sciences
/ Climate change
/ Climate Change/Climate Change Impacts
/ Climate control
/ Climate models
/ decline
/ Drought
/ Earth and Environmental Science
/ Earth Sciences
/ Freshwater
/ Global warming
/ Human influences
/ Inland water environment
/ Learning algorithms
/ Machine learning
/ Mean temperatures
/ Precipitation
/ Regional climate models
/ Regional climates
/ River basins
/ Rivers
/ Saskatchewan
/ Snow
/ Snow-water equivalent
/ Snowpack
/ Socioeconomic factors
/ Spatial variations
/ Storage
/ Temperature
/ Temperature control
/ Thresholds
/ Yukon Territory
2021
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Heterogeneous snowpack response and snow drought occurrence across river basins of northwestern North America under 1.0°C to 4.0°C global warming
Journal Article
Heterogeneous snowpack response and snow drought occurrence across river basins of northwestern North America under 1.0°C to 4.0°C global warming
2021
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Overview
Anthropogenic climate change is affecting the snowpack freshwater storage, with socioeconomic and ecological impacts. We present an assessment of maximum snow water equivalent (SWE
max
) change in large river basins of the northwestern North America region using the Canadian Regional Climate Model 50-member ensemble under 1.0 °C to 4.0 °C global warming thresholds above the pre-industrial period. The projections indicate steep SWE
max
decline in the warmer coastal/southern basins (i.e., Skeena, Fraser and Columbia), moderate decline in the milder interior basins (i.e., Peace, Athabasca and Saskatchewan), and either a small increase or decrease in the colder northern basins (i.e., Yukon, Peel, and Liard). A key factor for these spatial differences is the proximity of winter mean temperature to the freeze/melt threshold, with larger SWE
max
declines for the basins closer to the threshold. Using the random forests machine-learning model, we find that the SWE
max
change is primarily temperature controlled, especially for warmer basins. Further, under a categorical framework of below-normal SWE
max
defined as snow drought (SD), we find that above-normal temperature and precipitation are the dominant conditions for SD occurrences under higher global warming thresholds. This implies a limited capacity of precipitation increase to compensate the temperature-driven snowpack decline. Additionally, the frequency and severity of SD occurrences are projected to be most extreme in the southern basins where current water demands are highest. Overall, the results of this study, including insights on snowpack changes, their climatic controls, and the framework for SD classification, are applicable for basins spanning a range of hydro-climatological regimes.
Publisher
Springer Netherlands,Springer Nature B.V
Subject
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