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Publication Additional Information Download
Publication Type
Journal Article
Authorship
Aubry-Wake, C., Pradhananga, D., Pomeroy, J.W.
Title
Hydrological process controls on streamflow variability in a glacierized headwater basin.
Year
2022
Publication Outlet
Hydrological Processes, 36(10), e14731.
DOI
https://doi.org/10.1002/hyp.14731
Citation
Aubry-Wake, C., Pradhananga, D., Pomeroy, J.W. (2022) Hydrological process controls on streamflow variability in a glacierized headwater basin. Hydrological Processes, 36(10), e14731. https://doi.org/10.1002/hyp.14731
Abstract
Mountain glacierized headwaters are currently witnessing a transient shift in their hydrological and glaciological systems in response to rapid climate change. To characterize these changes, a robust understanding of the hydrological processes operating in the basin and their interactions is needed. Such an investigation was undertaken in the Peyto Glacier Research Basin, Canadian Rockies over 32 years (1988–2020). A distributed, physically based, uncalibrated glacier hydrology model was developed using the modular, object-oriented Cold Region Hydrological Modelling Platform to simulate both on and off-glacier high mountain processes and streamflow generation. The hydrological processes that generate streamflow from this alpine basin are characterized by substantial inter-annual variability over the 32 years. Snowmelt runoff always provided the largest fraction of annual streamflow (44% to 89%), with smaller fractional contributions occurring in higher streamflow years. Ice melt runoff provided 10% to 45% of annual streamflow volume, with higher fractions associated with higher flow years. Both rainfall and firn melt runoff contributed less than 13% of annual streamflow. Years with high streamflow were on average 1.43°C warmer than low streamflow years, and higher streamflow years had lower seasonal snow accumulation, earlier snowmelt and higher summer rainfall than years with lower streamflow. Greater ice exposure in warmer, low snowfall (high rainfall) years led to greater streamflow generation. The understanding gained here provides insight into how future climate and increased meteorological variability may impact glacier meltwater contributions to streamflow and downstream water availability as alpine glaciers continue to retreat.
Program Affiliations
GWF: Global Water Futures
Project Affiliations
GWF-IMPC: Integrated Modelling Program for Canada
GWF-MWF: Mountain Water Futures
Publication Stage
Published
Download Links
https://doi.org/10.1002/hyp.14731 Data Availability Statement: The CRHM modelling files (observation and project files), as well as the scripts used to analyze and plot the CRHM model outputs, can be found at: https://github.com/caubrywake/PeytoCRHM_1990_2020
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